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Article

Machine Learning Workflow for Fracture Modeling in the Tensleep Reservoir

1
Department of Mining, Petroleum and Metallurgical Engineering, Faculty of Engineering, Cairo University, Cairo 12613, Egypt
2
Oil and Gas Engineering Department, College of Engineering and Technology, Arab Academy for Science, Technology and Maritime Transport, Alexandria 1029, Egypt
*
Author to whom correspondence should be addressed.
Energies 2026, 19(7), 1683; https://doi.org/10.3390/en19071683
Submission received: 9 February 2026 / Revised: 26 February 2026 / Accepted: 6 March 2026 / Published: 30 March 2026

Abstract

Fractured reservoir characterization is a complex and challenging task due to its depositional nature and high uncertainty in the spatial distribution of fractures, typically when well data is limited, and interpolation algorithms are employed. This paper introduces an alternative workflow designed to enhance fracture modeling between well locations by incorporating seismic attributes, using publicly released data from the Teapot Dome Field. The paper’s objective is to create a fracture model for the Tensleep reservoir in the Teapot Dome Anticline by employing seismic attributes sensitive to fault and fracture features, while also demonstrating the limitations of interpolation-based models such as Gaussian simulation. The approach uses artificial neural networks to predict fracture intensity by analyzing seismic data and well logs, training supervised probabilistic artificial networks to identify the seismic attributes that most closely correlate with the fracture intensity property derived from well log data. The validated network successfully transformed the 3D seismic data into 3D fracture intensity data, achieving a high correlation coefficient between the selected seismic attributes and the training wells. The research findings are extremely valuable because they help address the lack of information on fractures, improve reservoir management, and optimize well placement.

1. Introduction

Fractures are among the more prevalent geological features found in the upper layer of the Earth’s crust. They can be identified in the outcrops as well as in subsurface data like seismic and well log records, and it is highly probable that most reservoirs contain some degree of natural fracturing [1]. The development of naturally fractured reservoirs typically necessitates a different strategy than that employed for conventional reservoirs. A major challenge in managing fractured reservoirs is the variability in rock properties, such as porosity and permeability, between the matrix and the fractures. Consequently, these fractured reservoirs are often classified as dual porosity reservoirs, where the matrix (first medium) and fractures (second medium) exhibit distinctly different capacitive and conductive characteristics [2].
Naturally fractured reservoirs (NFRs) are important for the evaluation and exploration of oil and gas reservoirs with abundant unconventional oil and rich experience in shale gas production. The difficulty in developing and investigating these NFRs is related to their complex fracture structure and variable fracture intensity features. The casing and cementing program, hydraulic test, and production program of wells will be designed based on fracture features, so it is very important to know the distribution of the fracture features precisely. There are many methods to define fracture features, and the seismic method or the logging method is widely used. However, the application of the logging method has a high cost, and the resolution is limited. The spatial resolution of the seismic method is commonly less than 10 m, so the fracture feature is also not clear. Additionally, the logging method and the seismic method need to be well spaced, and the interval will result in missing data. The advanced logging method can provide a high-resolution, well-spaced fracture feature, but the cost is extremely high [3].
Natural fractures in a reservoir may have positive and adverse impacts on the fluid movement. Fractures enhance permeability through extra routes for the flow of fluids, hence increasing hydrocarbon production. On the other hand, the fracture may act either as a conduit or barrier for water breakthrough, impeding oil production and changing the efficiency of the reservoir [1,2]. Such a dual role calls for an advanced approach in fracture modeling to capture the variability and randomness in fracture distribution within the reservoir [4]. For instance, in most instances, fractures provide secondary porosity and permeability in rock matrices that tend to exhibit low porosity, as in the case of carbonate and clastic reservoirs. The other features involved the fluid movements of matrix-dominated production zones, which also act as conduits to early water breakthrough [5].
Fracture properties can be affected by several geological factors, which are often referred to as “fracture drivers.” These factors include lithology, structural features, proximity to faults, stress regimes, and tectonic history. Fracture drivers are generally inferred from seismic and well log data, allowing geologists to estimate the location, orientation, and intensity of fractures across the reservoir. However, Formation MicroImager (FMI) log techniques, which can be effective at capturing detailed fracture data, are prohibitively expensive and thus limited to a small number of wells. Reservoir-wide fracture formation documentation remains incomplete, and there is a strong need for predictive models that can extrapolate fracture properties beyond the limited scopes of FMI data [6,7,8].
In high heterogeneous reservoirs, traditional characterization methods frequently lose the precise location and orientation of fractures. However, the recent integration of artificial intelligence into reservoir characterization has turned this challenge into a feasible task. Artificial intelligence can integrate various tools from multiple sources, thus overcoming uncertainty. The most widely recognized artificial intelligence techniques include Artificial Neural Networks (ANN) and Fuzzy Logic [9].
The study area is the Teapot Dome region in central Wyoming, USA, which was chosen because it contains a naturally fractured reservoir and its data set is available, especially the 3D seismic cube. The Teapot Dome is an important geological structure characterized by a complex fracture network, particularly within the sandstone reservoir known as Tensleep. Numerous studies have focused on characterizing and modeling these fractures in this area. Cooper and others [10,11,12,13] identified three sets of fractures, striking perpendicularly, parallel, and obliquely to the fold axis. Valerie [14] and Thomas [15] employed volumetric seismic features as a guide for characterizing and modeling the fractures. Some researchers, such as Ouenes et al. [16], integrated post-stack seismic attributes (e.g., curvature, inversion, and spectral imaging) with fracture drivers to generate continuous fracture models for the Tensleep reservoir. While valuable, their approach is limited by seismic resolution, deterministic correlations, and dependence on costly FMI data, which restricts its applicability across the reservoir. Similarly, Thachaparambil [17] extracted discrete 3D fracture networks from seismic data using volumetric attributes, providing insights into fracture geometry, but remained constrained by data resolution and the inability to capture nonlinear relationships. In contrast, our proposed machine learning workflow employs Artificial Neural Networks to integrate multiple seismic attributes and well log data, capturing complex nonlinear interactions and offering a more scalable, cost-effective solution for reservoir-wide fracture characterization. Cooper et al. [18] identified a dominant NW-WNW fracture set that plays a significant role in fluid movement within the reservoir. Thomas et al. [15] confirmed this through their study in which they developed a model of the discrete fracture network based on integrated field data, image probes, and three-dimensional seismic data. Characterizing the discrete fracture network in this reservoir is not only important for hydrocarbon recovery but also for understanding the nature of the dual-porosity reservoir. In addition, Teapot Dome was classified by Spooner et al. [19] as a Type II fractured reservoir. In this type of reservoir, fractures play a primary role in permeability, while the matrix plays a secondary role. This classification gives great importance to the accuracy of discrete fracture network modeling in improving the recovery factor, which is often low in naturally fractured reservoirs due to the high uncertainty in fracture characterization and modeling [20].
The paper tries to develop an integrated approach for characterizing fractures in the naturally fractured Tensleep Formation, Wyoming, USA. A scheme using the Artificial Neural Network technique is presented, incorporating seismic attributes along with the well log data, so that fracture intensity variations could be quantified for the whole reservoir. By using the strengths of DFN modeling, we will build a 3D fracture intensity cube that optimally approximates fracture distribution, orientation, and density within the Tensleep Formation.
The results from our paper offer a cost-effective and scalable approach to fractured characterization that has the potential to develop reservoir management and recovery strategies around the world in fractured reservoirs. This research has integrated artificial intelligence techniques into conventional reservoir characterization procedures to address the complexities related to modeling fractured reservoirs, furthering an improved understanding of fracture dynamics and their impact on reservoir performance using data-driven methodologies.
Despite the progress achieved by traditional interpolation and geostatistical methods, their ability to represent the heterogeneity of fractures in Teapot Dome remains limited. These approaches often oversimplify fracture variability and fail to capture nonlinear interactions between geological drivers and fracture intensity. Such shortcomings highlight the necessity of adopting advanced machine learning workflows, which can integrate diverse seismic and well log data to provide more accurate, scalable, and cost-effective fracture characterization. This study, therefore, introduces an ANN-based approach designed to overcome these limitations and improve reservoir-wide fracture modeling in the Tensleep Formation.

