Triassic in the eastern Sichuan basin ray slope and badong group strata division and correlation

Liu Zhen; Zhang Ruigang; Zhou Dan; Chen Fei; Li Wei; Chen Yang; Zhou Zhengda; Nie Lei

doi:10.1051/e3sconf/202235203021

E3S Web of Conferences (Jan 2022)

Triassic in the eastern Sichuan basin ray slope and badong group strata division and correlation

Liu Zhen,
Zhang Ruigang,
Zhou Dan,
Chen Fei,
Li Wei,
Chen Yang,
Zhou Zhengda,
Nie Lei

Affiliations

Liu Zhen: Chongqing Key Laboratory of exogenetic mineralization and mining environment (Chongqing Institute of Geology and mineral resources)
Zhang Ruigang: Chongqing Key Laboratory of exogenetic mineralization and mining environment (Chongqing Institute of Geology and mineral resources)
Zhou Dan: Chongqing Key Laboratory of exogenetic mineralization and mining environment (Chongqing Institute of Geology and mineral resources)
Chen Fei: Chongqing Key Laboratory of exogenetic mineralization and mining environment (Chongqing Institute of Geology and mineral resources)
Li Wei: Chongqing Key Laboratory of exogenetic mineralization and mining environment (Chongqing Institute of Geology and mineral resources)
Chen Yang: Chongqing Key Laboratory of exogenetic mineralization and mining environment (Chongqing Institute of Geology and mineral resources)
Zhou Zhengda: Chongqing Key Laboratory of exogenetic mineralization and mining environment (Chongqing Institute of Geology and mineral resources)
Nie Lei: Chongqing Key Laboratory of exogenetic mineralization and mining environment (Chongqing Institute of Geology and mineral resources)

DOI: https://doi.org/10.1051/e3sconf/202235203021
Journal volume & issue: Vol. 352
p. 03021

Abstract

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Triassic strata are widely developed in the eastern part of Sichuan Basin. The Mingyuexia anticline and Huangnitang anticline located in the eastern Sichuan structural belt develop Triassic Jialingjiang Formation to Xujiahe Formation. The middle Triassic Leikoupo Formation and Badong Formation on both sides of the anticline are synchronous and heterogeneous strata. They are distinguished regionally according to their different sedimentary environments and lithologic characteristics, and the phase transition boundary between Leikoupo Formation and Badong Formation is determined.

Published in E3S Web of Conferences

ISSN: 2267-1242 (Online)
Publisher: EDP Sciences
Country of publisher: France
LCC subjects: Geography. Anthropology. Recreation: Environmental sciences
Website: http://www.e3s-conferences.org/

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