Diagenetic xenotime dating to constrain the initial depositional time of the Yan-Liao Rift

doi:10.1016/j.precamres.2015.09.024

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

	Diagenetic xenotime dating to constrain the initial depositional time of the Yan-Liao Rift
	Zhang, Yan-Bin; Li, Qiu-Li; Lan, Zhong-Wu; Wu, Fu-Yuan; Li, Xian-Hua; Yang, Jin-Hui; Zhai, Ming-Guo
刊名	PRECAMBRIAN RESEARCH
	2015-12-01
卷号	271 页码:20-32
关键词	Diagenetic xenotime Monazite Changcheng group SIMS U-Pb dating
DOI	10.1016/j.precamres.2015.09.024
文献子类	Article
英文摘要	In the Mesoproterozoic and Neoproterozoic, the North China Craton (NCC) underwent long-lived sedimentation with minor volcanism in the Yan-Liao Rift forming the Mesoproterozoic Changcheng, Jixian and Qingbaikou Groups in sequence. The basal boundary age of the Lower Changcheng Group indicates the initial time of the NCC as a stable cratonic block and can be used to make correlations among several representative basins worldwide. Recent studies have debated the initial depositional time of the Changcheng System, which is the key to understanding the Proterozoic tectonic evolution of the NCC. This study documented the xenotime and monazite from the lowermost Changzhougou and Chuanlinggou Formations of the Changcheng Group. The monazite grains from the Chuanlinggou Formation yielded U-Pb ages between 1810 Ma and 2500 Ma, which are comparable to the detrital zircon U-Pb ages in the same formation, indicating their detrital origin. Xenotime mostly occurs as overgrowths on the detrital zircon grains, supporting a post-depositional origin. The low U content of the Changzhougou Formation's xenotimes indicates a hydrothermal origin. Its peak age of 1570 +/- 15 Ma may indicate a hydrothermal event. The xenotime from the Chuanlinggou Formation is characterized by a high U content and a REE pattern with a nonexistent or weak negative Eu anomaly and a higher Gd/Yb ratio, implying a diagenetic origin. These xenotime overgrowths yielded a wide age variation, even on a single grain, due to prolonged xenotime precipitation. The oldest population of 1716 +/- 3 Ma is interpreted as the minimum depositional age of the Chuanlinggou Formation. The lowest boundary of the Changchengian System must be older than 1716 Ma. This work demonstrates that diagenetic xenotime could better constrain the depositional time; however, extensive systematic research is required, especially with higher spatial resolution and more diagenetic xenotime grains. (C) 2015 Elsevier B.V. All rights reserved.
WOS关键词	NORTH CHINA CRATON ; U-PB GEOCHRONOLOGY ; SEDIMENTARY-ROCKS ; ZIRCON GEOCHRONOLOGY ; AUTHIGENIC XENOTIME ; PHOSPHATE MINERALS ; ION MICROPROBE ; EVOLUTION ; AGES ; BASIN
WOS研究方向	Geology
语种	英语
WOS记录号	WOS:000366790900002
资助机构	National Natural Science Foundation of China(41172173 ; National Natural Science Foundation of China(41172173 ; National Natural Science Foundation of China(41172173 ; National Natural Science Foundation of China(41172173 ; 41221022 ; 41221022 ; 41221022 ; 41221022 ; 41210003 ; 41210003 ; 41210003 ; 41210003 ; 41222023 ; 41222023 ; 41222023 ; 41222023 ; 41273069) ; 41273069) ; 41273069) ; 41273069) ; National Natural Science Foundation of China(41172173 ; National Natural Science Foundation of China(41172173 ; National Natural Science Foundation of China(41172173 ; National Natural Science Foundation of China(41172173 ; 41221022 ; 41221022 ; 41221022 ; 41221022 ; 41210003 ; 41210003 ; 41210003 ; 41210003 ; 41222023 ; 41222023 ; 41222023 ; 41222023 ; 41273069) ; 41273069) ; 41273069) ; 41273069)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/62139]
专题	地质与地球物理研究所_岩石圈演化国家重点实验室
作者单位	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	Zhang, Yan-Bin,Li, Qiu-Li,Lan, Zhong-Wu,et al. Diagenetic xenotime dating to constrain the initial depositional time of the Yan-Liao Rift[J]. PRECAMBRIAN RESEARCH,2015,271:20-32.
APA	Zhang, Yan-Bin.,Li, Qiu-Li.,Lan, Zhong-Wu.,Wu, Fu-Yuan.,Li, Xian-Hua.,...&Zhai, Ming-Guo.(2015).Diagenetic xenotime dating to constrain the initial depositional time of the Yan-Liao Rift.PRECAMBRIAN RESEARCH,271,20-32.
MLA	Zhang, Yan-Bin,et al."Diagenetic xenotime dating to constrain the initial depositional time of the Yan-Liao Rift".PRECAMBRIAN RESEARCH 271(2015):20-32.