2. Materials and Methods

The major steps involved in this study include data preparation, fracture characterization, seismic attribute analysis, ANN and PNN model development, and the construction of a 3D fracture intensity cube together with DFN modeling. These steps were developed to introduce an appropriate workflow regarding the characterization and prediction of fracture intensity within the Teapot Dome Tensleep Formation.

2.1. Data Preparation and Fracture Characterization

2.1.1. Dataset Collection

The dataset employed in this research was provided by the RMOTC and includes one 3D seismic cube and well log data from four wells located within the Tensleep Formation: 25-1-X-14, 48-X-28, 67-1-TPX-10, 71-1-X-14. One 3D seismic cube at the surface is about 70 km2. The maximum two-way time is 3000 ms. Each well had Formation MicroImager logs, fracture measurement logs, and well tops that were very important in model calibration and validation because of the essential fracture data they possessed.

2.1.2. Fracture Classification and Intensity Logs

Fractures from the four wells were initially classified into dip angle and azimuth classes based on the FMI log data; such a classification enabled the development of a fracture intensity log for each fracture set corresponding to different fracture orientations. These fracture intensity logs were necessary to train and validate the ANN model. Subsequently, they were combined with seismic attributes to build the 3D fracture intensity cube.

2.2. Seismic Attribute Interpretation

2.2.1. Seismic Horizon Interpretation and Structural Modeling (Time and Depth Domains)

Major seismic horizons within the Teapot Dome were interpreted on a 3D post-stack migrated seismic volume. Identified reflectors from previous studies were picked with the aid of Petrel software. Then, an auto-tracking function in the software was used to produce continuous horizons across each seismic line that formed the basic constituent of a 3D structural model developed in the time domain.
This data was afterwards converted to depth by creating a velocity model. It was built using velocity points provided by the processing center and distributed on interpreted horizons. The cell dimensions in this model were set to 50 × 50 m, while the model itself was divided into eight different layers vertically. The velocity model is a key tool used for converting data between time and depth, and vice versa. It is designed to handle various types of data, including volumetric (VOLUME) and surface-based (SURFACE) data.

2.2.2. Structural Model of Tensleep Reservoir in the Depth Domain

The structural model of Tensleep Reservoir in the depth domain was constructed from the top and bottom horizons of the Tensleep Formation. The model was split into 720 vertical layers, and each grid cell was 400 × 400 m. The number of layers, determined through iterative adjustments, was found to be optimal for accurately representing fracture data, including dip angles and azimuths. The model was subsequently utilized to generate seismic attributes aimed at detecting fractures within the formation.

