Characteristics of igneous rocks and their significance in hydrocarbon accumulation in Block C of Santos Basin, SE Brazil by Jian Zhao, Jie Zhang, Junfeng Zhao, Kangxu Ren, Chaofeng Wang, Yuan Guo

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Remote sensing spectral of igneous rocks from Xinchang county, Zhejiang Province and their forming mechanism(浙江新昌主要火成岩类的遥感光谱与形成机理) by ZHANGDeng-rong(张登荣), DONGChuan-wan(董传万), HUANGQin(黄勤), YANQiang(闫强)

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3-D engraving of volcanic mechanism in the Tiantai slope of Xihu Depression and its formation mechanism by Xueyi Wang, Qianghu Liu, Hongtao Zhu, Guowei Hou, Lanzhi Qin

Subjects: “…igneous rocks…”
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Petrological characteristics, reservoir property and oil-bearing potential of intrusive rocks in well Shaduo 1, Qintong Sag, Subei Basin by Xiang XIA, Xiaodong MA, Wenxuan HU, Suhua ZANG

“…Igneous rock oil and gas reservoir has gradually become an important type of oil and gas reservoir, but the igneous rock reservoir is highly heterogeneous, the reservoir property varies greatly, and the study of reservoir genetic mechanism is unsubstantial, which has become the main bottleneck of igneous rock reservoir evaluation. …”
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Diagenetic effect of mantle-derived CO2 charge to clay minerals in the Baiyun-Liwan deepwater area of the Pearl River Mouth Basin in South China Sea by Yanhua Liu, Honghan Chen, Yanfei Wang, Jinyang Han, Qian Li

“…Finally, two patterns of CO2 migration and accumulation in the Zhujiang and Zhuhai Formations were summarized: (1) the mantle-derived CO2 migrates vertically upward through the deep faults which connected with the mafic igneous rocks, and (2) lateral long-distance migration through connecting sand bodies after vertical upward migration. …”
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Structural characteristics and tectonic evolution of Mesozoic-Cenozoic faults in the Shunbei area, Tarim Basin by Zicheng Cao, Daqing Tang, Mansong Luo, Zhongzheng Jiang, Caijun Hong, Yongtao Xia, Hua Wei

“…The structural position, middle Permian igneous rocks, and the sandy mudstone of the Lower Triassic Tongketuer Formation have significant control on fault evolution.Detailed interpretation of faults in the T90-T50 stratigraphic interval in the Shunbei area shows that the central part of the No.5 fault and south central part of the No.7 fault are two large faults that connect downward to the source rock of the basin. …”
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Reservoir characteristics and hydrocarbon accumulation significance of metamorphic zones of intrusive rocks and surrounding rocks in second member of Paleocene Funing Formation in... by Suhua ZANG

“…The intrusive rocks of the Funing Formation were formed during the Wubao to Sanduo periods. The intrusion of igneous rocks created a circular metamorphic zone prior to the hydrocarbon charging stage, indicating a favorable accumulation match. …”
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Research on sedimentary environment and provenance for hydrocarbon source rocks of Upper Carboniferous Batamayineishan Formation in northeastern Junggar Basin: evidences from the g... by Qianru CAI, Jinduo WANG, Guanlong ZHANG, Zhihua SONG, Shengzhu WANG, Zhengrong XIONG, Shengli NI

“…Major and trace elements of mudstones indicate that the parent rocks are sedimentary rocks and felsic volcanic rocks and their provenance is derived from the weathering products of acidic igneous rocks of the Karamaili Island Arc, reflecting the tectonic transition from compression to extension during the post collision stage. …”
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Reservoir-forming rules and main controlling factors of Archean buried hill reservoir of middle to northern Liaoxi Uplift in Liaodong Bay area in Bohai Bay Basin by Longlong GUO, Jun WANG, Chunguang ZHANG, Hongde CHEN

“…The proportion of igneous rocks increases gradually from north to south. …”
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Distribution characteristics and accumulation mechanism of carbon dioxide gas reservoirs in the Pearl River Mouth Basin by Zhongliang Gao, Yanfei Wang, Shenglan Lei, Wenyong Wang, Ning Jiang, Dapeng Jiang, Jun Liu, Kecheng Li

“…Meanwhile, the distribution of inorganic mantle source CO2 is greatly controlled by the fault system, and its distribution locations have a close relationship with the ranges of basement faults and igneous rocks. The inorganic CO2 gas is sourced by the degassing of mantle-derived magma. …”
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