Mitogenomic phylogeny and divergence time estimation of Artemia Leach, 1819 (Branchiopoda: Anostraca) with emphasis on parthenogenetic lineages. [PDF]
Asem A +8 more
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Sedimentary Features and Distribution of High-Quality Reservoirs in the Ledong Area, Yinggehai Basin
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Neogene zonal vegetation of China and the evolution of the winter monsoon [PDF]
F.M.B. Jacques, G. Shi, W.M. Wang
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Characteristics of hydrocarbon accumulation and exploration potential of the northern South China Sea deepwater basins [PDF]
B. G. K. Aarssen Van +17 more
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Study on Sedimentary Facies of Ledong Formation in Yinggehai Basin Based on Seismic Facies Analysis
Hao Li, Pan Yang
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Multicomponent seismic exploration in Yinggehai Basin
The Leading Edge, 2002In Yinggehai Basin, an important area for offshore gas exploration in China, rapid filling and deposition caused undercompaction of a massive layer of mudstone. Several diapiric anticlinal structures formed in the center of this basin under the effect of deep hot fluids, making Yinggehai Basin a favorite area for exploration of oil and gas.
He Hanyi, Zhou Hongzhang, Fu Dandan
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A distinctive hydrocarbon basin—Yinggehai Basin, South China Sea
Journal of Southeast Asian Earth Sciences, 1991Abstract The Yinggehai basin is a Cenozoic hydrocarbon basin situated on the geosuture of the Indosinian Plate and South China Plate (the Red River Fault Zone). It is a strike-slip tensional basin developed from an unstable craton in the passive continental argin.
Zhang Qiming, Zhang Quanxing
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Yinggehai basin gas exploration: Comparison with Jiyang depression
Journal of Earth Science, 2012Yinggehai (莺歌海) basin and Jiyang (济阳) depression experienced similar tectonic evolution, which is mainly controlled by the strike-slip faults. The strike pull-apart basins are characteristic by multiple deposition cycles, migration of deposition and subsidence center, and diversity depositional systems.
Zhifeng Wan +4 more
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Mechanism of diapirism and episodic fluid injections in the Yinggehai Basin
Science in China Series D, 2002The diapirism in the Yinggehai Basin is a combined result of strong overpressure caused by rapid sedimentation of fine-grain sediments and the tensile stress field resulting from right-lateral slip of the boundary-fault. The diapirism showed multiple-stage, episodic nature, and caused intermittent counter-direction onlaps and changes in the thickness ...
Fang Hao +3 more
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OVERPRESSURE DEVELOPMENT AND HYDROFRACTURING IN THE YINGGEHAI BASIN, SOUTH CHINA SEA
Journal of Petroleum Geology, 1999Intensely overpressured compartments are present in the centre of the Yinggehai Basin, South China Sea. In this part of the basin, a diapiric area can be distinguished from a non‐diapiric area; structures in the former area result from shale diapirism at depth, and from the movement of hydrothermal fluids at more shallow levels.
Xie Xinong +3 more
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