2.3. Construction of Seismic Attributes

Seismic attributes computed from the 3D post-stack seismic volume enhanced fracture detection within the Tensleep Formation. Of the myriad attributes tried, only two were used, Volume Curvature and Ant Tracking, since they showed the greatest correlation with fracture intensity from the preliminary analysis. These were imported into Hampson Russell’s software as external attributes and were used to train the ANN and PNN models to estimate secondary porosity and fracture intensity.

2.4. Secondary Porosity and Fracture Intensity Estimation Using ANN

2.4.1. ANN Model Architecture for Secondary Porosity

As secondary porosity is a key proxy for fracture intensity, an ANN model that estimated secondary porosity was established. The general structure of the ANN contained one input layer, six hidden layers, and one output layer. In this work, the input data involved density logs, deep resistivity logs, and compressional slowness logs of three wells: 25-1-X-14, 48-X-28, and 71-1-X-4. Well 67-1-TPX-10 was used herein to validate the model.
In this respect, the ANN model was used to iteratively adjust the weight of connections between neurons, applying a backpropagation and a gradient descent algorithm. This would, in effect, minimize the error between the predicted and the actual porosity values. The model accurately predicted porosity for the input of secondary porosity into the fracture intensity model.

2.4.2. ANN Model for Fracture Intensity Estimation

An ANN model with a hidden layer of ten neurons was also developed to estimate fracture intensity for wells with no direct availability of FMI data. This ANN model took the estimated secondary porosity along with the density logs, compressional slowness logs and deep resistivity logs as inputs and provided fracture intensity estimates from its output. The ANN was trained on data from three wells-67-1-TPX-10, 48-X-28, and 71-1-X-4-and tested on well 25-1-X-14.
The results obtained from the ANN model showed a high correlation between predicted and actual fracture intensity, thereby proving its capability for generalization across the data and predicting fracture characteristics in wells lacking FMI logs.

2.5. 3D Fracture Intensity Cube Construction Using PNN

2.5.1. Multiple Attribute Regression for Seismic Attribute Selection

Multiple regressions were done on a total of forty seismic attributes to establish which seismic attributes best described fracture intensity. Based on these regressions, the capability of the HRS software was utilized to analyze, for each attribute, the correlation with fracture intensity and hence chose the best fifteen with the highest predictability accuracy. A validation curve showed that more than fifteen attributes produced overfitting, so the model was limited to only the better attributes.

2.5.2. Probabilistic Neural Network (PNN) Model for Fracture Intensity Prediction

In this respect, the PNN was trained using the chosen seismic attributes through the 3D seismic cube for fracture intensity modeling. Generally, the PNN consists of four layers comprising input, hidden, pattern, and output. The network approximates the probability density functions of fracture intensity from the training data integrated with seismic attribute inputs for a likely estimation of fracture intensity.
Cross-validation analysis favored an operator length of nine in the PNN model, which balanced the granularity and computational efficiency of predictions. The PNN model showed a training correlation coefficient of 0.93 while the validation error rate was less than 4% in most wells, further confirming the reliability of this model to predict the fracture intensity over the seismic data set.

2.6. Discrete Fracture Network (DFN) Model Construction

The fracture intensity cube generated by the PNN model was transformed into a 3D geocellular model representing fracture distribution across the Tensleep Formation. Sequential Gaussian simulation was used to create a fracture intensity property for each fracture set (class0, class1, class2, and class3), which served as inputs for constructing the Discrete Fracture Network (DFN).
Then, the DFN model was created using the fracture sets defined above. Herein, the Fisher distribution for the fracture orientation was employed to decrease the variability around the mean orientation. Power law was considered for fracturing length and normal for aperture. Permeability was derived accordingly using the cubic law. Table 1 summarizes the statistical distribution parameters for the main geometric properties (length, aperture, and orientation) applied in DFN modeling.
Upscaling was done to convert the data obtained from the DFN model into properties that were usable for either dual-porosity or -permeability flow simulation. Fracture porosity, permeability, sigma factor, and spacing were calculated and assigned to each grid cell comprising the reservoir simulation model. Upscaled properties enabled the correct simulation of fluid movement within a fractured reservoir and helped with dynamic reservoir management strategies.

2.7. Validation and Application of the 3D Fracture Intensity Model

The final 3D fracture intensity cube was verified by comparing the predicted fracture intensities against independent well data with known fracture properties. The model was validated by cross-correlation analysis, with the acceptable correlation coefficient being greater than 0.8 for all wells used in the validation. Strong validation of the model confirmed its applicability to predict fracture intensity at locations where data is sparse; hence, a scalable method was developed for future fractured reservoir characterization.

3. Results

This work used Artificial Neural Networks (ANN) and Probabilistic Neural Networks (PNN) for fracture intensity prediction in the Tensleep Formation at the Teapot Dome. Integrating seismic attribute analyses, ANN and PNN modeling, and Discrete Fracture Network (DFN) construction, this workflow established a rigorous and detailed reservoir fracture representation. All the steps of the workflow are substantiated across 18 figures, which visually validate the accuracy of the model and give insight into the reservoir fracture characteristics.

