End Late Paleozoic tectonic stress field in the southern edge of Junggar Basin

This paper presents the end Late Paleozoic tectonic stress field in the southern edge of Junggar Basin by interpreting stress-response structures (dykes, folds, faults with slickenside and conjugate joints). The direction of the maximum principal stress axes is interpreted to be NW–SE (about 325°),...

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Main Authors: Wei Ju, Guiting Hou, Le Li, Fangfeng Xiao
Format: Article
Language:English
Published: Elsevier 2012-09-01
Series:Geoscience Frontiers
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674987111001368
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spelling doaj-3771d72edd0a404184ce7098b6335bd92020-11-24T22:48:13ZengElsevierGeoscience Frontiers1674-98712012-09-013570771510.1016/j.gsf.2011.12.007End Late Paleozoic tectonic stress field in the southern edge of Junggar BasinWei Ju0Guiting Hou1Le Li2Fangfeng Xiao3The Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Science, Peking University, Beijing 100871, ChinaThe Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Science, Peking University, Beijing 100871, ChinaThe Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Science, Peking University, Beijing 100871, ChinaThe Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Science, Peking University, Beijing 100871, ChinaThis paper presents the end Late Paleozoic tectonic stress field in the southern edge of Junggar Basin by interpreting stress-response structures (dykes, folds, faults with slickenside and conjugate joints). The direction of the maximum principal stress axes is interpreted to be NW–SE (about 325°), and the accommodated motion among plates is assigned as the driving force of this tectonic stress field. The average value of the stress index R′ is about 2.09, which indicates a variation from strike-slip to compressive tectonic stress regime in the study area during the end Late Paleozoic period. The reconstruction of the tectonic field in the southern edge of Junggar Basin provides insights into the tectonic deformation processes around the southern Junggar Basin and contributes to the further understanding of basin evolution and tectonic settings during the culmination of the Paleozoic.http://www.sciencedirect.com/science/article/pii/S1674987111001368Tectonic stress fieldJunggar BasinEnd Late PaleozoicStress-response structuresStress regime
collection DOAJ
language English
format Article
sources DOAJ
author Wei Ju
Guiting Hou
Le Li
Fangfeng Xiao
spellingShingle Wei Ju
Guiting Hou
Le Li
Fangfeng Xiao
End Late Paleozoic tectonic stress field in the southern edge of Junggar Basin
Geoscience Frontiers
Tectonic stress field
Junggar Basin
End Late Paleozoic
Stress-response structures
Stress regime
author_facet Wei Ju
Guiting Hou
Le Li
Fangfeng Xiao
author_sort Wei Ju
title End Late Paleozoic tectonic stress field in the southern edge of Junggar Basin
title_short End Late Paleozoic tectonic stress field in the southern edge of Junggar Basin
title_full End Late Paleozoic tectonic stress field in the southern edge of Junggar Basin
title_fullStr End Late Paleozoic tectonic stress field in the southern edge of Junggar Basin
title_full_unstemmed End Late Paleozoic tectonic stress field in the southern edge of Junggar Basin
title_sort end late paleozoic tectonic stress field in the southern edge of junggar basin
publisher Elsevier
series Geoscience Frontiers
issn 1674-9871
publishDate 2012-09-01
description This paper presents the end Late Paleozoic tectonic stress field in the southern edge of Junggar Basin by interpreting stress-response structures (dykes, folds, faults with slickenside and conjugate joints). The direction of the maximum principal stress axes is interpreted to be NW–SE (about 325°), and the accommodated motion among plates is assigned as the driving force of this tectonic stress field. The average value of the stress index R′ is about 2.09, which indicates a variation from strike-slip to compressive tectonic stress regime in the study area during the end Late Paleozoic period. The reconstruction of the tectonic field in the southern edge of Junggar Basin provides insights into the tectonic deformation processes around the southern Junggar Basin and contributes to the further understanding of basin evolution and tectonic settings during the culmination of the Paleozoic.
topic Tectonic stress field
Junggar Basin
End Late Paleozoic
Stress-response structures
Stress regime
url http://www.sciencedirect.com/science/article/pii/S1674987111001368
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AT fangfengxiao endlatepaleozoictectonicstressfieldinthesouthernedgeofjunggarbasin
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