The Sugetbrak basalts from northwestern Tarim Block of northwest China:   Geochronology, geochemistry and implications for Rodinia breakup and ice   age in the Late Neoproterozoic

doi:10.1016/j.precamres.2013.07.009

CORC > 北京大学 > 地球与空间科学学院

	The Sugetbrak basalts from northwestern Tarim Block of northwest China: Geochronology, geochemistry and implications for Rodinia breakup and ice age in the Late Neoproterozoic
	Xu, Bei ; Zou, Haibo ; Chen, Yan ; He, Jinyou ; Wang, Yu
刊名	precambrian research
	2013
关键词	Late Neoproterozoic Tarim Block Rodinia SHRIMP U-Pb age Glaciation U-PB AGES SNOWBALL EARTH HYPOTHESIS BASIN NW CHINA SOUTH CHINA ISOTOPIC EVIDENCE VOLCANIC-ROCKS TRACE-ELEMENT MANTLE PLUME DOUSHANTUO FORMATION MARINOAN GLACIATION
DOI	10.1016/j.precamres.2013.07.009
英文摘要	Zircons from two samples of the Sugetbrak basalts (SB) yield weighted mean ages of 615.2 +/- 4.8 Ma and 614.4 +/- 9.1 Ma. These ages, interpreted as the eruption age of the SB, provide an age constraint on the timing of the Sugetbrak Formation in Sugetbrak, northwestern Tarim Block, China. These two ages suggest that the igneous activities related to the breakup of the Neoproterozoic supercontinent Rodinia lasted until 614-615 Ma in at least the northwest Tarim Block. Geochemical analysis indicates that the SB was generated in an intra-continental rifting environment. Application of the dynamic melting inversion method suggests that the Sugetbrak basalts represent 7-12% partial melts. Unlike large-volume tholeiites, these low-degree transitional basaltic melts may represent the waning stage of plume volcanism during a long-lasting continental breakup. Based on the ages of the SB and its stratigraphic relationship with the Yuermeinak diamictite, the Yuermeinak glaciation in the Sugetbrak section of the northwest Tarim Block should correlate with the Tereeken glaciation in the Qurugtagh area of the northeast Tarim Block, the Nantuo glaciation in Yangtze Block and the Elatina glaciation in South Australia. (C) 2013 Elsevier B.V. All rights reserved.; http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000328806100015&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 ; Geosciences, Multidisciplinary; SCI(E); 16; ARTICLE; 214-226; 236
语种	英语
内容类型	期刊论文
源URL	[http://ir.pku.edu.cn/handle/20.500.11897/220216]
专题	地球与空间科学学院
推荐引用方式 GB/T 7714	Xu, Bei,Zou, Haibo,Chen, Yan,et al. The Sugetbrak basalts from northwestern Tarim Block of northwest China: Geochronology, geochemistry and implications for Rodinia breakup and ice age in the Late Neoproterozoic[J]. precambrian research,2013.
APA	Xu, Bei,Zou, Haibo,Chen, Yan,He, Jinyou,&Wang, Yu.(2013).The Sugetbrak basalts from northwestern Tarim Block of northwest China: Geochronology, geochemistry and implications for Rodinia breakup and ice age in the Late Neoproterozoic.precambrian research.
MLA	Xu, Bei,et al."The Sugetbrak basalts from northwestern Tarim Block of northwest China: Geochronology, geochemistry and implications for Rodinia breakup and ice age in the Late Neoproterozoic".precambrian research (2013).