中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Early Cretaceous magmatic flare-up in the northern-central Tibetan Plateau: Products of low-angle bidirectional subduction and slab sinking of the Bangong-Nujiang Tethys Ocean

文献类型:期刊论文

作者Yang, Xingchen5,6; Zhao, Yuanfang5,6; Cai, Maotang5,6; Ji, Fengbao1; Meng, Lingtong3,4; Zhou, Qiuyu5,6; Zhou, Yuanjian5,6; Pei, Yingru5,6; Yuan, Changjiang2
刊名GONDWANA RESEARCH
出版日期2026-03-01
卷号151页码:131-152
关键词Tibetan Plateau Bangong-Nujiang Tethys Ocean Early Cretaceous Post-collisional magmatism Magmatic flare-up
ISSN号1342-937X
DOI10.1016/j.gr.2025.10.013
产权排序2
文献子类Article
英文摘要The Bangong-Nujiang suture zone (BNSZ), separating the Qiangtang and Lhasa blocks, exhibits extensive Early Cretaceous varied magmatism and significant metallogenetic potential. However, geodynamic mechanisms driving this magmatic flare-up remain controversial. To address this issue, we conducted a comprehensive study focusing on the multi-type intrusions within and adjacent to the melange zone in the Amdo-Nagqu area, middle BNSZ. Zircon U-Pb dating indicates that these intrusions emplaced during the Early Cretaceous (119-109 Ma). They display consistent arc-like whole-rock major and trace element characteristics with highly variable wholerock initial 87Sr/86Sr (0.706534-0.712838) ratios, negative epsilon Nd(t) (-3.7 to - 9.2) values, and negative to weakly positive zircon epsilon Hf(t) (-14.7 to + 2.0) values. These geochemical features suggest their petrogenesis involved crust-mantle interactions. Furthermore, the mafic samples are characterized by narrow-ranging 143Nd/144Nd ratios but a wide range of Hf/Nd ratios, and a broader variation of zircon delta 18O values (8.9-15.5 %o) compared with coeval felsic samples (7.8-9.8 %o), indicating the involvement of subducted sediments in the mantle source. Based on the new and previously published data, we suggest that the mafic intrusions originated from partial melting of the sediment-dominated melange in the sub-continental lithospheric mantle (SCLM), providing tangible evidence of the southward oceanic subduction. In contrast, the felsic intrusions formed through partial melting of the continental crust within hot zones, accompanied by varying degrees of mantle-derived magma mixing. We propose the following geodynamic model for the widespread, small-volume, compositionally diverse Early Cretaceous magmatism along the BNSZ: Demise of the Bangong-Nujiang Tethys Ocean via low-angle bidirectional subduction during the Early Cretaceous, followed by extensive and contemporaneous partial melting. This process was triggered by the decompression and hot asthenosphere upwelling through corner flow and local sporadic slab windows within the fractured zones, along with sinking of the eclogitized ocean slab.
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WOS关键词HIGH-MG ANDESITES ; A-TYPE GRANITES ; TECTONIC EVOLUTION ; LHASA TERRANE ; RIDGE SUBDUCTION ; MELANGE DIAPIRS ; SUTURE ZONE ; EXPERIMENTAL CONSTRAINTS ; METAMORPHIC COMPLEX ; QIANGTANG TERRANE
WOS研究方向Geology
语种英语
WOS记录号WOS:001630922800001
出版者ELSEVIER
源URL[http://ir.igsnrr.ac.cn/handle/311030/219762]  
专题陆地表层格局与模拟院重点实验室_外文论文
通讯作者Ji, Fengbao
作者单位1.Xizang Museum Nat Sci, 9 Zangda East Rd, Lhasa 850000, Peoples R China;
2.China Univ Geosci Beijing, Sch Earth Sci & Resources, Beijing 100083, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China;
4.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China;
5.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Land Surface Pattern & Simulat, Beijing 100101, Peoples R China;
6.Chinese Acad Geol Sci, Inst Geomech, Beijing 100081, Peoples R China;
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Yang, Xingchen,Zhao, Yuanfang,Cai, Maotang,et al. Early Cretaceous magmatic flare-up in the northern-central Tibetan Plateau: Products of low-angle bidirectional subduction and slab sinking of the Bangong-Nujiang Tethys Ocean[J]. GONDWANA RESEARCH,2026,151:131-152.
APA Yang, Xingchen.,Zhao, Yuanfang.,Cai, Maotang.,Ji, Fengbao.,Meng, Lingtong.,...&Yuan, Changjiang.(2026).Early Cretaceous magmatic flare-up in the northern-central Tibetan Plateau: Products of low-angle bidirectional subduction and slab sinking of the Bangong-Nujiang Tethys Ocean.GONDWANA RESEARCH,151,131-152.
MLA Yang, Xingchen,et al."Early Cretaceous magmatic flare-up in the northern-central Tibetan Plateau: Products of low-angle bidirectional subduction and slab sinking of the Bangong-Nujiang Tethys Ocean".GONDWANA RESEARCH 151(2026):131-152.

入库方式: OAI收割

来源:地理科学与资源研究所

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