3.1. Geological Setting and Dataset Overview

The Teapot Dome is in the Laramide structural belt of Wyoming (Figure 1), which describes the geographical location. Figure 2a shows the structural relationship of the Teapot Dome with respect to other Laramide uplifts, and Figure 2b illustrates the segmentation of the Teapot Dome by faults within the Salt Creek structural complex. These tectonics features, like the spatial distribution and intensity of fractures across the reservoir, provide the geologic framework in which the fracture characterization is constructed.
The Tensleep Formation is a hydrocarbon-bearing unit composed primarily of aeolian sandstone interbedded with marine dolomites. Figure 3 shows the stratigraphic column with the lithological units and hydrocarbon-rich layers that require reservoir productivity. Seismic interpretation visualized in Figure 4 delineates key reservoir horizons within a framework for integrating seismic attributes into fracture prediction models.
Available data from four wells, 48-X-28, 71-1-X-4, 67-1-TPX-10, and 25-1-X-14, whose locations are shown in Figure 5, were selected for model calibrations and their validation. These wells also had FMI logs, which provided the necessary fracture intensity data and were the reference points used to train the ANN and PNN models.

3.2. Structural Modeling and Seismic Attribute Interpretation

The 3D seismic dataset notes nine primary reflectors, which were auto-tracked to generate a structural model. The velocity model construction process is explained in Figure 6, which illustrates:
  • Velocity points (Figure 6a);
  • The structural skeleton (Figure 6b);
  • Interpreted seismic horizons (Figure 6c);
  • The finalized velocity model used for time-to-depth conversion (Figure 6d).
The structural model, visualized in Figure 7, captures the reservoir’s stratigraphic and structural complexity. The model consists of 720 vertical layers with a grid resolution of 400 × 400 m, providing a foundation for analyzing fractures and integrating seismic attributes.
Seismic attributes, particularly Volume Curvature and Ant Tracking, are computed to detect fractures by highlighting structural discontinuities and subtle subsurface features. The interpretation of seismic data and integration of attributes into fracture analysis workflows are illustrated in Figure 8, showing seismic crossline X-line 94 with interpreted horizons.

3.3. Fracture Set Distribution and Orientation Analysis

Fracture orientations and intensity analyses for individual wells provided insights into the spatial variability of fractures within the reservoir. Figure 9 presents polar plots of fracture orientation and intensity for the following wells: 48-X-28, 67-1-X-10, 25-1-X-14, and 71-1-X-4. Fractures were grouped into four sets (Codes 0 to 3), with color-coded representations bringing out variability. The combined view across all wells showed high heterogeneity, important for understanding fracture dynamics, fluid, and reservoir management.

3.4. ANN Model Development and Validation for Secondary Porosity and Fracture Intensity

3.4.1. Secondary Porosity Estimation

The ANN model of secondary porosity predictions uses bulk density, compressional slowness, and resistivity logs as input parameters. The model architecture, illustrated in Figure 10, features six hidden layers with 10 neurons in each layer. Each hidden layer applies a non-linear activation function (ReLU was selected to capture complex relationships between petrophysical parameters), while the output layer employs a linear activation function to predict continuous porosity values. Validation against well 67-1-TPX-10 showed a high correlation between the observed and predicted porosity values, as presented in Figure 11, confirming the predictive accuracy of the model.

3.4.2. Fracture Intensity Estimation

The ANN model for fracture intensity prediction incorporates four input parameters: bulk density, compressional slowness, deep resistivity, and secondary porosity, Figure 12. These inputs are connected to a hidden structure consisting of ten hidden layers, each comprising approximately 12 neurons. The hidden layers employ a non-linear activation function (ReLU) to capture the complex relationships between petrophysical parameters and fracture intensity. The output layer consists of a single neuron with a linear activation function, which provides continuous predictions of fracture density. Validation against well 25-1-X-14 demonstrated excellent agreement between predicted and observed fracture intensities, as shown in Figure 13, confirming the robustness and predictive accuracy of the model.

3.5. Selection of Seismic Attributes and PNN Model Training

We optimized the seismic attribute selection by employing multiple regression analysis. The error curve in Figure 14 indicates that the model achieved optimal performance with 15 attributes. Adding more attributes increased the risk of over-fitting, highlighting the importance of precise attribute selection. These 15 attributes are listed in Table 2 along with their physical meaning. In the multiple regression analysis, a fast process called stepwise regression was applied. This procedure identified the best single attribute first, followed by the best pair, then the best triplet, and so on. At each stage, the criterion for selecting the “best” group was based on the RMS prediction error, meaning that the optimal group was the one that predicted the target logs with the least RMS error. This systematic approach ensured that the selected attributes contributed effectively to fracture intensity mapping while minimizing redundancy and over-fitting.
The PNN model, trained with the selected attributes, achieves a training correlation of 0.93 and validation errors below 4%. Figure 15 presents a scatter plot comparing actual and predicted fracture intensities, confirming the model’s reliability. The operator length for the PNN model, provided in Figure 16, was determined to be nine, ensuring a balance between prediction accuracy and computational efficiency.
In this study, the Probabilistic Neural Network (PNN) was applied not for classification purposes, but as a mapping tool to predict fracture intensity. The PNN employs a Gaussian radial basis activation function, where each neuron computes an exponential function of the squared distance between the input vector and a training sample. This kernel function enables the network to estimate probability density functions and capture similarity measures, which are then translated into continuous probabilistic maps of fracture intensity. By adopting this non-parametric approach, the PNN provides smooth and reliable spatial predictions, making it particularly effective for reservoir characterization and fracture mapping compared to conventional feedforward ANNs.

