Zhang De-min, Bao Zhi-dong, Hao Yan, Yang Fei, Chen Min, Zhong Xiang-yun . Formation model of high-quality reservoirs within Cambrian buried hillin Yaha-Yingmaili area,Tarim Basin[J]. Natural Gas Geoscience, 2016 , 27(10) : 1797 -1807 . DOI: 10.11764/j.issn.1672-1926.2016.10.1797

[1]Huang Sijing,Zhang Xuehua,Liu Lihong,et al.Progress of research on carbonate diagenesis[J].Earth Science Frontiers,2009,16(5):219-231.[黄思静,张雪花,刘丽红,等.碳酸盐岩成岩作用研究现状与前瞻[J].地学前缘,2009,16(5):219-231.]
[2]Liu Hongjun,Jia Yani,Li Zhenhong,et al.Existence and significance of microumbones in karst basin:sample from Ordovician karstic paleogeomorphy in Ordos Basin[J].Natural Gas Geoscience,2006,17(4):490-493.[刘洪军,贾亚妮,李振宏,等.岩溶盆地中微隆起带的存在即意义__以鄂尔多斯盆地奥陶纪岩溶古地貌为例[J].天然气地球科学,2007,25(6):858-868.][JP]
[3]Wang Zhaoming,Zhang Lijuan,Sun Chonghao.Classification,period and exploration for carbonate karst in the Ordovician,Tarim Basin[J].Journal of Paleogeography,2015,17(5):635-644.[王招明,张丽娟,孙崇浩.塔里木盆地奥陶系碳酸盐岩岩溶分类、期次及勘探思路[J].古地理学报,2015,17(5):635-644.][JP]
[4]Zhang Baomin,Liu Jingjiang.Classification and characteristics of karst reservoirs in China and related theories[J].Petroleum Exploration and Development,2009,36(1):12-29.[张宝民,刘静江.中国岩溶储集层分类与特征及相关的理论问题[J].石油勘探与开发,2009,36(1):12-29.]
[5]Qian Yixiong,Conxita Taberner,Zou Senlin,et al.Diagenesis comparison between epigenic karstification and burial dissolution in carbonate reservoirs:An instance of ordovician carbonate reservoirs in Tabei and Tazhong regions,Tarim Basin[J].Marine Origin Petroleum Geology,2007,12(2):1-7.[钱一雄,Conxita Taberner,邹森林,等.碳酸盐岩表生岩溶与埋藏溶蚀比较——以塔北和塔中地区为例[J].海相油气地质,2007,12(2):1-7.][JP]
[6]Liu Cunge,Li Guorong,Zhang Yiwei,et al.Application of strontium isotope to the study of paleokarst:An case from Ordovician in the Tahe Oilfield,Tarim Basin[J].Acta Geologica Sinica,2007,81(10):1398-1406.[刘存革,李国蓉,张一伟,等.锶同位素在古岩溶研究中的应用——以塔河油田奥陶系为例[J].地质学报,2007,81(10):1398-1406.]
[7]Shi Shuyuan,Hu Suyun,Liu Wei,et al.Distinguishing paleokarst period by intergrating carbon oxygen isotopes and fluid inclusion characteristics[J].Natural Gas Geoscience,2015,26(2):208-217.[石书缘,胡素云,刘伟,等.综合运用碳氧同位素和包裹体信息判别古岩溶形成期次[J].天然气地球科学,2015,26(2):208-217.]
[8]Zhang Tao,Cai Xiyuan.Caledonian paleo-karstification and its characteristics in Tahe area,Tarim Basin[J].Acta Geologica Sinica,2007,81(8):1125-1134.[张涛,蔡希源.塔河地区加里东中期岩溶作用及分布模式[J].地质学报,2007,81(8):1125-1134.]
[9]Xia Riyuan,Tang Jiansheng,Zou Shengzhang,et al.Palaeo-karst research of the carbonate oil-gas field and its application to oil-gas exploration and development[J].Acta Geoscientica Sinica,2006,27(5):503-509.[夏日元,唐建生,邹胜章,等.碳酸盐岩油气田古岩溶研究及其在油气勘探开发中的应用[J].地球学报,2006,27(5):503-509.]
