Next Article in Journal
Comparative Tests of Partial Discharges in Nomex® 910 Paper and Cellulose Paper
Next Article in Special Issue
Effect of Pore Size Heterogeneity on Hydrocarbon Fluid Distribution, Transport, and Primary and Secondary Recovery in Nano-Porous Media
Previous Article in Journal
Effect of Impeller Design on Power Characteristics and Newtonian Fluids Mixing Efficiency in a Mechanically Agitated Vessel at Low Reynolds Numbers
Open AccessArticle

Controls on Reservoirs Quality of the Upper Jurassic Mengyin Formation Sandstones in Dongying Depression, Bohai Bay Basin, Eastern China

by Shaochun Yang 1,2,*, Ya Wang 1,2,*, Shiqi Zhang 1,2, Yongchao Wang 1,2, Yifan Zhang 1,2 and Yongfu Zhao 1,3
School of Geosciences, China University of Petroleum, Qingdao 266580, China
Key Laboratory of Deep Oil and Gas, China University of Petroleum (East China), Qingdao 266580, China
Management Center of Oil and Gas Exploration, SINOPEC Shengli Oilfield, Dongying 257017, China
Authors to whom correspondence should be addressed.
Energies 2020, 13(3), 646;
Received: 10 January 2020 / Revised: 29 January 2020 / Accepted: 30 January 2020 / Published: 3 February 2020
(This article belongs to the Special Issue Investigation of Mechanisms Responsible for Enhanced Oil Recovery)
The Upper Jurassic Mengyin Formation sandstones are important targets for petroleum exploration in Dongying Depression of Bohai Bay Basin, Eastern China. Although the current burial depth of the Upper Jurassic Mengyin Formation sandstones is shallow (900–2500 m), the reservoir rocks are characterized by low porosity and low permeability due to the complex diagenetic modifications after deposition. Experimental tests and statistical methods, such as thin section, scanning electron microscopy (SEM), cathodoluminescence (CL), high pressure mercury injection (HPMI) and fluid inclusion analysis are conducted to delineate the mineralogical, petrographic and petro-physical characteristics. Results show that physical and chemical processes, including burial depth, burial and thermal history and pore fluid evolution, are both important for the diagenetic modifications that result in a variety changes in pore system and reservoir quality. According to numerical simulation of porosity evolution during lengthy burial and thermal history, porosity loss due to the early deep burial process under the high paleo-geothermal gradient can reach about 20%. Moreover, the burial history (effective stress and temperature) has a better guidance to reservoir quality prediction compared with current burial depth. The extensive compaction in sandstones also resulted in extremely low pore fluid flow during subsequent diagenetic processes, thus, the reaction products of dissolution cannot be removed, which would be precipitated as carbonate cements during stable reburial phase. Dissolution resulted from uncomformity-related meteoric flushing have been the most important porosity-enhancing factor in Mengyin Formation sandstones in spite of low thin section porosity averaged out to 3.22%. Secondary pores derived from dissolution of unstable silicates are more likely to develop in sandstones near the regional unconformity. The oil source fault activities may enhance the heterogeneity of reservoir rocks and control the reservoir quality by inducing micro-fractures and providing the main pathways for hydrocarbon migration. View Full-Text
Keywords: reservoir quality; diagenesis; numerical simulation; uncomformity; meteoric flushing reservoir quality; diagenesis; numerical simulation; uncomformity; meteoric flushing
Show Figures

Figure 1

MDPI and ACS Style

Yang, S.; Wang, Y.; Zhang, S.; Wang, Y.; Zhang, Y.; Zhao, Y. Controls on Reservoirs Quality of the Upper Jurassic Mengyin Formation Sandstones in Dongying Depression, Bohai Bay Basin, Eastern China. Energies 2020, 13, 646.

Show more citation formats Show less citations formats
Note that from the first issue of 2016, MDPI journals use article numbers instead of page numbers. See further details here.

Article Access Map by Country/Region

Search more from Scilit
Back to TopTop