Discovery of mafic dikes in northeastern Tibet plateau belonging to the Emeishan large igneous province: Implications for paleocontinental reconstruction and mineral exploration

被引:0
|
作者
Yang, Kang [1 ,2 ]
Zhu, Wei-Guang [1 ]
Li, Chusi [1 ,3 ]
Bai, Zhong-Jie [1 ]
Wang, Yan-Jun [4 ]
Zheng, Shi-Ji [1 ]
Hu, Peng-Cheng [5 ]
机构
[1] Chinese Acad Sci, Inst Geochem, State Key Lab Ore Deposit Geochem, 99 West Lincheng Rd, Guiyang 550081, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Indiana Univ, Dept Geol & Atmospher Sci, Bloomington, IN 47405 USA
[4] East China Univ Technol, State Key Lab Nucl Resources & Environm, Nanchang 330013, Peoples R China
[5] Tianshui Normal Univ, Coll Resources & Environm Engn, Tianshui 741000, Peoples R China
基金
中国国家自然科学基金;
关键词
Mafic dikes; Large igneous province; Paleocontinental reconstruction; Yidun terrane; Tibet plateau; PLUME-LITHOSPHERE INTERACTION; TRIASSIC VOLCANIC-ROCKS; SONGPAN-GANZI; TECTONIC EVOLUTION; SW CHINA; FLOOD BASALTS; YIDUN ARC; GEOCHEMICAL CONSTRAINTS; CHEMICAL CLASSIFICATION; SOUTHWEST CHINA;
D O I
10.1016/j.gr.2024.07.026
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Due to the lack of paleomagnetic data and paleoclimatic records, the paleocontinental belonging of the Yidun terrane in northeastern Tibet plateau is debated. In this paper, we use the distribution of the Emeishan large igneous province (ELIP) to put the issue to rest. The ELIP is the product of mantle plume activity, which took place at 260 +/- 3 Ma in the western margin of the Yangtze craton. The Yangtze craton is the northern part of the South China paleocontinental block. Our new discovery of four mafic dikes in the Yidun terrane with ages and chemistry like the ELIP strongly supports a new interpretation that this terrane was an integral part of the Yangtze craton during the ELIP magmatic event. Baddeleyites from these mafic dikes yield the U-Pb ages of 257.1 +/- 4.8, 259.8 +/- 8.5, 260.2 +/- 4.5 and 261.5 +/- 6.8 Ma for each of these dikes, which are similar to the zircon U-Pb ages of the mafic-ultramafic intrusions of the ELIP within the Yangtze craton. The Yidun mafic dikes and some high-Ti basalts of the ELIP within the Yangtze craton have similar Sr-Nd isotope compositions and mantle-normalized incompatible trace element distribution patterns, indicating similar mantle source compositions. Mixing calculation using SrNd isotope compositions shows that the parental magmas for the Yidun mafic dikes experienced only 2-3 % crustal contamination. Partial melting modelling shows that the primary magmas for the Yidun mafic dikes were produced by 5-6 % mantle partial melting at the depths > 85 km below surface, consistent with mantle plume-related magmatism in a continental setting. The Yidun terrane is a new exploration frontier for magmatic Fe-Ti-V oxide deposits that are present elsewhere in the ELIP. (c) 2024 International Association for Gondwana Research. Published by Elsevier B.V. All rights are reserved, including those for text and data mining, AI training, and similar technologies.
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页码:1 / 13
页数:13
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