[1] Cai, X.F., 1994.Palaeoclimates as a Necessary Factor in Basin Analysis.Sedimentary Facies and Palaeogeography, 14(2):42-46 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YXGD402.004.htm
[2] Chen, J.F., Zhang, S.C., Sun, S.L., et al., 2006.Main Factors Influencing Marine Carbonate Source Rock Formation.Acta Geologica Sinica, 80(3):467-472 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dizhixb200603021
[3] Dai, J.X., Zou, C.N., Tao, S.Z., et al., 2007.Formation Conditions and Main Controlling Factors of Large Gas Fields in China.Natural Gas Geoscience, 18(4):473-484 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-TDKX200704001.htm
[4] Deng, Y.H., 2009.Analysis on Differences of Petroleum Type and Geological Conditions between Two Depression Belts in China Offshore.Acta Petrolei Sinica, 30(1):1-8 (in Chinese with English abstract). doi: 10.1038/aps.2008.1
[5] Duan, M.D., Ye, J.R., Wu, J.F., et al., 2017.Overpressure Formation Mechanism in Xihu Depression of the East China Sea Shelf Basin.Earth Science, 42(1):119-129 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2017.009
[6] Fu, N., Deng, Y.H., Zhang, G.C., et al., 2010.Transitional Source Rock and Its Contribution to Hydrocarbon Accumulation in Superimpose Rift-Subsidence Basin of Northern South China Sea:Taking Baiyun Sag of ZhuⅡ Depression as an Example.Acta Petrolei Sinica, 31(4):559-565 (in Chinese with English abstract).
[7] Fu, N., Mi, L.J., Zhang, G.C., et al., 2007.Source Rocks and Origin of Oil and Gas in the Northern Baiyun Depression of Pearl River Mouth Basin.Acta Petrolei Sinica, 28(3):32-38 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syxb200703007
[8] Hu, X, M., Wang, C.S., 2001.Summarization on the Studying Methods of the Palaeo-Ocean Dissolved Oxygen.Advance in Earth Sciences, 16(1):65-71 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkxjz200101013
[9] Ingall, E, D., Cappellen, P, V., 1990.Relation between Sedimentation Rate and Burial of Organic Phosphorus and Organic Carbon in Marine Sediments.Geochimica et Cosmochimica Acta, 54(2):373-386, https://doi.org/10.1016/0016-7037(90)90326-g
[10] Li, T.Y., He, S., Yang, Z., et al., 2008.The Marine Source Rock Formation Conditions and Control Factors.Geological Science and Technology Information, 27(6):63-70 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/syxb201801001
[11] Li, X.Q., Liu, J.S., Lu, Y.C., et al., 2018.Prototype Basin Chracterization of Huagang Formation of Xihu Depression, East China Sea Shelf Basin.Earth Science, 43(2):502-513 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2017.596
[12] Li, Y.C., 2015.Main Controlling Factors for the Development of High Quality Lacustrine Hydrocarbon Source Rocks in Offshore China.China Offshore Oil and Gas, 27(3):1-9 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zghsyq-gc201503001
[13] Li, Y.C., Deng, Y.H., Zhang, G.C., 2012.Zoned Distribution of Source Rocks and Hydrocarbon Offshore China.China Offshore Oil and Gas, 24(1):6-12 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zghsyq-gc201201002
[14] Li, Y.C., Deng, Y.H., Zhang, G.C., 2014.Gas-Rich Zone and Main Controlling Factors of Gas Source Rock in Offshore China.Natural Gas Geoscience, 25(9):1309-1319 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/trqdqkx201409002
[15] Liu, C.L., Yang, J.L., Hans-Joachim, R., et al., 2001.Factors Influencing Organic Carbon Distribution inLacustrine Sediments.Acta Sedimentologica Sinica, 19(1):113-116 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CJXB200101019.htm
[16] Pedersen, T.F., Calvert, S.E., 1990.Anoxia vs, Productivity:What Controls the Formation of Organic-Carbon-Rich Sediments and Sedimentary Rock? AAPG Bulletin, 74(4):454-466. https://doi.org/10.1306/0c9b232b-1710-11d7-8645000102c1865d
[17] Qian, H.J., Lu, X.C., Zhang, X.F., et al., 2009.Spatial Paleosalinity Distribution and Element Geochemistry of Argillaceous Source Rocks in the Upper Part of 4th Member of Tertiary Shahejie Formation in Dongying Sag.Acta Petrologica et Mineralogica, 28(2):161-168 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yskwxzz200902008
[18] Su, A., Chen, H.H., Wang, C.W., et al., 2013.Genesis and Maturity Identification of Oil and Gas in the Xihu Sag, East China Sea Basin.Petroleum Exploration and Development, 40(5):521-527 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SKYK201305003.htm
[19] Tao, S.Z., Zou, C.N., 2005.Accumulation and Distribution of Natural Gases in Xihu Sag, East China Sea Basin.Petroleum Exploration and Development, 32(4):103-110 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SKYK200504019.htm
[20] Tyson, R.V., Pearson, T.H., 1991.Modern and Ancient Continental Shelf Anoxia.Geological Soeiety of Special Publication, 58(1):1-24. doi: 10.1144-GSL.SP.1991.058.01.01/
[21] Wei, H.F., Chen, J.F., Chen, X.D., et al., 2013.The Controlling Factors and Sedimentary Environment for Developing Coastal Coal-Bearing Source Rock of Pinghu Formation in Xihu Depression.Geology in China, 40(2):487-497 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi201302013
[22] Ye, J.R., Qing, H, R., Bend, S, L., et al., 2007.Petroleum Systems in the Offshore Xihu Basin on the Continental Shelf of the East China Sea.AAPG Bulletin, 91(8):1167-1188, https://doi.org/10.1306/02220705158
[23] Zhang, G, C., 2005.Geological Features and New Exploration Realms of Offshore Gas in China.China Offshore Oil and Gas, 17(5):289-296 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zghsyq-gc200505001
[24] Zhang, G.C., 2010.Tectonic Evolution of Deepwater Area of Northern Continental Margin in South China Sea.Acta Petrolei Sinica, 31(4):528-533, 541 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dqkx201101016
[25] Zhang, G.C., 2012.Co-Control of Source and Heat.Acta Petrolei Sinica, 33(5):723-738 (in Chinese with English abstract).
