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Ying Li

Researcher at Shandong University of Science and Technology

Publications -  13
Citations -  205

Ying Li is an academic researcher from Shandong University of Science and Technology. The author has contributed to research in topics: Coal & Structural basin. The author has an hindex of 5, co-authored 11 publications receiving 168 citations.

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Depositional environment, sequence stratigraphy and sedimentary mineralization mechanism in the coal bed- and oil shale-bearing succession: A case from the Paleogene Huangxian Basin of China

TL;DR: In this article, the Huangxian Basin was chosen as a typical example to study the mechanism of sedimentation of coal and oil shale, and a sequence stratigraphic framework with two sequences (each including three systems tracts) was established to analyze the depositional evolution.
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The geologic settings of Chinese coal deposits

TL;DR: The coal-bearing strata in China have complicated geneses and di... as discussed by the authors, which are extensively developed in marine-influenced, continental, and transitional environments, and the coal resources are abundant in China.
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Sedimentary Model of Coal and Shale in the Paleogene Lijiaya Formation of the Huangxian Basin: Insight from Petrological and Geochemical Characteristics of Coal and Shale

TL;DR: In this paper, the sedimentary models of coal and shale associations are very important to expander the coal-and-shale associations in the Huangxian Basin, which lies in Eastern China.
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Sedimentological Characteristics of the Coal Seams of Yacheng Formation in Qiongdongnan Basin, China

TL;DR: Yacheng Formation has been divided into one cycle sequence of ultra long-period, three cylce sequences of long period and 12 cycle sequences of intermediate period based on data from comprehensive drilling cores, logging, the seismic survey and former studies.
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Mechanisms of accumulation and coexistence of coal and oil shale in typical basins

TL;DR: In this paper, the authors investigated the geotectonic basis of coal and oil shale coexistence and concluded that the basins' tectonic activity controlled the overall characteristics of basin filling, and thus represented the external conditions for the coexistence of coal.