气候变化领域集成服务门户(CCPortal): Tectono-sedimentary evolution of the Mesoproterozoic basins in the southern Yan-Liao and Mianchi-Queshan areas: insights from stratigraphic pattern and detrital zircon geochronology

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DOI	10.1007/s00531-019-01784-w
	Tectono-sedimentary evolution of the Mesoproterozoic basins in the southern Yan-Liao and Mianchi-Queshan areas: insights from stratigraphic pattern and detrital zircon geochronology
	Liu X.; Zhang J.; Li S.; Li X.; Yin C.
发表日期	2020
ISSN	14373254
起始页码	43
结束页码	62
卷号	109 期号:1
英文摘要	The widespread Mesoproterozoic successions around the world have recorded the breakup of the ancient supercontinent Columbia. In the North China Craton (NCC), the Mesoproterozoic basins in the Yan-Liao and southern NCC are the important evidence to study the nature and evolution of the Mesoproterozoic basins. In this study, we scrutinized the stratigraphic pattern and detrital zircon U–Pb geochronology in the southern Yan-Liao and Mianchi-Queshan areas in the southern NCC, to investigate the evolutionary relationship between the Mesoproterozoic basins in the north and south of NCC. Detrital zircons from the Mesoproterozoic sequence in the southern Yan-Liao areas showed monotonous source with age peak at ca. 2500 Ma, corresponding well with the ages of the Neoarchean complex in the central NCC. However, the Mesoproterozoic sequence in the Mianchi-Queshan areas, which is represented by the Ruyang Group, exhibited significantly different characteristics with influx of much younger zircons. The southern Yan-Liao and Mianchi-Queshan areas showed distinct similarity in the stratigraphic pattern, reflected by the Mesoproterozoic successions in these two areas being both bracketed by two sequence boundaries and further divided into two sequences under a uniform sea-level change. The Mesoproterozoic strata in these two areas probably possessed a correlative relationship in the stratigraphic patterns and basin evolutionary history. © 2019, Geologische Vereinigung e.V. (GV).
英文关键词	Basin evolution; Detrital zircon; Mesoproterozoic; North China Craton; Stratigraphic sequence
语种	英语
scopus关键词	basin evolution; detrital deposit; geochronology; Proterozoic; sequence stratigraphy; tectonic evolution; uranium-lead dating; zircon; China; North China Block
来源期刊	International Journal of Earth Sciences
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/147739
作者单位	Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), School of Earth Sciences and Engineering, Sun Yat-sen University, Zhuhai, 519000, China; Guangdong Provincial Key Lab of Geodynamics and Geohazards, School of Earth Sciences and Engineering, Sun Yat-Sen University, Guangzhou, 510372, China; Key Lab of Submarine Geosciences and Prospecting Techniques, MOE, Institute for Advanced Ocean Study, College of Marine Geosciences, Ocean University of China, Qingdao, 266100, China; Laboratories for Marine Mineral Resources and Marine Geology, National Laboratory for Marine Science and Technology, Qingdao, 266237, China
推荐引用方式 GB/T 7714	Liu X.,Zhang J.,Li S.,et al. Tectono-sedimentary evolution of the Mesoproterozoic basins in the southern Yan-Liao and Mianchi-Queshan areas: insights from stratigraphic pattern and detrital zircon geochronology[J],2020,109(1).
APA	Liu X.,Zhang J.,Li S.,Li X.,&Yin C..(2020).Tectono-sedimentary evolution of the Mesoproterozoic basins in the southern Yan-Liao and Mianchi-Queshan areas: insights from stratigraphic pattern and detrital zircon geochronology.International Journal of Earth Sciences,109(1).
MLA	Liu X.,et al."Tectono-sedimentary evolution of the Mesoproterozoic basins in the southern Yan-Liao and Mianchi-Queshan areas: insights from stratigraphic pattern and detrital zircon geochronology".International Journal of Earth Sciences 109.1(2020).