Where was South China in the Rodinia supercontinent? Evidence from U-Pb geochronology and Hf isotopes of detrital zircons

被引:303
作者
Yu, Jin-Hai [1 ,2 ]
O'Reilly, Suzanne Y. [2 ]
Wang, Lijuan [1 ,2 ]
Griffin, W. L. [2 ]
Zhang, Ming [2 ]
Wang, Rucheng [1 ]
Jiang, Shaoyong [1 ]
Shu, Liangshu [1 ]
机构
[1] Nanjing Univ, State Key Lab Mineral Deposits Res, Dept Earth Sci, Nanjing 210093, Peoples R China
[2] Macquarie Univ, GEMOC ARC Natl Key Ctr, Dept Earth & Planetary Sci, Sydney, NSW 2109, Australia
基金
中国国家自然科学基金;
关键词
Neoproterozoic reconstruction; Rodinia configuration; South China tectonic history; zircon geochronology; zircon Hf isotopes;
D O I
10.1016/j.precamres.2008.03.002
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
U-Pb geochronology and Lu-Hf isotopic studies on detrital zircons from late Neoproterozoic sediments of the Cathaysia block, South China, show abundant Grenville-age (similar to 1.0 Ga) and Neoarchaean populations, and minor Eoarchaean (similar to 3.8 Ga), Paleo- to Mesoarchaean (3.3-3.0 Ga), Mesoproterozoic (1.7-1.4 Ga) and Pan-African (0.70-0.54 Ga) populations. This is the first report of similar to 3.8 Ga material in the crust of the Cathaysia block. The presence of euhedral similar to 1.0 Ga zircons indicates that a Grenville orogenic belt was within or very close to the southern Cathaysia block. However, the provenance containing the similar to 3.8 Ga, 3.3-3.0 Ga, similar to 2.5 Ga, similar to 1.0 Ga and 0.70-0.54 Ga zircon populations cannot be found in the South China Block; the combination of zircon age distributions and the rounded, strongly abraded shapes of the Archean zircons suggesting long transport is consistent with derivation from other continental terranes previously linked with the southern part of the South China Block. Comparison with the tectono-magmatic history and compositions of rocks in western Laurentia - eastern Australia and eastern India - East Antarctica - western Australia, we suggest that these late Neoproterozoic sediments may have originated mainly from Eastern India-East Antarctica. This indicates that the South China Block was linked with the Eastern India - East Antarctica continents in the late Neoproterozoic rather than being located between the western Laurentia and eastern Australia continental blocks. U-Pb and Hf-isotope studies on detrital zircons provide an important independent constraint on the palaeogeography of the South China Block in the context of the breakup of Rodinia and the subsequent assembly of Gondwana in late Neoproterozoic time, and insights into the relationship between the Cathaysia and Yangtze blocks. (C) 2008 Elsevier B.V. All rights reserved.
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页码:1 / 15
页数:15
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