Potentially active faults in central Mongolia

<p> The activity of the Ereen Uul fault and the Sanglin Dalai Nurr fault in central Mongolia has not been studied in detail. The Erren Uul fault is a normal fault located 45 km southeast from Harhorin and the Sanglin Dalai Nurr fault is a right-lateral strike-slip fault located 30 km south of...

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Main Author: Guiltinan, Tiffany
Language:EN
Published: California State University, Long Beach 2015
Subjects:
Online Access:http://pqdtopen.proquest.com/#viewpdf?dispub=1584413
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spelling ndltd-PROQUEST-oai-pqdtoai.proquest.com-15844132015-03-05T04:00:58Z Potentially active faults in central Mongolia Guiltinan, Tiffany Geology <p> The activity of the Ereen Uul fault and the Sanglin Dalai Nurr fault in central Mongolia has not been studied in detail. The Erren Uul fault is a normal fault located 45 km southeast from Harhorin and the Sanglin Dalai Nurr fault is a right-lateral strike-slip fault located 30 km south of Harhorin next to the Hangay Mountains. Remote sensing and field observations were used to refine a map by the Mongolian Geologic Survey at a scale of 1:1,000,000 to a scale of 1:100,000. This new map covers an area of 8,072 km<sup>2 </sup>. The basin asymmetry factor, stream length-gradient index, and hypsometric curves were developed for basins adjacent to these faults. These geomorphic indices along with the refined map were used to conclude that the Ereen Uul and Sanglin Dalai Nurr faults are active.</p> California State University, Long Beach 2015-03-03 00:00:00.0 thesis http://pqdtopen.proquest.com/#viewpdf?dispub=1584413 EN
collection NDLTD
language EN
sources NDLTD
topic Geology
spellingShingle Geology
Guiltinan, Tiffany
Potentially active faults in central Mongolia
description <p> The activity of the Ereen Uul fault and the Sanglin Dalai Nurr fault in central Mongolia has not been studied in detail. The Erren Uul fault is a normal fault located 45 km southeast from Harhorin and the Sanglin Dalai Nurr fault is a right-lateral strike-slip fault located 30 km south of Harhorin next to the Hangay Mountains. Remote sensing and field observations were used to refine a map by the Mongolian Geologic Survey at a scale of 1:1,000,000 to a scale of 1:100,000. This new map covers an area of 8,072 km<sup>2 </sup>. The basin asymmetry factor, stream length-gradient index, and hypsometric curves were developed for basins adjacent to these faults. These geomorphic indices along with the refined map were used to conclude that the Ereen Uul and Sanglin Dalai Nurr faults are active.</p>
author Guiltinan, Tiffany
author_facet Guiltinan, Tiffany
author_sort Guiltinan, Tiffany
title Potentially active faults in central Mongolia
title_short Potentially active faults in central Mongolia
title_full Potentially active faults in central Mongolia
title_fullStr Potentially active faults in central Mongolia
title_full_unstemmed Potentially active faults in central Mongolia
title_sort potentially active faults in central mongolia
publisher California State University, Long Beach
publishDate 2015
url http://pqdtopen.proquest.com/#viewpdf?dispub=1584413
work_keys_str_mv AT guiltinantiffany potentiallyactivefaultsincentralmongolia
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