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Qingshao Liang

As seen in: MDPI
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Articles

Minerals | Free Full-Text | Microfacies Analysis of Mixed Siliciclastic-Carbonate Deposits in the Early-Middle Ordovician Meitan Formation in the Upper Yangtze Platform in SW China: Implications for Sea-Level Changes during the GOBE

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By Xing Wang, Xiaobing Lin, Jingchun Tian, Qingshao Liang
| MDPI
1. Introduction The Ordovician period has been regarded as an exceptional epoch in the Earth’s evolutionary history, distinguished by momentous global transformation and a distinctive paleogeographic framework [1,2,3,4,5]. In particular, the Great Ordovician Biodiversification Event (GOBE) during the Ordovician period has attracted widespread scholarly attention [6,7,8,9,10,11,12,13,14,15,16].
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Geological Environment and Controlling Factors of Panlongdong Karst Cave in Northeastern Sichuan Basin

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By Deqin Ma, Jingchun Tian, Qingshao Liang, Jian Li
| MDPI
Abstract : The karst landforms in northeastern Sichuan Basin are widely developed, but the understanding of the geological characteristics, controlling factors, and spatiotemporal evolution process of karst caves is still unclear. The research object of this study is the Panlongdong karst cave in the northeastern Sichuan Basin.
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Minerals | Free Full-Text | Geological Characteristics and Paleoenvironmental Evolution of Fine-Grained Sediments in the Third Member of the Xujiahe Formation in the Western Sichuan Depression, SW China

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By Yunfei Lu, Jingchun Tian, Qingshao Liang, Xiaobing Lin
| MDPI
This is an early access version, the complete PDF, HTML, and XML versions will be available soon. Open AccessArticle by Yunfei Lu 1,2, Jingchun Tian 1,2,*, Qingshao Liang 1,2 and Xiaobing Lin 1,2 1 Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China 2 State Key Laboratory of Oil & Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China * Author to whom correspondence should be addressed.
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