3.6. Construction of the 3D Fracture Intensity Cube and DFN Model

The PNN outputs were used to construct a 3D fracture intensity cube, which provided a spatially detailed representation of fracture intensity across the reservoir. Figure 17 illustrates the spatial distribution of fracture intensity, with color-coded zones representing varying intensity levels. This cube served as the foundation for constructing the DFN model.
The DFN model, depicted in Figure 18, incorporates fracture geometry and density for four fracture sets (Codes 1 to 4). Sequential Gaussian simulation was employed by assigning intensity properties to the DFN model, enabling realistic and detailed fracture characterization across the Tensleep Formation.

3.7. DFN Upscaling for Dynamic Simulation

Permeability and sigma factor were upscaled for dual-permeability flow simulations. The Discrete Fracture Network (DFN) model (Figure 18) provided a detailed representation of fracture distribution, orientation, and density across the Tensleep Formation, which served as the foundation for these upscaling processes.
The cubic law was used to calculate permeability. This law correlates fracture aperture with fluid flow, enabling the accurate estimation of fracture permeability within the network. Using the cubic law, fracture permeability was derived and assigned to individual grid cells in the simulation model. These permeability values were then statistically analyzed to ensure consistency with theoretical predictions.
In addition, fracture porosity, sigma factor, and spacing were calculated and integrated into the reservoir simulation grid. The upscaled properties allowed for dynamic simulations of fluid flow, providing insights into fluid migration pathways and supporting strategies for enhanced oil recovery (EOR) and secondary recovery. This approach underscores the importance of integrating detailed discrete fracture network (DFN) modeling with robust mathematical frameworks, such as the cubic law, to enhance predictions and optimize reservoir performance.

4. Discussion

This study provides a good application of Artificial Neural Networks (ANNs) and Probabilistic Neural Networks (PNNs) for predicting fracture intensity in the Tensleep Formation, a naturally fractured reservoir at Teapot Dome. By integrating seismics attributes and well log data, we develop a 3D fracture intensity cube and Discrete Fracture Network (DFN) model, which allows for an accurate and spatially comprehensive characterization of the fracture network. The results affirm the efficacy of machine learning in capturing complex geological features and underscore the transformative potential of AI-driven methods for fractured reservoir management.

4.1. Enhanced Fracture Characterization Through AI: Addressing Traditional Limitations

Naturally fractured reservoirs were very challenging for reservoir characterization owing to their highly heterogeneous and anisotropic nature, for instance, reservoirs of the Middle East and at Teapot Dome, Wyoming. Traditional methods of fracture characterization, such as sampling and FMI logging, result in very high resolution with respect to the fractures, yet are highly limited to their spatial coverage due to their high cost. A host of studies, such as Akshat and Sanjay [23], have established the fact that traditional approaches normally cannot capture the fracturing variability in a reservoir and thus provide poor recovery strategies. This paper, with the application of the ANN and PNN approaches, will not only address such shortfalls but also be computationally efficient and easily scalable for precise fracture intensity predictions over the entire reservoir.
The proposed model achieves this goal by using some of the seismic attributes, such as Volume Curvature and Ant Tracking, which were identified as key determinants of fracture intensity. The structural discontinuities and subtle changes that remain unclear within the raw seismic data agree with the works by Di and Gao [24] and Gao and Di [25], wherein the feasibility of seismic curvature attributes in mapping natural fractures and fault structures was demonstrated. We gained a decrease in prediction errors by optimizing the model to employ 15 highly predictive attributes in a manner where the model would not run the risk of overfitting and could generalize very well for the whole reservoir.

4.2. Implications of Seismic Attribute Selection and ANN-PNN Modeling Accuracy

The selection of seismic attributes is important to enhance the model performance; each attribute contributes differently to prediction within the framework. In our study, Volume Curvature and Ant Tracking are used as key indicators for fracture intensity, aligning with the works of Di and Gao [26], who established that curvature-related attributes can enhance fracture detection, especially in folded and faulted geological settings. Volume Curvature highlights flexural stress patterns that correlate with fracture formation, while Ant Tracking enhances the detection of fault trends by reducing subtle structural features. The integration of these attributes allowed our ANN model to predict fracture intensity with high spatial fidelity.
Our model achieved a training correlation of 0.93 by using multiple attributes regression for the selection of the optimal number of attributes, with very low validation errors for all wells. This is an important result since it shows that the AI model can capture the spatial variability of fractures with limited FMI data, avoiding the cost of acquiring extensive direct measurements. This work develops approaches suggested in Zaiery et al. [27], where machine learning models applied for fracture density estimation showed comparable performance in extrapolating fracture properties over spatially limited datasets.

