The metamorphic evolution of Salma-type eclogite in Russia: Constraints from zircon/titanite dating and phase equilibria modeling

doi:10.1016/j.precamres.2018.01.019

CORC > 地质与地球物理研究所 > 中国科学院地质与地球物理研究所 > 岩石圈演化国家重点实验室

	The metamorphic evolution of Salma-type eclogite in Russia: Constraints from zircon/titanite dating and phase equilibria modeling
	Yu, Huanglu 1; Zhang, Lifei 1; Zhang, Lijuan 1; Wei, Chunjing 1; Li, Xiaoli 1; Guo, Jinghui 2; Bader, Thomas 1; Qi, Yunfei 1
刊名	PRECAMBRIAN RESEARCH
	2019-06-15
卷号	326 页码:363-384
关键词	Salma-type eclogite Zircon age Titanite age Phase equilibria modeling Clockwise P-T path
ISSN号	0301-9268
DOI	10.1016/j.precamres.2018.01.019
英文摘要	Combined geochronology with phase equilibria modeling, the P-T-t evolution of metamorphic rocks can be deciphered. Four different representative samples, including retrogressed eclogite, garnetite, paragneiss and tonalite-trondhjemite-granodiorite (TTG) gneiss have been selected for detailed petrography and U/Pb dating from the Belomorian Eclogite Province in Russia. Zircon cores yield Archean ages for the protoliths of these samples. Zircon rims of the TTG gneiss have recorded Neoarchean anataxis at ca 2.73 Ga, whereas 1.91-1.92 Ga zircon rims of the garnetite and the paragneiss have dated high-pressure granulite facies metamorphism. Titanite in the retrogressed eclogite has recorded amphibolite facies retrogression at ca 1.86 Ga. Phase equilibria modelings for retrogressed eclogite, garnetite, and paragneiss define P-T conditions of 17-18 kbar/below 790 degrees C for the peak eclogite facies metamorphism, 11-12 kbar/870-900 degrees C for the high-pressure granulite facies metamorphism, and 8-10 kbar/650-710 degrees C for titanite's stability which corresponds to the amphibolite facies metamorphism. A clockwise P-T path is inferred for the Salma-type eclogite, which is characterized by thermal relaxation from the peak eclogite facies to the high-pressure granulite facies, and nearly isobaric cooling from the high-pressure granulite facies to the amphibolite facies.
资助项目	National Nature Science Foundation of China[41121062] ; National Nature Science Foundation of China[41172196] ; National Nature Science Foundation of China[41311120071]
WOS关键词	BELOMORIAN MOBILE BELT ; U-PB AGE ; PARTIAL MELTING EQUILIBRIA ; HIGH-GRADE METAMORPHISM ; TIANSHAN OROGENIC BELT ; TECTONIC EVOLUTION ; GRANULITE-FACIES ; PALEOPROTEROZOIC ECLOGITES ; UHP METAMORPHISM ; KARELIAN CRATON
WOS研究方向	Geology
语种	英语
出版者	ELSEVIER SCIENCE BV
WOS记录号	WOS:000469157300021
资助机构	National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/92275]
专题	地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者	Zhang, Lifei
作者单位	1.Peking Univ, Sch Earth & Space Sci, MOE Key Lab Orogen Belt & Crustal Evolut, Beijing 100871, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
推荐引用方式 GB/T 7714	Yu, Huanglu,Zhang, Lifei,Zhang, Lijuan,et al. The metamorphic evolution of Salma-type eclogite in Russia: Constraints from zircon/titanite dating and phase equilibria modeling[J]. PRECAMBRIAN RESEARCH,2019,326:363-384.
APA	Yu, Huanglu.,Zhang, Lifei.,Zhang, Lijuan.,Wei, Chunjing.,Li, Xiaoli.,...&Qi, Yunfei.(2019).The metamorphic evolution of Salma-type eclogite in Russia: Constraints from zircon/titanite dating and phase equilibria modeling.PRECAMBRIAN RESEARCH,326,363-384.
MLA	Yu, Huanglu,et al."The metamorphic evolution of Salma-type eclogite in Russia: Constraints from zircon/titanite dating and phase equilibria modeling".PRECAMBRIAN RESEARCH 326(2019):363-384.