Arcuate Pamir in the Paleogene? Insights from a review of stratigraphy and sedimentology of the basin fills in the foreland of NE Chinese Pamir, western Tarim Basin
Autor: | Yao Zhang, Fengqi Zhang, Jiakai Yan, Junfeng Gong, Lei Wu, Shenqiang Chen, Xiaogan Cheng, Xiubin Lin, Weiwei Ding, Rong Yang, Xinwei Chen, Hanlin Chen |
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Rok vydání: | 2018 |
Předmět: |
010504 meteorology & atmospheric sciences
Subduction Context (language use) 010502 geochemistry & geophysics 01 natural sciences Conglomerate Paleontology Stratigraphy Facies General Earth and Planetary Sciences Sedimentology Paleogene Foreland basin Geology 0105 earth and related environmental sciences |
Zdroj: | Earth-Science Reviews. 180:1-16 |
ISSN: | 0012-8252 |
DOI: | 10.1016/j.earscirev.2018.03.003 |
Popis: | The tectonic evolution of the Pamir bears essential information for understanding intracontinental tectonic processes within the context of India-Asia convergence. However, it is unclear whether the arcuate shape of the Pamir is entirely the result of the India-Asia collision, or may have been in part an inherited, pre-Cenozoic feature. In this study, we address the evolution of the NE Chinese Pamir during the Paleogene by reviewing the stratigraphy of twelve sections in the western Tarim Basin and the establishment of sedimentary facies. The results indicate three episodes of deposition of alluvial coarse sediments in the foreland regions of NE Chinese Pamir during the (1) early Paleocene, (2) late Paleocene to early Eocene and (3) middle Eocene to Oligocene, respectively. These are correspondingly attributed to (1) retroarc deformation in an Andean-type margin of the southern Asia during subduction of the Neo-Tethys Ocean, (2) the immediate response in the Pamir to the India-Asia collision, and (3) continued India-Asia convergence. The alluvial conglomerates with grain-size up to 5–10 cm, imply a transport distance |
Databáze: | OpenAIRE |
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