气候变化领域集成服务门户(CCPortal): Evolution of a plume-influenced source-to-sink system: An example from the coupled central Emeishan large igneous province and adjacent western Yangtze cratonic basin in the Late Permian, SW China

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DOI	10.1016/j.earscirev.2020.103224
	Evolution of a plume-influenced source-to-sink system: An example from the coupled central Emeishan large igneous province and adjacent western Yangtze cratonic basin in the Late Permian, SW China
	Wang X.; Shao L.; Eriksson K.A.; Yan Z.; Wang J.; Li H.; Zhou R.; Lu J.
发表日期	2020
ISSN	00128252
卷号	207
英文摘要	Source-to-sink paleogeography in a time-constrained sequence stratigraphic framework has been reconstructed for the non-marine to marine transitional Lopingian strata (Late Permian) in the western Yangtze Cratonic Basin (WYCB) and the adjacent inner zone of the Emeishan large igneous province (ELIP) in order to reveal the evolution of a mantle plume influenced cratonic basin. The Lopingian coal-bearing strata can be subdivided into seventeen 4th-order sequences and three 3rd-order composite sequences representing 6.76 Myr. Paleogeographic reconstructions of the WYCB demonstrate the existence of N-S trending terrestrial, transitional and marine facies belts distributed west to east away from the central ELIP. Geomorphological analysis indicates that the western boundary of the source area coincided with the major axis of the uplifted central ELIP. Based on sediment flux estimates and modeling (BQART model), relief of the central ELIP increased from near sea-level in the earliest Late Permian and reached equilibrium at about 200 m in the latest Permian. Sediment volume backfilling analysis indicates that total tectonic uplift of the central ELIP in the Late Permian was more than 500 m. Evolution of the coupled central ELIP and WYCB can be subdivided into three stages, pre-eruptive uplift stage, pre- and syn-eruptive subsidence stage, and syn- and post-eruptive uplift stage. Post-eruptive basin filling was controlled by sediment supply that was related to tectonic uplift, drainage topography and climate change, and basin accommodation that was related to sea-level fluctuations and plume-induced syn-sedimentary tectonics. © 2020 Elsevier B.V.
关键词	BQART model Emeishan large igneous province Late Permian Mantle plume Paleogeographic reconstruction Source-to-sink system
英文关键词	climate variation; craton; large igneous province; mantle plume; paleogeography; Permian; reconstruction; sea level change; sequence stratigraphy; topography; uplift; China; Yangtze Platform
语种	英语
来源期刊	Earth Science Reviews
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/203923
作者单位	State Key Laboratory of Coal Resources and Safe Mining, College of Geoscience and Surveying Engineering, China University of Mining and Technology (Beijing), Beijing, 100083, China; Department of Geosciences, Virginia Tech, Blacksburg, VA 24061, United States; Yunnan Provincial Coal Geological Survey Institute, Kunming, 650218, China; China Geological Survey Bureau, Beijing, 100083, China
推荐引用方式 GB/T 7714	Wang X.,Shao L.,Eriksson K.A.,et al. Evolution of a plume-influenced source-to-sink system: An example from the coupled central Emeishan large igneous province and adjacent western Yangtze cratonic basin in the Late Permian, SW China[J],2020,207.
APA	Wang X..,Shao L..,Eriksson K.A..,Yan Z..,Wang J..,...&Lu J..(2020).Evolution of a plume-influenced source-to-sink system: An example from the coupled central Emeishan large igneous province and adjacent western Yangtze cratonic basin in the Late Permian, SW China.Earth Science Reviews,207.
MLA	Wang X.,et al."Evolution of a plume-influenced source-to-sink system: An example from the coupled central Emeishan large igneous province and adjacent western Yangtze cratonic basin in the Late Permian, SW China".Earth Science Reviews 207(2020).