Stratigraphic and sedimentary characteristics of the Upper   Jurassic-Lower Cretaceous strata in the Junggar Basin, Central Asia:   Tectonic and climate implications

doi:10.1016/j.jseaes.2016.09.001

CORC > 北京大学 > 地球与空间科学学院

	Stratigraphic and sedimentary characteristics of the Upper Jurassic-Lower Cretaceous strata in the Junggar Basin, Central Asia: Tectonic and climate implications
	Fang, Yanan ; Wu, Chaodong ; Wang, Yizhe ; Wang, Luxin ; Guo, Zhaojie ; Hu, Hanwen
刊名	JOURNAL OF ASIAN EARTH SCIENCES
	2016
关键词	Kalazha Formation Alluvial fan Conglomerate Sedimentary hiatus Depositional environment Stratigraphic Correlation DETRITAL ZIRCON GEOCHRONOLOGY NORTHERN TIEN-SHAN NORTHWEST CHINA NW CHINA TARIM BASIN TIAN-SHAN INTRACONTINENTAL DEFORMATION ACCRETIONARY OROGENESIS CONTINENTAL GROWTH AUTONOMOUS REGION
DOI	10.1016/j.jseaes.2016.09.001
英文摘要	The Junggar Basin, located in northwestern China, provides important records for investigating Mesozoic tectonic and climate evolution in Central Asia. The Upper Jurassic-lowermost Cretaceous strata in the basin include the Qigu, Kalazha, and Qingshuihe Formations in ascending order. By synthesizing outcrop and well data and previous research, we conducted a detailed sedimentologic and stratigraphic correlation analysis for the three formations. Our study shows that a sharp lithofacies change from intermittent braided-river red fine-grained sediments of the Qigu Formation to alluvial fan conglomerates of the Kalazha Formation, is widespread along the basin margins. From bottom to top, the Kalazha alluvial fan conglomerates can be divided into six sequences showing a progradation to retrogradation cycle, and they finally retrograde into the lake sediments of the lowermost Cretaceous Qingshuihe Formation. However, within the Junggar Basin, the Kalazha Formation is commonly considered to be absent and the Qingshuihe Formation possesses a basal fluvial coarse-grained sandstone bed (50100 m), beneath which a widespread unconformity is observed. Stratigraphic correlation suggests that the alluvial fan conglomerates of the Kalazha Formation along the basin margins are equivalent to the basal sandstone bed of the Qingshuihe Formation within the basin. Finally, we conclude that progressive tectonic uplift and climate aridification occurred in the Junggar Basin during deposition of the Qigu Formation in the Late Jurassic, while the basin began to experience a relatively humid climate and underwent rapid subsidence during deposition of the Kalazha Formation in the latest Jurassic-earliest Cretaceous, probably driven by the far-field effects of the short-lived but significant Mongol-Okhotsk collisional orogeny. (C) 2016 Elsevier Ltd. All rights reserved.; State Science and Technology Major Project [2011ZX05009001]; SCI(E); ARTICLE; cdwu@pku.edu.cn; 294-308; 129
语种	英语
内容类型	期刊论文
源URL	[http://ir.pku.edu.cn/handle/20.500.11897/458524]
专题	地球与空间科学学院
推荐引用方式 GB/T 7714	Fang, Yanan,Wu, Chaodong,Wang, Yizhe,et al. Stratigraphic and sedimentary characteristics of the Upper Jurassic-Lower Cretaceous strata in the Junggar Basin, Central Asia: Tectonic and climate implications[J]. JOURNAL OF ASIAN EARTH SCIENCES,2016.
APA	Fang, Yanan,Wu, Chaodong,Wang, Yizhe,Wang, Luxin,Guo, Zhaojie,&Hu, Hanwen.(2016).Stratigraphic and sedimentary characteristics of the Upper Jurassic-Lower Cretaceous strata in the Junggar Basin, Central Asia: Tectonic and climate implications.JOURNAL OF ASIAN EARTH SCIENCES.
MLA	Fang, Yanan,et al."Stratigraphic and sedimentary characteristics of the Upper Jurassic-Lower Cretaceous strata in the Junggar Basin, Central Asia: Tectonic and climate implications".JOURNAL OF ASIAN EARTH SCIENCES (2016).