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DOI | 10.1016/j.jseaes.2008.01.005 |
Gangdese retroarc thrust belt and foreland basin deposits in the Damxung area, southern Tibet | |
Pullen, Alex; Kapp, Paul; Gehrels, George E.; DeCelles, Peter G.; Brown, Edwin H.; Fabijanic, J. Matthew; Ding, Lin | |
通讯作者 | Pullen, A (通讯作者) |
发表日期 | 2008 |
ISSN | 1367-9120 |
EISSN | 1878-5786 |
起始页码 | 323 |
结束页码 | 336 |
卷号 | 33期号:5-6 |
英文摘要 | Geologic mapping and U-Pb detrital zircon geochronologic studies of (meta)sedimentary rocks in the Damxung area (similar to 90 kin north of Lhasa) of the southern Lhasa terrane in Tibet provide new insights into the history of deformation and clastic sedimentation prior to late Cenozoic extension. Cretaceous nonmarine elastic rocks similar to 10 kin southeast of Damxung are exposed as structural windows in the footwall of a thrust fault (the Damxung thrust) that carries Paleozoic strata in the hanging wall. To the north of Damxung in the southern part of the northern Nyainqentanglha Range (NNQTL), metaclastic rocks of previously inferred Paleozoic age are shown to range in depositional age from Late Cretaceous to Eocene. The metaclastic rocks regionally dip southward and are interpreted to have been structurally buried in the footwall of the Damxung thrust prior to being tectonized during late Cenozoic transtension. Along the northern flank of the NNQTL, Lower Eocene syncontractional redbeds were deposited in a triangle zone structural setting. All detrital zircon samples of Cretaceous-Eocene strata in the Damxung area include Early Cretaceous grains that were likely sourced from the Gangdese arc to the south. We suggest that the that newly recognized Late Cretaceous to Early Eocene (meta)clastic deposits and thrust faults represent the frontal and youngest part of a northward directed and propagating Gangdese retroarc thrust belt and foreland basin system that led to significant crustal thickening and elevation gain in southern Tibet prior to India-Asian collision. (C) 2008 Elsevier Ltd. All rights reserved. |
关键词 | TSANGPO SUTURE ZONETECTONIC EVOLUTIONLHASA BLOCKTERTIARY DEFORMATIONSHEAR ZONECOLLISIONROCKSINDIAGEOTRAVERSEHIMALAYA |
英文关键词 | Tibet; Gangdese arc; Lhasa terrane; plateau formation; retroarc thrust belt |
语种 | 英语 |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:000259419400003 |
来源期刊 | JOURNAL OF ASIAN EARTH SCIENCES
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来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/257577 |
推荐引用方式 GB/T 7714 | Pullen, Alex,Kapp, Paul,Gehrels, George E.,et al. Gangdese retroarc thrust belt and foreland basin deposits in the Damxung area, southern Tibet[J]. 中国科学院青藏高原研究所,2008,33(5-6). |
APA | Pullen, Alex.,Kapp, Paul.,Gehrels, George E..,DeCelles, Peter G..,Brown, Edwin H..,...&Ding, Lin.(2008).Gangdese retroarc thrust belt and foreland basin deposits in the Damxung area, southern Tibet.JOURNAL OF ASIAN EARTH SCIENCES,33(5-6). |
MLA | Pullen, Alex,et al."Gangdese retroarc thrust belt and foreland basin deposits in the Damxung area, southern Tibet".JOURNAL OF ASIAN EARTH SCIENCES 33.5-6(2008). |
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