Genesis of post-collisional calc-alkaline and alkaline granitoids in   Qiman Tagh, East Kunlun, China

doi:10.1016/j.lithos.2015.08.022

CORC > 北京大学 > 地球与空间科学学院

	Genesis of post-collisional calc-alkaline and alkaline granitoids in Qiman Tagh, East Kunlun, China
	Yu, Miao ; Feng, Chengyou ; Zhao, Yiming ; Li, Daxin
刊名	LITHOS
	2015
关键词	Qiman Tagh Calc-alkaline magma Alkaline magma Post-collisional magmatism Petrogenesis A-TYPE GRANITES ND ISOTOPIC EVIDENCE CONTINENTAL-CRUST VOLCANIC-ROCKS MANTLE WEDGE EXPERIMENTAL CONSTRAINTS MICROGRANULAR ENCLAVES TECTONIC IMPLICATIONS ZIRCON GEOCHRONOLOGY TIBETAN PLATEAU
DOI	10.1016/j.lithos.2015.08.022
英文摘要	The post-collisional magmatism of Qiman Tagh is characterized by the intrusion of voluminous intermediate to felsic granitoids, including syenogranite, monzogranite, granodiorite, tonalite and diorite. The granitoids can be divided into two magmatic suites: Calc-alkaline (CA) and alkaline (Alk), which were emplaced from similar to 236 Ma to similar to 204 Ma. The CA suite contains metaluminous granodiorites and monzogranites. Typical Qiman Tagh CA granodiorites show moderately fractionated REE patterns ((La/Yb)(N) = 4.35-25.11) with significant negative Eu anomalies (ELVEu* = 0.54-134), and the primitive mantle-normalized spidergrams show strong depletion of Nb and Sr. The Qiman Tagh CA monzogranites show similar fractionated REE patterns ((La/Yb)(N) = 2.70-13.5) with less prominent negative Eu anomalies, and the chondrite-normalized spidergrams show strongly depleted Ba, Nb and Sr. The Alk suite, including syenogranite, is highly potassic (K2O/Na2O = 1.09-3.56) and peraluminous (A/CNK = 0.91-1.06). Compared to typical Qiman Tagh CA granodiorites, the man Tagh Alk granitoids can be distinguished by their higher Rb, Nb, Ga/Al, FeO/MgO, Y/Sr and Rb/Sr, as well as their lower Mg-#, MgO, CaO, Al2O3, Sr, Co, V, Eu/Eu, Ba/Nb, La/Nb, Ba/La and Ce/Nb. The Qiman Tagh CA rocks were most likely to be derived from the partial melting of garnet-amphibolite-facies rocks in the lower crust, leaving behind anhydrous granulite-facies rocks with plagioclase and garnet in the residue. The Alk rocks may have formed by the continued partial melting of granulite-facies rocks at elevated temperatures (>830 degrees C). Crown Copyright (C) 2015 Published by Elsevier B.V. All rights reserved.; National Natural Science Foundation of China [41172076]; Program of High-level Geological Talents [201309]; Youth Geological Talents of the China Geological Survey [201112]; Geological Survey Program from the China Geological Survey [1212011085528]; Scientific Research Fund of the Non-Commercial Unit from Ministry of Land and Resources, China [201411025]; SCI(E); ARTICLE; fengchy@cags.ac.cn; 45-59; 239
语种	英语
内容类型	期刊论文
源URL	[http://ir.pku.edu.cn/handle/20.500.11897/439064]
专题	地球与空间科学学院
推荐引用方式 GB/T 7714	Yu, Miao,Feng, Chengyou,Zhao, Yiming,et al. Genesis of post-collisional calc-alkaline and alkaline granitoids in Qiman Tagh, East Kunlun, China[J]. LITHOS,2015.
APA	Yu, Miao,Feng, Chengyou,Zhao, Yiming,&Li, Daxin.(2015).Genesis of post-collisional calc-alkaline and alkaline granitoids in Qiman Tagh, East Kunlun, China.LITHOS.
MLA	Yu, Miao,et al."Genesis of post-collisional calc-alkaline and alkaline granitoids in Qiman Tagh, East Kunlun, China".LITHOS (2015).