Reinterpretation of the active faulting in central Mongolia

We present remote-sensing and field observations of an ∼350-km-long east-west left-lateral strike-slip fault (the South Hangay fault) in the Hangay Mountains of central Mongolia, an area previously believed to be deforming solely by slip on scattered, and randomly oriented, normal faults. The known...

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Main Authors: Walker, RT, Nissen, E, Molor, E, Bayasgalan, A
Format: Journal article
Language:English
Published: 2007
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author Walker, RT
Nissen, E
Molor, E
Bayasgalan, A
author_facet Walker, RT
Nissen, E
Molor, E
Bayasgalan, A
author_sort Walker, RT
collection OXFORD
description We present remote-sensing and field observations of an ∼350-km-long east-west left-lateral strike-slip fault (the South Hangay fault) in the Hangay Mountains of central Mongolia, an area previously believed to be deforming solely by slip on scattered, and randomly oriented, normal faults. The known dip-slip faults are shown to be short segments introduced at bends in the much longer strike-slip fault Our observations show that the active faulting in the Hangay Mountains is consistent with the regional strain field of Mongolia and does not require, as suggested in other studies, that the faults result from stresses introduced by the locally elevated topography. Our observations help to define the active tectonics of this important part of the India-Eurasia collision. The South Hangay strike-slip fault is a potential source of large-magnitude earthquakes and constitutes a previously unrecognized hazard in this part of Mongolia. © 2007 The Geological Society of America.
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spelling oxford-uuid:244299bf-916b-4152-a006-71ca752b6a402022-03-26T11:49:02ZReinterpretation of the active faulting in central MongoliaJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:244299bf-916b-4152-a006-71ca752b6a40EnglishSymplectic Elements at Oxford2007Walker, RTNissen, EMolor, EBayasgalan, AWe present remote-sensing and field observations of an ∼350-km-long east-west left-lateral strike-slip fault (the South Hangay fault) in the Hangay Mountains of central Mongolia, an area previously believed to be deforming solely by slip on scattered, and randomly oriented, normal faults. The known dip-slip faults are shown to be short segments introduced at bends in the much longer strike-slip fault Our observations show that the active faulting in the Hangay Mountains is consistent with the regional strain field of Mongolia and does not require, as suggested in other studies, that the faults result from stresses introduced by the locally elevated topography. Our observations help to define the active tectonics of this important part of the India-Eurasia collision. The South Hangay strike-slip fault is a potential source of large-magnitude earthquakes and constitutes a previously unrecognized hazard in this part of Mongolia. © 2007 The Geological Society of America.
spellingShingle Walker, RT
Nissen, E
Molor, E
Bayasgalan, A
Reinterpretation of the active faulting in central Mongolia
title Reinterpretation of the active faulting in central Mongolia
title_full Reinterpretation of the active faulting in central Mongolia
title_fullStr Reinterpretation of the active faulting in central Mongolia
title_full_unstemmed Reinterpretation of the active faulting in central Mongolia
title_short Reinterpretation of the active faulting in central Mongolia
title_sort reinterpretation of the active faulting in central mongolia
work_keys_str_mv AT walkerrt reinterpretationoftheactivefaultingincentralmongolia
AT nissene reinterpretationoftheactivefaultingincentralmongolia
AT molore reinterpretationoftheactivefaultingincentralmongolia
AT bayasgalana reinterpretationoftheactivefaultingincentralmongolia