[26] Zhang, G.C., Wang, Q., Miao, S.D., et al., 2014.The Duality Distribution Pattern of Marine-Continental Transitional Hydrocarbon Source Rocks:A Case Study from Baiyun Sag in Pearl River Mouth Basin, China Offshore.Natural Gas Geoscience, 25(9):1299-1308 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/trqdqkx201409001
[27] Zhang, G.H., Zhang, J.P., 2015.A Discussion on the Tectonic Inversion and Its Genetic Mechanism in the East China Sea Shelf Basin.Earth Science Frontiers, 22(1):260-270 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dxqy201501022
[28] Zhang, J.P., Zhang, T., Tang, X.J., 2014.Basin Type and Dynamic Environment in the East China Sea Shelf Basin.Acta Geologica Sinica, 88(11):2033-2043 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb201411002
[29] Zhao, X, L., Zhao, C.B., Guan, X.T., et al., 1992.The Application of Spore-Pollen Data in a Quantitative Explanation of Tertiary Palaeoclimate in Our Country.Acta Petrolei Sinica, 13(2):215-225 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYXB199202035.htm
[30] Zhao, Z, G., Wang, P., Qi, P., et al., 2016.Regional Background and Tectonic Evolution of East China Sea Basin.Earth Science, 41(3):546-554 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2016.045
[31] Zhong, T., Cao, B., Liu, J.S., et al., 2017.Genesis of Chlorite Rims and Its Significance to Low Porosity and Low Permeability Sandstone Reservoir of Huagang Formation in North Central Xihu Sag, East Sea of China.Journal of Chengdu University of Technology (Science & Technology Edition), 44(6):708-716 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cdlgxyxb201706008
[32] Zhu, W.L., 2010.Advancements of Oil and Gas Exploration in China Offshore Area:Overview and Perspective.Engineering Sciences, 12(5):18-24 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GCKX201005003.htm
[33] Zhu, Y.M., Zhou, J., Gu, S.X., et al., 2012.Molecular Geochemistry of Eocene Pinghu Formation Coal-Bearing Source Rocks in the Xihu Depression, East China Sea Shelf Basin.Acta Petrolei Sinica, 33(1):32-39 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syxb201201004
[34] 蔡雄飞, 1994.古气候条件是盆地分析不可缺少的因素.岩相古地理, 14(2):42-46. http://www.cnki.com.cn/Article/CJFDTOTAL-YXGD402.004.htm
[35] 陈践发, 张水昌, 孙省利, 等, 2006.海相碳酸盐岩优质烃源岩发育的主要影响因素.地质学报, 80(3):467-472. doi: 10.3321/j.issn:0001-5717.2006.03.021
[36] 戴金星, 邹才能, 陶士振, 等, 2007.中国大气田形成条件和主控因素.天然气地球科学, 18(4):473-484. doi: 10.3969/j.issn.1672-1926.2007.04.001
[37] 邓运华, 2009.试论中国近海两个坳陷带油气地质差异性.石油学报, 30(1):1-8. http://d.old.wanfangdata.com.cn/Periodical/syxb200901001
[38] 段谟东, 叶加仁, 吴景富, 等, 2017.东海陆架盆地西湖凹陷超压成因机制.地球科学, 42(1):119-129. https://doi.org/10.3799/dqkx.2017.009
[39] 傅宁, 邓运华, 张功成, 等, 2010.南海北部叠合断陷盆地海陆过渡相烃源岩及成藏贡献——以珠二坳陷白云凹陷为例.石油学报, 31(4):559-565. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syxb201004007
