Interactions between Surface Processes, Tectonics and Mantle Dynamics in the Evolution of Topography

A special issue of Geosciences (ISSN 2076-3263).

Deadline for manuscript submissions: closed (30 September 2019) | Viewed by 9481

Special Issue Editor


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Guest Editor
Sciences Department, Roma Tre University, Largo San Leonardo Murialdo, 1, 00146 Rome, Italy
Interests: tectonic geomorphology; topography; rivers; mountain chains; continental rift; landscape evolution

Special Issue Information

Dear Colleagues,

Topography is the integrated result of processes that operate from the depths of the Earth up to its surface, at different time and at different spatial scales. Its "life cycle" starts with tectonics that generate topographic contrasts and set up the boundary conditions for geomorphological processes. Ruled by climate, these latter respond to the tectonic input redistributing rocks via erosion, transport, and sedimentation. These processes load and unload the underlying crust and mantle lithosphere, becoming a forcing factor of tectonics.

In different geodynamic contests, in addition to crustal and subcrustal processes, density variations in the mantle produce flows that generate the so-called dynamic topography. Downward, convergent flows induce the formation of a surface depression (negative dynamic topography), while an upward, divergent flow a positive dynamic topography. The wavelength and height of this peculiar topographic signal is proportional to the intensity, depth and scale of the flow.

In synthesis, to investigate the generation and the evolution of the Earth's topography, and to discern/quantify the different components that contribute to its geometry, is a task that needs many expertises: Geomorphology and Quaternary Geology, Structural Geology, Geophysics, Analogue and Numerical Modeling of processes.

Therefore, I would like to invite you to submit papers about your recent work on topography from local to regional scales, as a result of the interaction of exogenic and endogenic processes, acting from the surface down to the mantle. This Special Issue is an opportunity to combine different approaches in the research of topography generation and evolution.

Prof. Paola Molin
Guest Editor

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Keywords

  • topography
  • geomorphology
  • surface processes
  • tectonics
  • crustal and subcrustal processes
  • mantle flows and dynamic topography
  • geophysics
  • analogue and numerical modeling

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Published Papers (2 papers)

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Research

13 pages, 4788 KiB  
Article
Evidence of Segmentation in the Iberia–Africa Plate Boundary: A Jurassic Heritage?
by Manel Fernàndez, Montserrat Torne, Jaume Vergés, Emilio Casciello and Chiara Macchiavelli
Geosciences 2019, 9(8), 343; https://doi.org/10.3390/geosciences9080343 - 7 Aug 2019
Cited by 19 | Viewed by 4785
Abstract
The present structure of the Iberia–Africa plate boundary between the Gorringe Bank and the Algerian Basin is characterized by a highly segmented geometry and diffused seismicity. Filtered Bouguer gravity data show conspicuous highs coinciding with the Gorringe Bank, the Guadalquivir–Portimao Bank, and the [...] Read more.
The present structure of the Iberia–Africa plate boundary between the Gorringe Bank and the Algerian Basin is characterized by a highly segmented geometry and diffused seismicity. Filtered Bouguer gravity data show conspicuous highs coinciding with the Gorringe Bank, the Guadalquivir–Portimao Bank, and the Ronda/Beni–Bousera massifs, reflecting the current geometry of the plate boundary segments. The Africa–Eurasia Alpine convergence produced crustal-scale thrusting in the Atlantic segments and roll-back subduction in the Ligurian–Tethys segments. Despite the growing consensus that the Gorringe and the Guadalquivir–Portimao Banks resulted from tectonic inversion of hyperextended margin structures inherited from the Early Jurassic, this heritage is more debatable for the Ronda/Beni–Bousera massifs lacking models linking the Atlantic and Mediterranean realms. On the basis of gravity analysis combined with plate reconstruction models, geological cross-sections, and recent local tomography, we infer a strong Jurassic heritage of the present-day segmentation and substantiate a comprehensive tectonic evolution model of the Iberia–Africa plate boundary since the Early Jurassic to Recent that includes the Atlantic and the Mediterranean domains. Full article
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14 pages, 2276 KiB  
Article
Eocene Origin of Owens Valley, California
by Francis J. Sousa
Geosciences 2019, 9(5), 194; https://doi.org/10.3390/geosciences9050194 - 28 Apr 2019
Cited by 5 | Viewed by 4164
Abstract
Bedrock (U-Th)/He data reveal an Eocene exhumation difference greater than four kilometers athwart Owens Valley, California near the Alabama Hills. This difference is localized at the eastern fault-bound edge of the valley between the Owens Valley Fault and the Inyo-White Mountains Fault. Time-temperature [...] Read more.
Bedrock (U-Th)/He data reveal an Eocene exhumation difference greater than four kilometers athwart Owens Valley, California near the Alabama Hills. This difference is localized at the eastern fault-bound edge of the valley between the Owens Valley Fault and the Inyo-White Mountains Fault. Time-temperature modeling of published data reveal a major phase of tectonic activity from 55 to 50 Ma that was of a magnitude equivalent to the total modern bedrock relief of Owens Valley. Exhumation was likely accommodated by one or both of the Owens Valley and Inyo-White Mountains faults, requiring an Eocene structural origin of Owens Valley 30 to 40 million years earlier than previously estimated. This analysis highlights the importance of constraining the initial and boundary conditions of geologic models and exemplifies that this task becomes increasingly difficult deeper in geologic time. Full article
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