Active deformation of the Shargyn Basin, a transpressional strike-slip intersection in western Mongolia

Thesis: S.B., Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2013.

Bibliographic Details
Main Author: Thompson, Thomas Ben
Other Authors: Oliver Jagoutz.
Format: Thesis
Language:eng
Published: Massachusetts Institute of Technology 2018
Subjects:
Online Access:http://hdl.handle.net/1721.1/114129
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author Thompson, Thomas Ben
author2 Oliver Jagoutz.
author_facet Oliver Jagoutz.
Thompson, Thomas Ben
author_sort Thompson, Thomas Ben
collection MIT
description Thesis: S.B., Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2013.
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spelling mit-1721.1/1141292019-04-11T05:13:10Z Active deformation of the Shargyn Basin, a transpressional strike-slip intersection in western Mongolia Thompson, Thomas Ben Oliver Jagoutz. Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences. Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences. Earth, Atmospheric, and Planetary Sciences. Thesis: S.B., Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2013. "June 2013." Cataloged from PDF version of thesis. Includes bibliographical references (pages 37-41). Intraplate faulting in central Asia is a major component of the Indo-Eurasian collision. The kinematics and mechanisms of intraplate deformation are important in understanding broad active tectonic patterns, reconstructing past tectonics, analyzing seismic hazard and identifying potential resources. We examine the fault kinematics surrounding the 150 km wide Shargyn Basin at the intersection of the left-lateral transpressional Gobi-Altai fault system and the right-lateral transpressional Altai fault system. The studies were performed using satellite data and targeted field transects. The results suggest the Shargyn basin is formed by a compressional stepover, an uplifted wedge from the intersecting strike-slip systems and many strike-slip terminating thrust splays. Furthermore, local foliation is almost always fault parallel, pointing to the importance of pre-existing structural weaknesses in the development of active faults. This research demonstrates some of the potential kinematics for intraplate transpressional orogenies and emphasizes the importance of pre-existing crustal structure in the development of active faults. by Thomas Ben Thompson. S.B. 2018-03-12T19:31:06Z 2018-03-12T19:31:06Z 2013 Thesis http://hdl.handle.net/1721.1/114129 1027723880 eng MIT theses are protected by copyright. They may be viewed, downloaded, or printed from this source but further reproduction or distribution in any format is prohibited without written permission. http://dspace.mit.edu/handle/1721.1/7582 41 pages application/pdf a-mp--- Massachusetts Institute of Technology
spellingShingle Earth, Atmospheric, and Planetary Sciences.
Thompson, Thomas Ben
Active deformation of the Shargyn Basin, a transpressional strike-slip intersection in western Mongolia
title Active deformation of the Shargyn Basin, a transpressional strike-slip intersection in western Mongolia
title_full Active deformation of the Shargyn Basin, a transpressional strike-slip intersection in western Mongolia
title_fullStr Active deformation of the Shargyn Basin, a transpressional strike-slip intersection in western Mongolia
title_full_unstemmed Active deformation of the Shargyn Basin, a transpressional strike-slip intersection in western Mongolia
title_short Active deformation of the Shargyn Basin, a transpressional strike-slip intersection in western Mongolia
title_sort active deformation of the shargyn basin a transpressional strike slip intersection in western mongolia
topic Earth, Atmospheric, and Planetary Sciences.
url http://hdl.handle.net/1721.1/114129
work_keys_str_mv AT thompsonthomasben activedeformationoftheshargynbasinatranspressionalstrikeslipintersectioninwesternmongolia