[10]Qiao Zhanfeng,Shen Anjiang,Zou Weihong,et al.A fault-controlled non-exposed meteoric karstification:A case study of Ordovician carbonate reservoir at structure YM2 in northern Tarim Basin,northwest China[J].Acta Geologica Sinica,2011,85(12):2070-2083.[乔占峰,沈安江,邹伟宏,等.断裂控制的非暴露型大气水岩溶作用模式——以塔北英买2构造奥陶系碳酸盐岩储层为例[J].地质学报,2011,85(12):2070-2083.][JP]
[11]He Jinyou,Jia Chengzao,Wu Guanghui,et al.Characteristics and model of Sinian weathering paleo-karst in Aksu area,Xinjiang.[J].Acta Petrologica Sinica,2010,26(8):2513-2518.[何金有,贾承造,邬光辉,等.新疆阿克苏地区震旦系风化壳古岩溶特征及其发育模式[J].岩石学报,2010,26(8):2513-2518.]
[12]Shen Anjiang,Pan Wenqing,Zheng Xingping,et al.Types and characteristics of Lower Paleozoic karst reservoir in Tarim Basin[J].Marine Origin Petroleum Geology,2010,15(2):20-29.[沈安江,潘文庆,郑兴平,等.塔里木盆地下古生界岩溶型储层类型及特征[J].海相油气地质,2010,15(2):20-29.]
[13]Ouyang Yonglin,Ma Xiaoming,Guo Xiaolong,et al.Prediction of ancient weathering crust karst reservoirs using separate frequency seismic attributes[J].Natural Gas Geoscience,2008,19(3):381-384.[欧阳永林,马小明,郭晓龙,等.利用分频地震属性进行古风化壳岩溶储层预测__以千米桥潜山凝析气田为例[J].天然气地球科学,2008,19(3):381-384.]
[14]Wang Buqing,Huang Zhibin,Ma Peiling,et al.Establishment of division standard,evidence and principle of structural units in Tarim Basin[J].Geotectonica et Metallogenia,2009,33(1):86-93.[王步清,黄志斌,马培领,等.塔里木盆地构造单元划分标准、依据和原则的建立[J].大地构造与成矿学,2009,33(1):86-93.][JP]
[15]Xu Guoqiang,Liu Shugen,Li Guorong,et al.Comparison of tectonic evolutions and petroleum geological conditions in Tazhong and Tabei paloehighs in Tarim Basin[J].Oil & Gas Geology,2005,26(1):114-129.[徐国强,刘树根,李国蓉,等.塔中、塔北古隆起形成演化及油气地质条件对比[J].石油与天然气地质,2005,26(1):114-129.]
[16]An Haiting,Li Haiyin,Wang Jianzhong,et al.Tectonic evolution and its controlling on oil and gas accumulation in the northern Tarim Basin[J].Geotectonica et Metallogenia,2009,33(1):142-147.[安海亭,李海银,王建忠,等.塔里木盆地北部地区构造和演化特征及其对油气成藏的控制[J].大地构造与成矿学,2009,33(1):142-147.]
[17]Zhang Demin,Bao Zhidong,Pan Wenqing,et al.Type and origin of the Lower Paleozoic dolostones in Tarim Basin[J].Journal of Paleogeography,2013,15(5):693-706.[张德民,鲍志东,潘文庆,等.塔里木盆地下古生界白云岩类型及成因[J].古地理学报,2013,15(5):693-706.]
[18]Su Zhongtang,Chen Hongde,Xu Fenyan,et al.Geochemistry and dolomitization mechanism of Majiagou dolomites in Ordovician[J].Acta Petrogica Sinica,2011,27(8):2230-2238.[苏中堂,陈洪德，徐粉燕,等.鄂尔多斯盆地马家沟组白云岩地球化学特征及白云岩化机制分析[J].岩石学报,2011,27(8):2230-2238.]
[19]Shao Longyi,He Hong,Peng Suping,et al.Types and origin of dolostones of the Cambrian and Ordovician of Bachu Uplift area in Tarim Basin[J].Journal of Paleogeography,2002,4(2):19-28.[邵龙义,何宏,彭苏萍,等.塔里木盆地巴楚隆起寒武系及奥陶系白云岩类型及形成机理[J].古地理学报,2002,4(2):19-28.]
[20]Davies G R,Smith L B.Structurally controlled hydrothermal dolomite reservoir facies:An overview[J].AAPG Bulletin,2006,90(11):5-109.