[40] 傅宁, 米立军, 张功成, 等, 2007.珠江口盆地白云凹陷烃源岩及北部油气成因.石油学报, 28(3):32-38. http://d.old.wanfangdata.com.cn/Periodical/syxb200703007
[41] 胡修棉, 王成善, 2001.古海洋溶解氧研究方法综述.地球科学进展, 16(1):65-71. doi: 10.3321/j.issn:1001-8166.2001.01.013
[42] 李天义, 何生, 杨智, 等, 2008.海相优质烃源岩形成环境及其控制因素分析.地质科技情报, 27(6):63-70. doi: 10.3969/j.issn.1000-7849.2008.06.012
[43] 李祥权, 刘金水, 陆永潮, 等, 2018.东海陆架盆地西湖凹陷花港组原型盆地性质厘定.地球科学, 43(2):502-513. https://doi.org/10.3799/dqkx.2017.596
[44] 李友川, 2015.中国近海湖相优质烃源岩形成的主要控制因素.中国海上油气, 27(3):1-9. http://d.old.wanfangdata.com.cn/Periodical/zghsyq-gc201503001
[45] 李友川, 邓运华, 张功成, 2012.中国近海海域烃源岩和油气的分带性.中国海上油气, 24(1):6-12. doi: 10.3969/j.issn.1673-1506.2012.01.002
[46] 李友川, 邓运华, 张功成, 2014.中国近海天然气富集带及气源岩形成的主要控制因素.天然气地球科学, 25(9):1309-1319. http://d.old.wanfangdata.com.cn/Periodical/trqdqkx201409002
[47] 刘春莲, 杨建林, Hans-Joachim, R., 等, 2001.影响湖相沉积岩中有机碳分布的主要因素——以三水盆地为例.沉积学报, 19(1):113-116. doi: 10.3969/j.issn.1000-0550.2001.01.019
[48] 钱焕菊, 陆现彩, 张雪芬, 等, 2009.东营凹陷沙四段上部泥质烃源岩元素地球化学及其古盐度的空间差异性.岩石矿物学杂志, 28(2):161-168. doi: 10.3969/j.issn.1000-6524.2009.02.008
[49] 苏奥, 陈红汉, 王存武, 等, 2013.东海盆地西湖凹陷油气成因及成熟度判别.石油勘探与开发, 40(5):521-527. http://d.old.wanfangdata.com.cn/Periodical/syktykf201305002
[50] 陶士振, 邹才能, 2005.东海盆地西湖凹陷天然气成藏及分布规律.石油勘探与开发, 32(4):103-110. doi: 10.3321/j.issn:1000-0747.2005.04.017
[51] 魏恒飞, 陈践发, 陈晓东, 等, 2013.西湖凹陷平湖组滨海型煤系烃源岩发育环境及其控制因素.中国地质, 40(2):487-497. doi: 10.3969/j.issn.1000-3657.2013.02.013
[52] 张功成, 2005.中国近海天然气地质特征与勘探领域.中国海上油气, 17(5):289-296. doi: 10.3969/j.issn.1673-1506.2005.05.001
[53] 张功成, 2010.南海北部陆坡深水区构造演化及其特征.石油学报, 31(4):528-533, 541. http://d.old.wanfangdata.com.cn/Periodical/syxb201004002
[54] 张功成, 2012.源热共控论.石油学报, 33(5):723-738, http://d.old.wanfangdata.com.cn/Periodical/syxb201205001
[55] 张功成, 王琪, 苗顺德, 等, 2014.中国近海海陆过渡相烃源岩二元分布模式——以珠江口盆地白云凹陷为例.天然气地球科学, 25(9):1299-1308. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=trqdqkx201409001
[56] 张国华, 张建培, 2015.东海陆架盆地构造反转特征及成因机制探讨.地学前缘, 22(1):260-270. http://d.old.wanfangdata.com.cn/Periodical/dxqy201501022
[57] 张建培, 张田, 唐贤君, 2014.东海陆架盆地类型及其形成的动力学环境.地质学报, 88(11):2033-2043. http://d.old.wanfangdata.com.cn/Periodical/dizhixb201411002
[58] 赵秀兰, 赵传本, 关学婷, 等, 1992.利用孢粉资料定量解释我国第三纪古气候.石油学报, 13(2):215-225. http://www.cnki.com.cn/Article/CJFDTOTAL-SYXB199202035.htm
[59] 赵志刚, 王鹏, 祁鹏, 等, 2016.东海盆地形成的区域地质背景与构造演化特征.地球科学, 41(3):546-554. https://doi.org/10.3799/dqkx.2016.045
[60] 钟韬, 曹冰, 刘金水, 等, 2017.西湖凹陷花港组低孔低渗砂岩储层中绿泥石环边的成因及其意义.成都理工大学学报(自然科学版), 44(6):708-716. doi: 10.3969/j.issn.1671-9727.2017.06.08
[61] 朱伟林, 2010.中国近海油气勘探进展.中国工程科学, 12(5):18-24. doi: 10.3969/j.issn.1009-1742.2010.05.003
[62] 朱扬明, 周洁, 顾圣啸, 等, 2012.西湖凹陷始新统平湖组煤系烃源岩分子地球化学特征.石油学报, 33(1):32-39. http://d.old.wanfangdata.com.cn/Periodical/syxb201201004