[1] |
GUO Wang, CHEN Gang, LI Yuhong, ZHANG Yunpeng, LI Yonghong, DANG Hongliang.
Lacustrine Organic Matter Accumulation During Gradually Arid Palaeoclimate in the Late of Middle Jurassic, Northern Qaidam Basin
[J]. Geological Journal of China Universities, 2025, 31(02): 200-212.
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[2] |
SUN Houxue, HAO Fang, WANG Qi, TIAN Jinqiang.
Sedimentary Environment and Organic Matter Enrichment Mechanism of the Yuertusi Formation Source Rocks during Early Cambrian Period
[J]. Geological Journal of China Universities, 2024, 30(05): 622-633.
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[3] |
ZHANG Xiaoshuan, ZHANG Xin, LIAO Qiping, FAN Yafei, LIU jinming, WEI Dongtao.
The Characteristics of Sandy Conglomerate Reservoir in Mazhong Area of the Junggar Basin and A Nonlinear Inversion Method be Used to Predict It
[J]. Geological Journal of China Universities, 2024, 30(04): 496-504.
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[4] |
YIN Shengyu, GONG Deyu, SU Jing, HU Zhengzhou, WU Wei’an, WANG Ruiju.
Genetic Types and Origins of Upper Paleozoic-reservoiered Oil in Dongdaohaizi Sag and Its Surrounding Areas in the Junggar Basin
[J]. Geological Journal of China Universities, 2024, 30(02): 218-230.
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[5] |
CHEN Huanqing, CHEN Shunxin.
Research on the Construction of Achievement Platform of Fine Reservoir Description of Oilfield Development
[J]. Geological Journal of China Universities, 2024, 30(01): 100-109.
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[6] |
XIA Changfa, LIN Chunming, ZHANG Xia, HUANG Shuya, LI Xulong, ZHAO Xuepei, LI Xin, SONG Fulai, ZOU Bingfang, LI Tiejun.
Provenance and Sedimentary Facies of the Member 3 of Paleogene Dongying Formation in the Eastern Part of the Liaohe Depression Tidal Area
[J]. Geological Journal of China Universities, 2023, 29(5): 766-775.
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[7] |
XIAO Xiaoguang.
Study on Genetic Mechanism and Lower Limit of Deep Effective Reservoirs in the Xihu Sag
[J]. Geological Journal of China Universities, 2023, 29(4): 630-643.
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[8] |
CHEN Jie, LIANG Xiao, TONG Mingsheng, ZHANG Jianli, LIU Lang, XU Jianliang, CHENG Liang, LIU Ruolin, YANG Cheng.
Tectonic and Sedimentary Evidences for Oil and Gas Exploration Targets and Prospects of the Ediacaran-Cambrian Petroleum Systems in the Northern Oman Basin (Block 5)
[J]. Geological Journal of China Universities, 2022, 28(6): 943-957.
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[9] |
GAN Jun, ZHANG Yingzhao, YANG Xibing, LUO Wei, XIONG Xiaofeng, LI Xing, LIANG Gang.
Natural Gas Accumulation Model Controlled Jointly by Source and Reservoir in Deep Water Area of Qiongdongnan Basin
[J]. Geological Journal of China Universities, 2022, 28(5): 635-643.
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[10] |
HE Wanhui, WANG Wei, YIN Hongwei, LIU Shaowen, ZHU Jitian, XIONG Xiaofeng.
Structural Evolution in Deep Water Area of Qiongdongnan Basin and Comparison of Structural Differences between Eastern and Western Segments
[J]. Geological Journal of China Universities, 2022, 28(5): 644-654.
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[11] |
ZENG Xiaoyu, GUO Minggang, ZHU Jitian, XIONG Xiaofeng, DUAN Liang, PENG Junfeng.
The Influence of Multi-stage Magmatic Intrusion Events on Thermal Evolution of Source Rocks in Changchang Sag
[J]. Geological Journal of China Universities, 2022, 28(5): 709-716.
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[12] |
GUO Xiaoxiao, XU Xinde, GAN Jun, XIONG Xiaofeng, WANG Ziling, YOU Junjun.
Causes of Gas Geochemical Differences in the Ultra-high Pressure Gas Field, the Eastern Slope of Yinggehai Basin
[J]. Geological Journal of China Universities, 2022, 28(5): 717-725.
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[13] |
ZHU Jitian, GUO Minggang, XIONG Xiaofeng, ZENG Xiaoyu, HE Yi, TANG Lishan, SONG Peng.
Natural Gas Migration Rule and Play in Deep-water Area in Qiongdongnan Basin
[J]. Geological Journal of China Universities, 2022, 28(5): 726-734.
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[14] |
WANG Hui, XIU Zongxiang, SUN Yongfu, LIU Shaowen, SONG Yupeng, DONG Lifeng, SONG Binhui.
Analysis of the Stability of Submarine Slope Considering the Effects of Undrained Shear Strength of the Cover Layer of Gas Hydrates
[J]. Geological Journal of China Universities, 2022, 28(5): 747-757.
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[15] |
WU Dongxu, LI Chang, ZHOU Jingao, HU Cong, HUANG Zhengliang, YU Zhou, LI Weiling, GUO wei.
Characteristics and Genesis Mechanism of the Dolomite Reservoir in the Ordovician Majiagou Formation in the Ordos Basin
[J]. Geological Journal of China Universities, 2022, 28(4): 606-616.
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