期刊
EARTH AND PLANETARY SCIENCE LETTERS
卷 575, 期 -, 页码 -出版社
ELSEVIER
DOI: 10.1016/j.epsl.2021.117196
关键词
low-delta O-18 magmatic ring; Rodinia supercontinent; South China; Yangtze Block
资金
- Strategic Priority Research Program (B) of the Chinese Academy of Sciences [XDB18030300]
- China Postdoctoral Science Foundation [2019M650833]
- State Key Laboratory of Lithospheric Evolution [SKL-K201902]
This study reports Neoproterozoic (ca. 785-780 Ma) granites with low-delta O-18 values from the western margin of the Yangtze Block, which are linked to assimilation of syn-magmatically altered rocks and have their source constrained by high temperature hydrothermal alteration. The zircons exhibit a decrease in delta O-18 values from core to rim, indicating a remelting process at high temperatures.
We report Neoproterozoic (ca. 785-780 Ma) granites from the western margin of the Yangtze Block that are characterised by magmatic zircons with delta O-18 values as low as 2.98 parts per thousand. The lack of low-delta O-18 magmatic zircons in the ca. 820-805 Ma rhyolite samples from the Neoproterozoic Suxiong Formation indicates that there is no recycling of pre-existing hydrothermally altered crust in the study area prior to the emplacement of the ca. 785-780 Ma granites. Thus the ca. 785-780 Ma granites with low-delta O-18 values from the western margin of the Yangtze Block can be linked to assimilation of syn-magmatically altered rocks (rather than the assimilation of a pre-existing hydrothermally altered crust). The granites have a source constrained by their depleted Hf isotopes and low-delta O-18 values resulting from high temperature hydrothermal alteration. The delta O-18 values of the zircons from core to rim exhibit a decrease indicative of the remelting of material during the interaction between magma and water at high temperatures. In combination with the widespread low-delta O-18 signatures that occur in the northern and southern margins of the Yangtze Block and Cathaysia Block, the locations of low-delta O-18 magmatic zircons exhibit a Neoproterozoic low-delta O-18 magmatic ring around South China. This continent-scale Neoproterozoic extensional and magmatic event cannot be attributed to subduction processes in South China resulting in the emplacement of a magmatic ring of felsic igneous rocks with low-delta O-18 values. We therefore propose a model involving a Neoproterozoic super-mantle plume with a diameter of approximately 1500 km controlling the development of the rift systems around South China. (C) 2021 Elsevier B.V. All rights reserved.
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