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DOI | 10.1002/gj.3976 |
Petrogenesis and tectonic implications of Palaeocene (ca. 54 Ma) rhyolites in the western Lhasa Terrane, south Tibet: Constraints from geochemistry and Sr-Nd-Hf isotope compositions | |
Ding, Xiang-Li; Ding, Lin; Wang, Chao; Wang, Hou-Qi; Guo, Xu-Dong | |
通讯作者 | Wang, C (通讯作者) |
发表日期 | 2021 |
ISSN | 0072-1050 |
EISSN | 1099-1034 |
起始页码 | 494 |
结束页码 | 507 |
卷号 | 56期号:1 |
英文摘要 | The widespread Linzizong volcanic successions (LVS) in the Lhasa Terrane was a magmatic response to the tectonic transition from Neo-Tethyan oceanic subduction to the India-Asia collision, which has been the subject of many studies; however, studies on the LVS in the western Lhasa Terrane are scarce compared to those in the east, limiting our understanding of the tectonic transition. Zircon U-Pb ages of two rhyolitic samples from the Shiquanhe region in the west of the Lhasa Terrane indicate that at least part of the Zenong Group, previously thought to have formed during the Early Cretaceous, was actually erupted during the Late Palaeocene (ca. 54 Ma) and belongs to the LVS. The rhyolites are characterized by high SiO(2)and Al2O3, moderate K2O and Na2O, and low MgO, CaO, and FeO contents, enrichment in Rb and Th, depletion in Sr, Ba, Eu, Nb, and Ta, and have relatively uniform whole-rock epsilon(Nd)(t) (-1.90 to -0.89) and zircon epsilon(Hf)(t) (+0.95 to +5.03) values. These geochemical characteristics indicate that they were formed by the partial melting of juvenile continental crust with subsequent plagioclase, biotite, amphibole, and Fe-Ti oxide fractionation. Combined with the results of previous studies, our data show that the western Lhasa Terrane underwent intensive Early Cenozoic crustal growth, similar to what occurred in the east, due to underplating of mantle-derived magma resulting from the roll-back and eventual break-off of the Neo-Tethys slab after the initial continental collision. |
关键词 | LINZIZONG VOLCANIC SUCCESSIONA-TYPE GRANITESTI-IN-ZIRCONGANGDESE MOUNTAINSO ISOTOPESROCKSAREAGEOCHRONOLOGYGENESISSATURATION |
英文关键词 | crustal melting; high-SiO(2)rhyolite; Lhasa Terrane; Linzizong volcanic successions; Palaeocene; zircon geochemistry |
语种 | 英语 |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:000564218000001 |
来源期刊 | GEOLOGICAL JOURNAL |
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/260139 |
推荐引用方式 GB/T 7714 | Ding, Xiang-Li,Ding, Lin,Wang, Chao,et al. Petrogenesis and tectonic implications of Palaeocene (ca. 54 Ma) rhyolites in the western Lhasa Terrane, south Tibet: Constraints from geochemistry and Sr-Nd-Hf isotope compositions[J]. 中国科学院青藏高原研究所,2021,56(1). |
APA | Ding, Xiang-Li,Ding, Lin,Wang, Chao,Wang, Hou-Qi,&Guo, Xu-Dong.(2021).Petrogenesis and tectonic implications of Palaeocene (ca. 54 Ma) rhyolites in the western Lhasa Terrane, south Tibet: Constraints from geochemistry and Sr-Nd-Hf isotope compositions.GEOLOGICAL JOURNAL,56(1). |
MLA | Ding, Xiang-Li,et al."Petrogenesis and tectonic implications of Palaeocene (ca. 54 Ma) rhyolites in the western Lhasa Terrane, south Tibet: Constraints from geochemistry and Sr-Nd-Hf isotope compositions".GEOLOGICAL JOURNAL 56.1(2021). |
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