Early Oligocene Na-rich peraluminous leucogranites in the Yardoi gneiss dome, southern Tibet Formation mechanism and tectonic implications | |
Gao, LE (Gao LiE); Zeng, LS (Zeng LingSen); Liu, J (Liu Jing); Xie, KJ (Xie KeJia) | |
刊名 | ACTA PETROLOGICA SINICA
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2009 | |
卷号 | 25期号:9页码:2289-2302 |
关键词 | Tibet North Himalayan Gneiss Dome Yardoi gneiss dome Leucogranite Crustal anatexis |
ISSN号 | 1000-0569 |
英文摘要 | The east-west trending Northern Himalayan Gneiss Dome (NHGD) consists of a series Of Semi-continuous gneiss domes within the Tethyan Himalayan Belt. The Yardoi gneiss dome, the easternmost one among these domes, consists of garnet two-mica gneiss, garnet amphibolite, two-mica granite and leucogranite. Available SHRIMP zircon U/Pb data show that the Yardoi leucogranite formed at 35.3 +/- 1.1Ma, older than those similar leucogranites to the west (commonly with ages <25Ma). Bulk element and Sr and Nd isotope analyses show that (1) a majority of the Yardoi leucogranites are Na-rich and peraluminous; (2) similar to the wall-rock gneisses, the Yardoi Ieucogranites are enriched in LILE (e.g. K, Sr, Rb, and Ba), but highly depleted in Ti, Y, Yb, Sc, and Cr; (3) as compared to those either in the gneisses or in the amphibolites, the Yardoi leucogranites are depleted both in LREE and in HREE. However, they are enriched in LREE relative to HREE; (4) the Yardoi leucogranites have initial Sr isotope compositions ranging from 0.71195 to 0.71934, similar to those in the amphibolites, whereas they have relatively lower epsilon(Nd)(i) values ( -8.9 similar to 15. 0), which is intermediate between those in the amphibolites and the gneisses. Two end member simple mixing calculations indicate that partial melting of a source mixed of garnet amphibolite with subordinate pelitic gneiss could account for the formation of the Yardoi Na-rich peraluminouis melts. The Yardoi leucogranites have an average Zr saturation temperature of 673 degrees C. At this temperature, both H(2)O-fluxed melting of metapelite at high-pressures ( similar to 10kbar) and amphibolite parting melting can produce Na-rich peraluminous granitic melts. However, amphibolite partial melting dominated the similar to 35 Ma anatectic event in the Yardoi gneiss dome. This event might be a major factor that led to the transition from compressional to extensional deformation in the overthickened Himalayan belt. |
学科主题 | 变质岩岩石学 |
WOS关键词 | HIMALAYAN LEUKOGRANITES ; ZIRCON SATURATION ; LANGTANG VALLEY ; GEOCHEMICAL CONSTRAINTS ; METAMORPHIC SEQUENCE ; CONTINENTAL-CRUST ; TETHYAN HIMALAYA ; ANATEXIS ; ORIGIN ; MAGMAS |
WOS研究方向 | Geology |
语种 | 中文 |
出版者 | SCIENCE PRESS |
WOS记录号 | WOS:000270044500021 |
内容类型 | 期刊论文 |
源URL | [http://119.78.100.197/handle/2HKVOGP0/38931] ![]() |
专题 | 中国地质调查局 |
作者单位 | Chinese Acad Sci, Inst Tibetan Plateau Res, Beijing 100085, Peoples R China |
推荐引用方式 GB/T 7714 | Gao, LE ,Zeng, LS ,Liu, J ,et al. Early Oligocene Na-rich peraluminous leucogranites in the Yardoi gneiss dome, southern Tibet Formation mechanism and tectonic implications[J]. ACTA PETROLOGICA SINICA,2009,25(9):2289-2302. |
APA | Gao, LE ,Zeng, LS ,Liu, J ,&Xie, KJ .(2009).Early Oligocene Na-rich peraluminous leucogranites in the Yardoi gneiss dome, southern Tibet Formation mechanism and tectonic implications.ACTA PETROLOGICA SINICA,25(9),2289-2302. |
MLA | Gao, LE ,et al."Early Oligocene Na-rich peraluminous leucogranites in the Yardoi gneiss dome, southern Tibet Formation mechanism and tectonic implications".ACTA PETROLOGICA SINICA 25.9(2009):2289-2302. |
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