从成岩-蚀变特征探讨塔深1井白云岩储层成因
|
摘要
塔深1井钻遇的寒武系地层属于中寒武统阿瓦塔格组和上寒武统丘里塔格下亚群。阿瓦塔格组以灰色-深灰色粉晶-细晶藻白云岩为主,丘里塔格下亚群以灰色-浅灰色晶粒结构白云岩与残余亮晶结构白云岩为主。藻白云岩在阴极发光下以明亮的中等强度砖红色-桔黄色为主要特点,具有相对偏重的δ18O值(-6.3‰~-4.5‰,平均为-5.3‰,VPDB)、相对较高的稀土总量以及与正常海相碳酸盐岩相似的稀土配分样式。晶粒白云岩与残余亮晶结构白云岩在阴极发光下以偏暗的中等强度蓝紫色-砖红色为主要特点,具有相对偏轻的δ18O值(-9.2‰~-5.7‰,平均为-7.5‰,VPDB)、相对偏低的稀土总量、Eu正异常与重稀土明显亏损为特点的稀土配分模式。阿瓦塔格组和丘里塔格下亚群白云岩在上述岩石学特征和地球化学特征上的差异表明储层发育的成岩-蚀变过程存在差异。研究认为,埋藏较深的阿瓦塔格组优质储层的形成受多种因素控制,其中准同生期大气淡水作用下石膏结核的溶解及非稳定碳酸盐矿物的溶解奠定了基础,后期成岩改造及流体作用进行了强化,局部遭充填破坏。
Cambrian strata of well TS1 are composed of Awatage Formation( middle Cambrian) and the lower Qiulitage Group( upper Cambrian). A detail investigation of cores and analysis of thin sections shows that Awatage Formation is mainly composed of dark gray to gray algal dolomite( micritic to fine-crystal), and Qiulitage Group is mainly composed of gray to light gray crystalline dolomite and ghost structure dolomite. Algal dolomites are present in moderate strength with brick-red to orange colors as the main features under cathodoluminescence together withδ18 O value from-6. 3‰ to-4. 5‰( average value is-5. 3‰, VPDB), and contain a relatively high total rare earth elements( REE) with REE patterns similar to those of normal marine carbonate rocks. Crystalline dolomites and ghost dolomites show purple to red-brick color in dimly moderate strength under cathodoluminescene with lighter δ18 O value from-9. 2‰ to-5. 7‰( average value is-7. 5‰, VPDB), together with relatively low total rare earth element/positive Eu anomaly and obvious loss of HREE. The difference between Awatage Formation and Lower Qiulitage Group indicates that the diagenesis-alteration process of dolomite reservoirs is different. This study suggests that the high quality reservoir of Awatage Formation in great depth might be controlled by several factors. Among them, dissolution of gypsum nodules and other unstable minerals by meteoric water or sea water in penecontemporaneous period established the foundation, followed by diagenesis-alteration strengthening constructively with fluid action, which even damaged the space by local filling and recrystallization.
Cambrian strata of well TS1 are composed of Awatage Formation( middle Cambrian) and the lower Qiulitage Group( upper Cambrian). A detail investigation of cores and analysis of thin sections shows that Awatage Formation is mainly composed of dark gray to gray algal dolomite( micritic to fine-crystal), and Qiulitage Group is mainly composed of gray to light gray crystalline dolomite and ghost structure dolomite. Algal dolomites are present in moderate strength with brick-red to orange colors as the main features under cathodoluminescence together withδ18 O value from-6. 3‰ to-4. 5‰( average value is-5. 3‰, VPDB), and contain a relatively high total rare earth elements( REE) with REE patterns similar to those of normal marine carbonate rocks. Crystalline dolomites and ghost dolomites show purple to red-brick color in dimly moderate strength under cathodoluminescene with lighter δ18 O value from-9. 2‰ to-5. 7‰( average value is-7. 5‰, VPDB), together with relatively low total rare earth element/positive Eu anomaly and obvious loss of HREE. The difference between Awatage Formation and Lower Qiulitage Group indicates that the diagenesis-alteration process of dolomite reservoirs is different. This study suggests that the high quality reservoir of Awatage Formation in great depth might be controlled by several factors. Among them, dissolution of gypsum nodules and other unstable minerals by meteoric water or sea water in penecontemporaneous period established the foundation, followed by diagenesis-alteration strengthening constructively with fluid action, which even damaged the space by local filling and recrystallization.
