Detrital zircon provenance of the Late Triassic Songpan-Ganzi complex: Sedimentary record of collision of the North and South China blocks
Detrital zircon provenance of the Late Triassic Songpan-Ganzi complex: Sedimentary record of collision of the North and South China blocks
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DOI：
10.1130/g21929.1
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发表时间：
2006
期刊：
影响因子：
5.8
通讯作者：
A. Weislogel;S. Graham;E. Chang;J. Wooden;G. Gehrels;He Yang
中科院分区：
文献类型：
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作者：
A. Weislogel;S. Graham;E. Chang;J. Wooden;G. Gehrels;He Yang
松潘-甘孜三叠纪复理石序列的大部分被认为来自于中国东部大别和苏鲁超高压变质带的剥蚀(例如，[聂氏等，1994年][1]；[周和格雷厄姆，1996年][2])；然而，关于复理石的来源仍存在激烈的争论
The majority of the Songpan-Ganzi Triassic flysch sequence is believed to have derived from denudation of the Dabie and Sulu ultrahigh-pressure (UHP) metamorphic belt in eastern China (e.g., [Nie et al., 1994][1]; [Zhou and Graham, 1996][2]); however, intense debate still exists on the sources of