4.3. Constructing a 3D Fracture Intensity Cube: A Step Toward Dynamic Modeling

The resulting model comes up with a 3D fracture intensity cube, which gives details regarding a spatially improved mesh of fracture intensities within the Tensleep Formation. This provided a framework from which to base the DFN model for simulations of the fracture geometry, orientation, and density at a reservoir-wide scale. The development of such a detailed 3D model is important for understanding the fluid flow pathways, which are believed to be greatly influenced by fracture distribution and intensity. This model, as observed by Di and Gao [26] and Akshat and Sanjay [23], will enhance the prediction of fluid movement within the reservoir, ensuring better EOR and even better planning of secondary recovery with the definition of high-intensity fracture zones that might act either as conduits or barriers to flow.
The 3D fracture intensity cube further feeds the DFN model with directly upscaled intensity data for dynamic simulations. Again, the approach here rests on the findings of Lefranc et al. [28]: while the DFN models are critical for effective fracture characterization, in the absence of spatially continuous data, these models usually fail in heterogeneous reservoirs. By incorporating our intensity cube into the DFN model, we enable dual-porosity/-permeability flow simulation that captures complex fractures and matrix interactions in flow properties.

4.4. Probabilistic Neural Network (PNN) and Cross-Validation: Ensuring Model Robustness

During the implementation of the PNN model, the validation of nine as the optimum operator length yields constantly low values for validation error, thus further confirming the reliability of this model. Such an accurate model is very important; this is because the reservoir models should work reliably under various conditions and with various types of datasets. Our model could maintain the validation error below 4% while achieving high cross-correlation across wells. This proves that the model is robust. This level of reliability is essential in fractured reservoirs, where unexpected variations in fracture intensity may significantly impact production forecasting and secondary recovery methods.
The optimum attribute weighting process, which entails cross-validation, definitely improves the model reliability. Evidence to this point was provided by Rockhold et al. [29] and Zaiery et al. [27], who claimed that refining attribute weights is essential to decreasing prediction errors. Accordingly, to reduce overfitting, a systematic adjustment of the weights of each attribute was conducted, thereby assuring strong generalization throughout the modeling process for independent wells—an essential feature of its applicability to other naturally fractured reservoirs.

4.5. Practical Implications for Reservoir Management and Secondary Recovery

The development and training phase of the neural network requires access to high-quality data (including FMI logs) and appropriate computational resources. This stage involves an initial investment to ensure the robustness of the model. Once the model has been trained and validated, however, its application becomes more economical: it can be deployed in new wells or nearby areas using conventional logs, thereby reducing the need for additional costly FMI acquisitions.
Our results have wide implications for reservoir management, particularly in mature fields where optimizing secondary recovery is crucial. The resulting 3D fracture intensity cube provides reservoir engineers with high-resolution maps of fracture intensity. These maps are valuable for well placement, improving drilling paths, and preventing water breakthroughs by identifying highly conductive zones within fracture networks. By modeling fracture intensity and orientation precisely, our framework supports more targeted secondary recovery strategies, addressing challenges noted in previous studies on fractured reservoirs [10,18,30].

4.6. Model Limitations and Future Directions

The PNN approach in our study shows excellent prediction of how severe fractures may be, but future work could look into ways to make it more responsive to real-time changes and better at including geomechanical factors. For instance, the inclusion of real-time seismic monitoring information could enhance model predictions by considering variations in reservoir stress states, especially as they relate to production activities. According to Soumya et al. [31], geomechanical modeling can increase our ability to predict how stress data and fracture slip probabilities play out, especially in reservoirs where we are injecting fluids. This could give us an accurate forecast, particularly if we use top-notch machine learning tools like LSTM networks that have been finely tuned with PSO, because they really capture the flow of time in the reservoir. In a previous study, Xuemei et al. [4] showed that the LSTM-PSO model demonstrates great capability of handling complex nonlinear data, and probably further improvements of predictive performance of fracture models are possible by including temporal information together with spatial information.

5. Conclusions

Our study confirms the potential of AI-driven fracture characterization methods, particularly in naturally fractured reservoirs where traditional approaches often face limitations. By integrating seismic data with ANN and PNN models, we developed a workflow capable of predicting fracture intensity in a robust and scalable manner. The resulting 3D fracture intensity cube, incorporated into the DFN model, provides reservoir engineers with high-resolution maps that support well placement, optimize drilling paths, and help mitigate water breakthroughs.
While the development stage requires investment in high-quality data and computational resources, the cost-effectiveness of the workflow is primarily realized during its application phase. Once trained and validated, the model can be applied to new wells or nearby areas using conventional logs, thereby reducing reliance on additional costly FMI acquisitions.
This framework offers practical value for reservoir management, especially in mature fields where secondary recovery strategies are critical. Future research may further enhance the methodology by incorporating real-time geomechanical information and advanced AI techniques, leading to more flexible models that can adapt to the evolving challenges of fractured reservoir management.

Author Contributions

Conceptualization, I.A., A.S.D. and G.H.; methodology, I.A., A.S.D. and G.H.; software, I.A.; validation, I.A., A.S.D. and G.H.; formal analysis, I.A., A.S.D. and G.H.; investigation, I.A.; resources, I.A.; data curation, I.A.; writing—original draft preparation, I.A.; writing—review and editing, I.A., A.S.D. and G.H.; visualization, I.A.; supervision, A.S.D. and G.H.; project administration, I.A. All authors have read and agreed to the published version of the manuscript.

Funding

This research received no external funding.

Data Availability Statement

Part of the dataset used in this study was obtained from the SEG website, and the remaining part was purchased personally by the first author (Israa Ahmed). The authors confirm that all data sources were legally accessed and properly utilized for the purposes of this research.