引文
Cuia R D,Riva A,Scifoni A,et al.2011.Dolomite characteristics and diagenetic model of the Calcari Grigi Group(Asiago Plateau,Southern Alps-Italy):an example of multiphase dolomitization[J].Sedimentology,58(6):1 347~1 369.
Gillhaus A,Richter D K,Meijer J,et al.2001.Quantitative high resolution cathodoluminescence spectroscopy of diagenetic and hydrothermal dolomites[J].Sedimentary Geology,140:191~199.
Habermann D,Meijer J,Neuser R D,et al.1999.Micro-PIXE and quantitative cathodoluminescence spectroscopy:combined high resolution trace element analyses in minerals[J].Nuclear Instruments and Methods in Physics Research,B150:470~477.
Habermann D,Neuser R D and Richter D K.1998.Low limit of Mn2+-activated cathodoluminescence of calcite:state of the art[J].Sedimentary Geology,116:13~24.
He Zhiliang,Xu Hongjie and Duan Tiejun.2005.A preliminary analysis on compound structural styles in the Tarim polycyclic basin[J].Chinese Journal of Geology,40(2):153~166(in Chinese with English abstract).
He Dengfa,Jia Chengzao,Li Desheng,et al.2005.Formation and evolution of polycyclic superimposed Tarim Basin[J].Oil&Gas Geology,26(1):64~77(in Chinese with English abstract).
He Dengfa,Zhou Xinyuan,Zhang Chaojun,et al.2006.Characteristics of geologic framework of multicycle superimposed basin in Tarim Basin[J].China Petroleum Exploration,1:31~41(in Chinese with English abstract).
Hu Wenxuan,Chen Qi,Wang Xiaolin,et al.2010.REE models for the discrimination of fluids in the formation and evolution of dolomite reservoirs[J].Oil&Gas Geology,31(6):810~818(in Chinese with English abstract).
Huang Sijing.1992.Relationship between cathodoluminescence and concentration of iron and manganese in carbonate minerals[J].Mineralogy and Petrology,12(4):74~79(in Chinese with English abstract).
Huang Sijing.1988.The cathodoluminescence and diagenesis of the carbonates of Guanwushan formation,middle Devonian,Ganxi,northwestern Sichuan[J].Journal of Chendu College of Geology,15(1):50~56(in Chinese with English abstract).
Huang Sijing.1990.Cathodoluminescence and diagenetic alteration of marine carbonate minerals[J].Sedimentary Facies and Palaeogeography,4:9~15(in Chinese with English abstract).
Huang Sijing,Qing Hairuo,Hu Zuowei,et al.2008.Cathodoluminescence and diagenesis of the carbonate rocks in Feixianguan formation of Triassic,eastern Sichuan Basin of China[J].Earth ScienceJournal of China University of Geoscience,33(1):26~34(in Chinese with English abstract).
Jiao Cunli,He Zhiliang,Xing Xiujuan,et al.2011.Tectonic hydrothermal dolomite and its significance of reservoirs in Tarim Basin[J].Acta Petrologica Sinica,27(1):277~284(in Chinese with English abstract).
Kang Yuzhu.2005.Cases of discovery and exploration of marine fields in China(part 4):Tahe oilfield in Tarim Basin[J].Marine Origin Petroleum Geology,10(4):31~38(in Chinese with English abstract).
Li Sumei,Alon Amrani,Pang Xiongqi,et al.2015.Origin and quantitative source assessment of deep oils in the Tazhong Uplift,Tarim Basin[J].Organic Geochemistry,78:1~22.
