Late-Miocene thrust fault-related folding in the northern Tibetan Plateau: Insight from paleomagnetic and structural analyses of the Kumkol basin

Late-Miocene thrust fault-related folding in the northern Tibetan Plateau: Insight from... Journal of Asian Earth Sciences 156 (2018) 246–255 Contents lists available at ScienceDirect Journal of Asian Earth Sciences journal homepage: www.elsevier.com/locate/jseaes Late-Miocene thrust fault-related folding in the northern Tibetan Plateau: Insight from paleomagnetic and structural analyses of the Kumkol basin a,b, c c c a,b Haijian Lu , Bihong Fu , Pilong Shi , Guoliang Xue , Haibing Li Key Laboratory of Deep Earth Dynamics, Beijing 100037, China Institute of Geology, Chinese Academy of Geological Sciences, Baiwanzhuang Road #26, Beijing 100037, China Institute of Remote Sensing and Digital Earth, Chinese Academy of Sciences, Dengzhuang South Road #9, Beijing 100094, China ARTICLE I NFO ABSTRACT Keywords: Constraints on the timing and style of the Tibetan Plateau growth help spur new understanding of the tectonic Magnetostratigraphy evolution of the northern Tibetan Plateau and its relation to the India-Asia continental collision. In this regard, Growth strata records of tectonic deformation with accurate ages are urgently needed, especially in regions without relevant Late Miocene studies. The Kumkol basin, located between two major intermontane basins (the Hoh Xil and Qaidam basins), Kumkol basin may hold clues to how these major basins evolve during the Cenozoic. However, little has been known about the The northern http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Journal of Asian Earth Sciences Elsevier

Late-Miocene thrust fault-related folding in the northern Tibetan Plateau: Insight from paleomagnetic and structural analyses of the Kumkol basin

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Publisher
Elsevier
Copyright
Copyright © 2018 Elsevier Ltd
ISSN
1367-9120
eISSN
1878-5786
D.O.I.
10.1016/j.jseaes.2018.01.026
Publisher site
See Article on Publisher Site

Abstract

Journal of Asian Earth Sciences 156 (2018) 246–255 Contents lists available at ScienceDirect Journal of Asian Earth Sciences journal homepage: www.elsevier.com/locate/jseaes Late-Miocene thrust fault-related folding in the northern Tibetan Plateau: Insight from paleomagnetic and structural analyses of the Kumkol basin a,b, c c c a,b Haijian Lu , Bihong Fu , Pilong Shi , Guoliang Xue , Haibing Li Key Laboratory of Deep Earth Dynamics, Beijing 100037, China Institute of Geology, Chinese Academy of Geological Sciences, Baiwanzhuang Road #26, Beijing 100037, China Institute of Remote Sensing and Digital Earth, Chinese Academy of Sciences, Dengzhuang South Road #9, Beijing 100094, China ARTICLE I NFO ABSTRACT Keywords: Constraints on the timing and style of the Tibetan Plateau growth help spur new understanding of the tectonic Magnetostratigraphy evolution of the northern Tibetan Plateau and its relation to the India-Asia continental collision. In this regard, Growth strata records of tectonic deformation with accurate ages are urgently needed, especially in regions without relevant Late Miocene studies. The Kumkol basin, located between two major intermontane basins (the Hoh Xil and Qaidam basins), Kumkol basin may hold clues to how these major basins evolve during the Cenozoic. However, little has been known about the The northern

Journal

Journal of Asian Earth SciencesElsevier

Published: May 1, 2018

References

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