[21]Amel H,Jafarian A,Husinec A,et al.Microfacies,depositional environment and diagenetic evolution controls on the reservoir quality of the Permian upper Dalan Formation,Kish Gasfield,Zagros basin[J].Marine and Petroleum Geology,2015,67:57-71.
[22]Ma Yongsheng,Cai Xunyu,Zhao Peirong,et al.Formation mechanism of deep-buried carbonate reservoir and its model of Three-Element controlling reservoir:A case study from the Puguang Oilfield in Sichuan[J].Acta Geologica Sinica,2010,84(8):1087-1094.[马永生,蔡勋育,赵培荣,等.深层—超深层碳酸盐岩优质储层发育机理和“三元控储”模式[J].地质学报,2010,84(8):1087-1094.]
[23]Liu Shugen,Ma Yongsheng,Wang Guozhi,et al.Formation and conservation mechanism of the high-quality reservoirs in Sinian-Lower Paleozoic Sichuan Basin[J].Petroleum Geology and Recovery Efficiency,2008,15(1):1-5.[刘树根,马永生，王国芝,等.四川盆地震旦系—下古生界优质储层形成与保存机理.油气地质与采收率[J],2008,15(1):1-5.]
[24]Chen Hanlin,Yang Shufeng,Jia Chengzao,et al.Confirmation of Permian intermediate-acid igneous rock zone and a new understanding of tectonic evolution in the northern part of the Tarim Basin[J].Acta Mineralogica Sinica,1998,18(2):370-376.[陈汉林，杨树锋,贾承造,等.塔里木盆地北部二叠纪中酸性火成岩带的厘定及其对塔北构造演化的新认识[J].矿物学报,1998,18(2):370-376.]
[25]Li Yong,Su Wen,Kong Ping,et al.Zircon U-Pb ages of the early Permian magmatic rocks in the Tazhong-Bachu region,Tarim Basin by LA-ICP-MS[J].Acta Petrologica Sinica,2007,23(5):1097-1107.[李勇,苏文,孔屏,等.塔里木盆地塔中—巴楚地区早二叠世岩浆岩的LA-ICP-MS锆石U-Pb年龄[J].岩石学报,2007,23(5):1097-1107.]
[26]Sun Bonian.Disscussion on the northern Tarim Basin Permian phytogeographical department[M]//Jia Runxu.China North Tarim Basin Oil and Gas Geological Research.Beijing:China University of Geosciences Press,1991:115-124.[孙柏年.塔里木盆地北缘二叠纪植物地理区系探讨[M]//贾润胥主编.中国塔里木盆地北部油气地质研究.北京:中国地质大学出版社,1991:115-124.]
[27]Yang Shufeng,Chen Hanlin,Li Zilong,et al.Early Permian Tarim Large Igneous Province in northwest China[J].Science China:Earth Sciences,2014,44(2):187-199.[杨树锋,陈汉林，厉子龙,等.塔里木早二叠世大火成岩省[J].中国科学：地球科学 2014,44(2):187-199.]
[28]Zhu Dongya,Hu Wenxuan,Zhang Xuefeng,et al.Characteristics of burial dissolution in the Ordovician limestone of Tahe Oilfield[J].Acta Petrolei Sinica,2007,28(5):57-62.[朱东亚,胡文瑄，张学丰,等.塔河油田奥陶系灰岩埋藏溶蚀作用特征[J].石油学报,2007,28(5):57-62.]
[29]Hu Mingyi,Cai Xiyao,Hu Zhonggui,et al.Deep buried dissolution of Ordovician carbonates in Tazhong area of Tarim Basin[J].Journal of Oil and Gas Technology,2009,31(6):49-54.[胡明毅,蔡习尧，胡忠贵,等.塔中地区奥陶系碳酸盐岩深部埋藏溶蚀作用研究[J].石油天然气学报:江汉石油学院学报,2009,31(6):49-54.]
[30]Jin Zhijun,Zhu Dongya,Hu Wenxuan,et al.Geological and geochemical Signatures of hydrothermal activity and their influence on carbonate reservoir beds in the Tarim Basin[J].Acta Geologica Sinica,2006,80(2):245-253.[金之钧,朱东亚，胡文瑄,等.塔里木盆地热液活动地质地球化学特征及其对储层影响[J].地质学报,2006,80(2):245-253.]