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DOI10.1007/s11434-008-0362-x
Early Oligocene anatexis in the Yardoi gneiss dome, southern Tibet and geological implications
Zeng LingSen; Liu Jing; Gao Lie; Xie KeJia; Wen Li
通讯作者Zeng, LS (通讯作者)
发表日期2009
ISSN1001-6538
EISSN1861-9541
起始页码104
结束页码112
卷号54期号:1
英文摘要The Yardoi gneiss dome is located to the easternmost of the North Himalayan Gneiss Dome (NHGD), southern Tibet. It consists of metapelite, garnet amphibolite, granite and leucogranite, and is a key subject to constrain the formation and tectonic evolution of NHGD. SHRIMP zircon U/Pb data on the leucogranite yield an age of 35.3 +/- 1.1 Ma, which is substantially older than that of the similar leucogranites to the west. Sr and Nd isotope systematics indicate that this leucogranite was derived from partial melting of the mixed garnet amphibolite and metapelite. Our data suggest that ( 1) during the early stage of Himalayan magmatism, amphibolite dehydration melting overwhelmed that of the metapelite; and (2) such a melting at middle-lower crust might be a major factor that initiated the movement along the Southern Tibetan Detachment System (STDS).
关键词ND-ISOTOPE DISEQUILIBRIUMHIMALAYAN LEUKOGRANITESCRUSTAL ANATEXISLANGTANG VALLEYGEOCHEMICAL CONSTRAINTSMETAMORPHIC SEQUENCESIERRA-NEVADAKANGMAR DOMEEVOLUTIONGRANITE
英文关键词leucogranite; metapelite; crustal anatexis; Himalayan Orogenic Belt; North Himalayan Gneiss Dome
语种英语
WOS研究方向Science & Technology - Other Topics
WOS类目Multidisciplinary Sciences
WOS记录号WOS:000263128300015
来源期刊CHINESE SCIENCE BULLETIN
来源机构中国科学院青藏高原研究所
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/257642
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GB/T 7714
Zeng LingSen,Liu Jing,Gao Lie,et al. Early Oligocene anatexis in the Yardoi gneiss dome, southern Tibet and geological implications[J]. 中国科学院青藏高原研究所,2009,54(1).
APA Zeng LingSen,Liu Jing,Gao Lie,Xie KeJia,&Wen Li.(2009).Early Oligocene anatexis in the Yardoi gneiss dome, southern Tibet and geological implications.CHINESE SCIENCE BULLETIN,54(1).
MLA Zeng LingSen,et al."Early Oligocene anatexis in the Yardoi gneiss dome, southern Tibet and geological implications".CHINESE SCIENCE BULLETIN 54.1(2009).
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