Acknowledgments

The authors would like to express sincere gratitude to Hayan Abdul Ghani Al-Suwad, Minister of Oil of Iraq, and to Basim Mohammed Khudair, Deputy Minister of Oil for Extraction Affairs, for their valuable support. Special thanks are also extended to Karim Yasser Hashim, Director General of the Reservoirs and Field Development Department at the Ministry of Oil, and to Hisham Yass Shalan, Director General of the Training and Development Department at the Ministry of Oil, for their encouragement and guidance. The authors are deeply appreciative of the support provided by Saeed Zgair Shalaka, Director of Dhi Qar Oil Company, and by Rasheed Sherhan, Deputy Director General for Production Affairs at Dhi Qar Oil Company, whose assistance has been instrumental in the authors’ professional journey. Finally, heartfelt thanks go to Mohaned Adel Jayan for his unwavering moral and financial support throughout the authors’ academic path.

Conflicts of Interest

The authors declare no conflicts of interest. This research was entirely self-funded. Israa Ahmed personally covered all expenses, including data acquisition, and was solely responsible for the design of the study, the collection, analyses, and interpretation of data, the writing of the manuscript, and the decision to publish the results.

Abbreviations

The following abbreviations are used in this manuscript:
DFNDiscrete fracture network
NFRsNaturally fractured reservoirs
FMIFormation MicroImager
3DThree-dimensional
ANNArtificial Neural Network
PNNProbabilistic Neural Network
PSOParticle Swarm Optimization
LSTMLong Short-Term Memory

