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Xinghe Yu
Researcher at China University of Geosciences (Beijing)
Publications - 23
Citations - 199
Xinghe Yu is an academic researcher from China University of Geosciences (Beijing). The author has contributed to research in topics: Sedimentary rock & Sedimentary depositional environment. The author has an hindex of 7, co-authored 22 publications receiving 133 citations. Previous affiliations of Xinghe Yu include China University of Petroleum.
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Classification, formation, and transport mechanisms of mud clasts
TL;DR: In this article, the relative balance of volumetric abundance of sedimentary clasts in non-marine to marine sedimentary records is identified as the most important criterion for classification.
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Jurassic sedimentary evolution of southern Junggar Basin: Implication for palaeoclimate changes in northern Xinjiang Uygur Autonomous Region, China
TL;DR: In this article, the authors discussed the controlling factors of sedimentary evolution and palaeoclimate changes in Junggar Basin during the Jurassic period based on lithology, fossils and tectonic setting.
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The Ground Penetrating Radar facies and architecture of a Paleo-spit from Huangqihai Lake, North China: Implications for genesis and evolution
TL;DR: In this article, a paleo-spit is identified from Huangqihai Lake in North China and proposed as a classic example for investigating the influence of lake level changes and storms on the construction of these bodies.
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Change from tide-influenced deltas in a regression-dominated set of sequences to tide-dominated estuaries in a transgression-dominated sequence set, East China Sea Shelf Basin
TL;DR: In this article, the authors explore facies and architectural changes from tide-influenced deltas to tide-dominated estuaries in transgressive-regressive cycles, as well as their controlling factors.
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Quantitative Characterization of Architecture Elements and Their Response To Base-Level Change In A Sandy Braided Fluvial System At A Mountain Front
TL;DR: In this article, the authors analyzed the architectural elements of the Yungang Formation and found that during base-level rise the braided fluvial system developed large-scale channel units, bar units, and overbank fills.