Tectonic geomorphology of the eastern extent of the Kashmir Basin Fault (KBF) zone

The Kashmir Basin Fault (KBF) is exposed as a train of discontinuous active fault traces for a strike length of ~120 km (Shah, 2013), in Kashmir, Himalayas. However, its eastern extent was not mapped previously and therefore, this study demonstrates that the active fault trace extends further east,...

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Main Author: Shah, Afroz Ahmad
Other Authors: Christoph Grützner
Format: Conference Paper
Published: Grützner & Reicherter Geosolutions UG (haftungsbeschränkt) Schönrathstraße 68, 52066 Aachen, Germany http://www.gr-geo.com 2013
Subjects:
Online Access:http://hdl.handle.net/20.500.11937/15839
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author Shah, Afroz Ahmad
author2 Christoph Grützner
author_facet Christoph Grützner
Shah, Afroz Ahmad
author_sort Shah, Afroz Ahmad
building Curtin Institutional Repository
collection Online Access
description The Kashmir Basin Fault (KBF) is exposed as a train of discontinuous active fault traces for a strike length of ~120 km (Shah, 2013), in Kashmir, Himalayas. However, its eastern extent was not mapped previously and therefore, this study demonstrates that the active fault trace extends further east, where the geomorphic expression of active faulting is clear for a distance of ~43 km. The fault shows a very prominent dextral strike-slip motion with little to no dip-slip component associated with it, particularly, on the easternmost portion. Further west it mainly shows dip-slip motion with a slight indication of dextral strike-slip. This new active fault trace extends the total strike length of the KBF zone to ~163 km, which has implications for seismic hazard and the distribution of deformation along the NW portion of the Himalayas.
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spelling curtin-20.500.11937-158392023-02-07T08:01:25Z Tectonic geomorphology of the eastern extent of the Kashmir Basin Fault (KBF) zone Shah, Afroz Ahmad Christoph Grützner Andreas Rudersdorf Klaus Reicherter NW Himalayas Kashmir Basin Fault Active faults Distributed deformation The Kashmir Basin Fault (KBF) is exposed as a train of discontinuous active fault traces for a strike length of ~120 km (Shah, 2013), in Kashmir, Himalayas. However, its eastern extent was not mapped previously and therefore, this study demonstrates that the active fault trace extends further east, where the geomorphic expression of active faulting is clear for a distance of ~43 km. The fault shows a very prominent dextral strike-slip motion with little to no dip-slip component associated with it, particularly, on the easternmost portion. Further west it mainly shows dip-slip motion with a slight indication of dextral strike-slip. This new active fault trace extends the total strike length of the KBF zone to ~163 km, which has implications for seismic hazard and the distribution of deformation along the NW portion of the Himalayas. 2013 Conference Paper http://hdl.handle.net/20.500.11937/15839 Grützner & Reicherter Geosolutions UG (haftungsbeschränkt) Schönrathstraße 68, 52066 Aachen, Germany http://www.gr-geo.com fulltext
spellingShingle NW Himalayas
Kashmir Basin Fault
Active faults
Distributed deformation
Shah, Afroz Ahmad
Tectonic geomorphology of the eastern extent of the Kashmir Basin Fault (KBF) zone
title Tectonic geomorphology of the eastern extent of the Kashmir Basin Fault (KBF) zone
title_full Tectonic geomorphology of the eastern extent of the Kashmir Basin Fault (KBF) zone
title_fullStr Tectonic geomorphology of the eastern extent of the Kashmir Basin Fault (KBF) zone
title_full_unstemmed Tectonic geomorphology of the eastern extent of the Kashmir Basin Fault (KBF) zone
title_short Tectonic geomorphology of the eastern extent of the Kashmir Basin Fault (KBF) zone
title_sort tectonic geomorphology of the eastern extent of the kashmir basin fault (kbf) zone
topic NW Himalayas
Kashmir Basin Fault
Active faults
Distributed deformation
url http://hdl.handle.net/20.500.11937/15839