Su Ao, Du Jiang-min, Chen Hong-han, Yu Yan, Lei Ming-zhu . Diagenetic fluid type and activity history of controlling the development of abnormal pore zone: Taking the north margin of Baodao Sag,Qiongdongnan Basin as an example[J]. Natural Gas Geoscience, 2016 , 27(10) : 1837 -1847 . DOI: 10.11764/j.issn.1672-1926.2016.10.1837

[1]Bloch S,Lander R H,Bonnell L.Anomalously high porosity and permeability in deeply buried sandstone reservoirs:Originand predictability[J].AAPG Bulletin,2002,86(2):301-328.
[2]Schmidt V,McDonald D A.Secondary Reservoir Porosity During Sandstone Digenetic[M].Beijing:Petroleum Industry Press,1982:272-276.[沃尔特,施密特.砂岩成岩过程中的次生储集孔隙[M].北京:石油工业出版社,1982:272-276.]
[3]Surdam R C,Boese S W,Crossey L J.The chemistry of secondary porosity[J].AAPG Memoir,1984,37(2):127-149.
[4]Ramm M.Porosity-depth trends in reservoir sandstones theoretical models related toJurassic sandstones offshore Norway[J].Marine and Petroleum Geology,1992,9(5):553-567.
[5]Anna B,Susanne G,Peter K.Porosity-preserving chloritecements in shallow-marine volcaniclasticsandstones:Evidence from Cretaceous sandstones of the Sawan Gasfield,Pakistan[J].AAPG Bulletin,2009,93(5):595-615．
[6]Ehrenberg S N.Preservation of anomalous high porosity in deeplyburied sandstones by grain-coating chlorite:examples from the Norwegian continental Shelf[J].AAPG Bulletin,1993,77(7):1260-1286．
[7]Long Huashan,Xiang Caifu,Niu Jiayu,et al.Hydrothermal fluid flow and its influence on the hydrocarbon migration and accumulation along Binhai fault in Qikou Sag,Bohai Bay Basin[J].Acta Petrolei Sinica,2014,35(4):673-684.[龙华山,向才富,牛嘉玉,等.歧口凹陷滨海断裂带热流体活动及其对油气成藏的影响[J].石油学报,2014,35(4):673-684.]
[8]Bildstein R H.Worden E B.Assessment of anhydrite dissolution as therate-limiting step during thermochemical sulfate reduction[J].Chemical Geology,2001,176(1):173-189.
[9]Zhang Zhongmin,Zhu Wei,Zhao Chenglin.Evolution pattern and distribution of the secondary pores in the deep elastic reservoirs of low tertiary in Liaohe Basin[J].Journal of Daqing Petroleum Institute,2002,26(3):12-14.[张忠民,朱伟,赵澄林.辽河盆地下第三系深部碎屑岩储层次生孔隙演化模式及其分布[J].大庆石油学院学报,2002,26(3):12-14.]
[10]McMahon P B,Chapelle F H,Falls W,et al.Role ofmicrobiol processes in linkingsandstonediagenesis with organic-rich clays[J].Journal of Sedimentary Petrology,1992,62(1):1-10.
[11]Robert H G,Carlos R.Recrystallization in quartz overgrowths[J].Journal of Sedimentary Research,2002,72(3):432-440.
[12]Zhu Weilin,Zhang Gongcheng,Gao Le.Geological characteristics and exploration objectives of hydrocarbons in the northern conti- nental margin basin of South China Sea port[J].Acta Petrolei Sinica,2008,29(1):1-9.[朱伟林,张功成,高乐.南海北部大陆边缘盆地油气地质特征与勘探方向[J].石油学报,2008,29(1):1-9.]
[13]Zhao Xiaoqing.Effect of Target Layer Diagenetic Zhao Xiaoqing Joan Southeast Basin and Favorable Reservoir Prediction[D].Daqing Petroleum Institute,2010.[赵小庆.琼东南盆地目的层成岩作用研究与有利储层预测[D].大庆石油学院,2010.][JP]
[14]Ying Fengxing,Hua Dongbo,Long Yumei,et al.SY/T 5477-2003 the Industry Standard of China and Division of Diagenetic Stages in Clastic Rocks[S].Beijing:Petroleum Industry Press,2003.[应凤祥,何东博,龙玉梅,等.SY/T5477-2003中华人民共和国石油天然气行业标准:碎屑岩成岩阶段划分[S].北京:石油工业出版社,2003.]
[15]Chowdhury A H,Noble J P A.Origin,distribution and significance of carbonate cements in the Albert Formation reservoir sandstones,New Brunswick,Canada[J].Mar Petrol Geol,1996,13(7):837-846.[JP]
[16]Surdam R C,Crossey L J,Hagen E S,et al.Organic-inorganic interactions and sandstone diagenesis[J].AAPG Bulletin,1989,73(1):1-23.
[17]Jansa L F,Noguera Urrea V H.Geology and diagenetic history of overpressured sandstone reservoirs,venture gas field,offshore Nova Scotia,Canada[J].AAPG Bulletin,1990,74(10):1640-1658.
[18]Morad S,Al-Aasm I S,Ramseyer R,et al.Diagenesis of carbonate cements in Permo-Triassic sandstones from the Iberian Range,Spain:Evidence from chemical composition and stable isotopes[J].Sediment Geol.,1990,67(3):281-295.
[19]Friedman I,O’Neil J R.Compilation of Stable Isotope Fractionation Factors of Geochemical Interest[M].U.S.:Geological Survey Press,1997:1-12.
[20]Ren Jianguo,Huang Yipu,Fang Zhishan.Oxygen and hydrogen isotope composition of meteoric water in the tropical West Pacific Ocean[J].Acta Oceanologica Sinica,2000,22(5):60-64.[任建国,黄奕普,方志山,等.热带西太平洋雨水的氢氧同位素组成[J].海洋学报,2000,22:60-64.][JP]
[21]Bodnar R J.Revised equation and table for determining the freezing point depression of H2O-NaCl solutions[J].Ceochimica et Cosmochimica Acta,1993,57(3):683-684.
[22]Dai Jinxing,Song Yan,Dai Chunsen,et al.Anic Gas and Itsgas Reservoir Formation Conditions in East China[M].Beijing:Science Press,1995:17-20.[戴金星,宋岩,戴春森,等.中国东部无机成因气及其气藏形成条件[M].北京:科学出版社,1995:17-20.]
[23]Liu Kan,Sun Ying,Yu Qingchun.Characteristics of dissolution of CO2 geological storage applied to the ordovician reef limestone in Bachu area of Tarim Basin[J].Journal of Earch Sciences Environment,2013,35(3):1-4.[刘侃,孙颖,于青春.塔里木盆地巴楚地区奥陶系礁灰岩CO2地质储存的溶解溶蚀特征[J].地球科学与环境学报.2013,35(3):1-4.]
[24]How seknecht D W.Assessing the relative importance of compaction processesand cement at ion to reduction of porosity in sandstones[J].AAPG Bulletin,1987,71(6):633-642.
[25]Saigal G C,Bjrlykke K,Larter S.The effects of oil emplacementon diagenetic processes-Examples from the Fulmar reservoir sandstones,Central North Sea[J].AAPG Bulletin,1992,76(7):1024-1032.
[26]You Li,Li Wei,Li Cai,et al.Main factors affecting physical properties of deep burial reservoir in baodao area of southeast Hainan Basin[J].Special Oil and Gas Reservoirs,2014,21(3):38-40.[尤丽,李伟,李才,等.琼东南盆地宝岛区深埋藏储层物性主控因素[J].特种油气藏,2014,21(3):38-40.]