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Wenxuan Hu

Researcher at Nanjing University

Publications -  157
Citations -  3294

Wenxuan Hu is an academic researcher from Nanjing University. The author has contributed to research in topics: Source rock & Geology. The author has an hindex of 25, co-authored 133 publications receiving 2250 citations.

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The Permian hybrid petroleum system in the northwest margin of the Junggar Basin, northwest China

TL;DR: In this paper, the authors defined a hybrid petroleum system for the northwest margin of the Junggar Basin, by documenting the complexity in its formation and evolution, and showed that the three source rocks charged reservoirs mainly in three geologic intervals, with common mixing of oils from different sources and/or with different maturities.
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Raman spectroscopic measurements of CO2 density: Experimental calibration with high-pressure optical cell (HPOC) and fused silica capillary capsule (FSCC) with application to fluid inclusion observations

TL;DR: In this paper, a high-pressure optical cell and fused silica capillary capsules were used to prepare pure CO 2 samples with densities between 0.0472 and 1.0060 g/cm 3.
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Petroleum migration and mixing in the northwestern Junggar Basin (NW China): constraints from oil-bearing fluid inclusion analyses

TL;DR: In this article, oil-bearing fluid inclusions are present in four reservoir sandstone samples from the slope and fault zone areas in the northwestern margin of the Junggar Basin (NW China).
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Mesogenetic dissolution of the middle Ordovician limestone in the Tahe oilfield of Tarim basin, NW China

TL;DR: The mesogenetic dissolution is well developed in the middle Ordovician Yijianfang formation (O2yj) limestone, and the dissolution pores are very important for petroleum accumulation in the south slope area of the Tahe oilfield which lies in the north of the Tarim basin, northwestern China.
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Formation mechanism of deep Cambrian dolomite reservoirs in the Tarim basin, northwestern China

TL;DR: In this paper, a porosity variation model was proposed for the deep dolomite reservoirs that were influenced by hydrothermal fluids, which indicated that there may be high-quality dolomerite reservoirs in the deep strata of basins where hydrothermas are active.