References

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Figure 1. Location of the Teapot Dome in Wyoming. The white square outlines the broader area of interest. The inset on the right presents a magnified view of a smaller portion within this square. Arrows indicate the source region of the inset enlargement [13].
Figure 1. Location of the Teapot Dome in Wyoming. The white square outlines the broader area of interest. The inset on the right presents a magnified view of a smaller portion within this square. Arrows indicate the source region of the inset enlargement [13].
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Figure 2. (a) Schematic map of the Teapot Dome within the Laramide uplifts (modified after James et al. [21]). (b) Schematic location of the Teapot Dome within the Salt Creek structural complex (modified after Chiaramonte [22]).
Figure 2. (a) Schematic map of the Teapot Dome within the Laramide uplifts (modified after James et al. [21]). (b) Schematic location of the Teapot Dome within the Salt Creek structural complex (modified after Chiaramonte [22]).
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Figure 3. Schematic stratigraphic column of the Tensleep Formation, highlighting lithological units and key hydrocarbon-bearing layers (modified after Chiaramonte [22]).
Figure 3. Schematic stratigraphic column of the Tensleep Formation, highlighting lithological units and key hydrocarbon-bearing layers (modified after Chiaramonte [22]).
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Figure 4. Seismic in-line (128) with interpreted reservoir horizons within the Tensleep Formation.
Figure 4. Seismic in-line (128) with interpreted reservoir horizons within the Tensleep Formation.
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Figure 5. Well location map of the Teapot Dome Field: Spatial distribution of key wells (48-X-28, 71-1-X-4, 67-1-TPX-10, and 25-1-X-14) overlaid on seismic time slice at the Teapot Dome Field. White circles indicate the well locations.
Figure 5. Well location map of the Teapot Dome Field: Spatial distribution of key wells (48-X-28, 71-1-X-4, 67-1-TPX-10, and 25-1-X-14) overlaid on seismic time slice at the Teapot Dome Field. White circles indicate the well locations.
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Figure 6. (a) Velocity points (blue dots) provided by the processing center; (b) model skeleton; (c) interpreted horizons; (d) final velocity model used for time-to-depth conversion. The green arrow indicates the north direction in the 3D view.
Figure 6. (a) Velocity points (blue dots) provided by the processing center; (b) model skeleton; (c) interpreted horizons; (d) final velocity model used for time-to-depth conversion. The green arrow indicates the north direction in the 3D view.
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Figure 7. 3D structural model of the Teapot Dome Field: Visual representation of segmented geological zones and layers. The green arrow indicates the north direction in the 3D view.
Figure 7. 3D structural model of the Teapot Dome Field: Visual representation of segmented geological zones and layers. The green arrow indicates the north direction in the 3D view.
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Figure 8. Seismic 3D cross line (X-line 94) with interpretation of the horizons.
Figure 8. Seismic 3D cross line (X-line 94) with interpretation of the horizons.
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Figure 9. Fracture set distribution across wells: Polar plots showing fracture orientation and distribution for individual wells and a combined view of all wells.
Figure 9. Fracture set distribution across wells: Polar plots showing fracture orientation and distribution for individual wells and a combined view of all wells.
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Figure 10. Artificial neural network architecture for secondary porosity prediction.
Figure 10. Artificial neural network architecture for secondary porosity prediction.
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Figure 11. The estimated secondary porosity log is well matched with the original porosity log in the validation well (67-1-TP-10). The black line in the last track is the calculated secondary porosity, and the light blue line is the one predicted by the ANN model.
Figure 11. The estimated secondary porosity log is well matched with the original porosity log in the validation well (67-1-TP-10). The black line in the last track is the calculated secondary porosity, and the light blue line is the one predicted by the ANN model.
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Figure 12. Artificial neural network architecture for fracture density prediction.
Figure 12. Artificial neural network architecture for fracture density prediction.
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Figure 13. The estimated fracture density log closely aligns with the original fracture density log in the validation well, denoted as 25-1-X-14. In the final track, the black line represents the computed fracture density, while the light blue line represents the fracture density predicted by the Artificial Neural Network (ANN) model.
Figure 13. The estimated fracture density log closely aligns with the original fracture density log in the validation well, denoted as 25-1-X-14. In the final track, the black line represents the computed fracture density, while the light blue line represents the fracture density predicted by the Artificial Neural Network (ANN) model.
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Figure 14. Average error relative to the number of seismic attributes selected, indicating optimal performance at 15 attributes.
Figure 14. Average error relative to the number of seismic attributes selected, indicating optimal performance at 15 attributes.
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Figure 15. Actual vs. predicted fracture intensity using 15 attributes. Data points are color-coded by well, and the red line represents the regression trend. The model achieves a cross-correlation of 0.93 and an error of 0.49, indicating strong predictive performance.
Figure 15. Actual vs. predicted fracture intensity using 15 attributes. Data points are color-coded by well, and the red line represents the regression trend. The model achieves a cross-correlation of 0.93 and an error of 0.49, indicating strong predictive performance.
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Figure 16. Validation of operator length in PNN model.
Figure 16. Validation of operator length in PNN model.
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Figure 17. Cross-sectional view of the reservoir showing the spatial distribution of fracture intensity.
Figure 17. Cross-sectional view of the reservoir showing the spatial distribution of fracture intensity.
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Figure 18. Discrete Fracture Network (DFN) Model: 3D representation of fracture sets within the Tensleep Formation, with color-coded fracture classes (Code 1 to Code 4) indicating varying fracture orientations and intensities. The inset provides a zoomed-in view of the fracture patterns for clarity. The green arrow indicates the north direction in the 3D view.
Figure 18. Discrete Fracture Network (DFN) Model: 3D representation of fracture sets within the Tensleep Formation, with color-coded fracture classes (Code 1 to Code 4) indicating varying fracture orientations and intensities. The inset provides a zoomed-in view of the fracture patterns for clarity. The green arrow indicates the north direction in the 3D view.
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Table 1. Statistical distribution parameters for the main geometric properties.
Table 1. Statistical distribution parameters for the main geometric properties.
ParameterDistribution TypeExponent/MeanRange
Fracture LengthPower Law α = 2.10–500 m
Fracture ApertureNormal0.002270.00002–0.016 mm
Fracture OrientationGaussian69°0–90°
Table 2. Seismic attributes with their physical meaning.
Table 2. Seismic attributes with their physical meaning.
AttributePhysical Meaning
1(Curvature)2Squared curvature emphasizes zones of strong bending in reflectors, highlighting fracture-prone areas
2Amplitude-Weighted Phase (Curvature)Combines reflector amplitude with phase information, useful for identifying subtle fracture-related changes in wavelet shape.
3Instantaneous Phase (Curvature)Shows the phase angle of the seismic trace at each time, independent of amplitude, highlights continuity and structural features.
4Integrated Absolute Amplitude (Curvature)Measures cumulative energy of reflections; higher values may indicate fracture zones with strong scattering.
5Filter 15/20–25/30 (Curvature)Bandpass filter isolating specific frequency ranges; helps detect fractures that resonate at certain scales.
6Filter 45/50–55/60 (Curvature)Higher-frequency bandpass filter enhances small-scale fracture features.
7Integrate (Curvature)Cumulative measure of curvature across a window; highlights broader structural bending linked to fracture networks.
8Instantaneous Frequency (Curvature)Local frequency of seismic signal; sensitive to changes in lithology and fracture density.
9Apparent Polarity (Curvature)Indicates whether reflections are positive or negative; polarity reversals can be linked to fracture-related fluid changes.
10Integrate (Ant tracking)Summed ant tracking values; highlights continuous fracture corridors detected by ant tracking algorithms.
11Amplitude-Weighted Frequency (Ant tracking)Frequency attribute weighted by amplitude; emphasizes fracture zones with strong seismic responses.
12Average Frequency (Curvature)Mean frequency over a window; lower values may indicate attenuation due to fracturing.
13Y-Coordinate (Curvature)Spatial reference attribute; used to correlate fracture intensity with geographic position.
14Cosine Instantaneous Phase (Ant tracking)Cosine transform of phase; enhances subtle phase variations linked to fracture orientation.
15Derivative (Curvature)Rate of change in curvature; sharp changes often correspond to fracture edges or fault boundaries.
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MDPI and ACS Style

Ahmed, I.; Hamada, G.; Dahab, A.S. Machine Learning Workflow for Fracture Modeling in the Tensleep Reservoir. Energies 2026, 19, 1683. https://doi.org/10.3390/en19071683

AMA Style

Ahmed I, Hamada G, Dahab AS. Machine Learning Workflow for Fracture Modeling in the Tensleep Reservoir. Energies. 2026; 19(7):1683. https://doi.org/10.3390/en19071683

Chicago/Turabian Style

Ahmed, Israa, Gharib Hamada, and Abdel Sattar Dahab. 2026. "Machine Learning Workflow for Fracture Modeling in the Tensleep Reservoir" Energies 19, no. 7: 1683. https://doi.org/10.3390/en19071683

APA Style

Ahmed, I., Hamada, G., & Dahab, A. S. (2026). Machine Learning Workflow for Fracture Modeling in the Tensleep Reservoir. Energies, 19(7), 1683. https://doi.org/10.3390/en19071683

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