Li Kaikai,Cai Chunfang,Cai Liulu,et al.2010.Hydrothermal fluid activities and main controlling factors of deep reservoir development in the lower Paleozoic of the Tahe oilfield[J].Petroleum Geology&Experiment,32(1):46~51(in Chinese with English abstract).
Lin Jun,Zhou Fangfang and Yuan Guofen.2010.Features of deep-burial dolomitization of the Cambrian reservoirs in Tahe region[J].Oil&Gas Geology,31(1):13~21(in Chinese with English abstract).
Liu Lihong,Huang Sijing,Wang Chunlian,et al.2010.Cathodoluminescence zonal texture of calcite cement in carbonate rock and its relationship with trace element composition:a case of Ordovician carbonate rock of Tahe oilfield,Tarim Basin[J].Marine Origin Petroleum Geology,15(1):55~60(in Chinese with English abstract).
Marshall J D.1988.Cathodoluminescence of Geological Materials[M].Boston:Unwin Hyman,146.
Meng Xianghao.2012.A research of the deep Cambrian high-quality reservoir characteristics and formation mechanism in Tahe area[D].Cheng Du:Chengdu University of Technology(in Chinese with English abstract).
Meng Xianghao,Zhang Shaonan,Li Xiuhua,et al.2010.Reservoir space in the Cambrian in the ultradeep well No.1,Tarim Basin[J].Acta Geologica Sinica of Sichuang,30(1):31~34(in Chinese with English abstract).
Meng Xianghao,Zhang Shaonan,Lin Jun,et al.2009.Geochemical tracing of istopic fluid of the Cambrian dolomite reservoir in well Tashen 1[J].Mineralogy and Petrology,29(4):75~82(in Chinese with English abstract).
Meng Xianghao,Zhang Shaonan,Lin Jun,et al.2011.Analysis on main controlling factors of Cambrian reservoir space with high quality for Well Tashen 1,the deepest subaerial well in China[J].Fault-Block Oil&Gas Field,18(1):1~5(in Chinese with English abstract).
Pagel M,Barbin V,Blanc P,et al.2000.Cathodoluminescence in Geosciences[M].Berlin Heidelberg New York Tokyo:Springer,514.
Qian Yixiong,Chen Yue,Chen Qianlu,et al.2006.General characteristics of burial dissolution for Ordovician carbonate reservoirs in the northwest of Tazhong area[J].Acta Petrolei Sinica,27(3):47~52(in Chinese with English abstract).
Qiao Jichao.2008.Research about the reservoir characteristics of the Cambrian dolomite in TS1 well,and its geochemical characteristics[D].Cheng Du:Chengdu University of Technology(in Chinese with English abstract).
Richter D K,G9tte T H,G9tze J,et al.2003.Progress in application of cathodoluminescence(CL)in sedimentary petrology[J].Mineralogy and Petrology,79:127~166.
Song Zhimin.1993.Cathololuminescence of Geology Basis[M].Wuhan:China University of Geoscience Press,43~60(in Chinese with English abstract).
Wang Lichao,Hu Wenxuan,Wang Xiaolin,et al.2014.Seawater normalized REE patterns of dolomites in Geshan and Panlongdong sections,China:Implications for tracing dolomitization and diagenetic fluids[J].Marine and Petroleum Geology,56:63~73.
Wang Tieguan,Song Daofu,Li Meijun,et al.2014.Natural gas source and deep gas exploration potential of the Ordovician Yingshan Formation in the Shunnan-Gucheng region,Tarim Basin[J].Oil&Gas Geology,35(6):753~762(in Chinese with English abstract).
Wang Xiaolin,Hu Wenxuan,Li Qing,et al.2011.Negative carbon isotope excursion on the Cambrian series 2-series 3 boundary for Penglaiba section in Tarim Basin and its significances[J].Geological Review,57(1):16~23(in Chinese with English abstract).
Wang Xiaolin,Jin Zhijun,Hu Wenxuan,et al.2009.Using in situ REEanalysis to study the origin and diagenesis of dolomite of lower Paleozoic,Tarim Basin[J].Sci.China Ser.D-Earth Sci.,39(6):721~733(in Chinese with English abstract).
Wang Zhaoming,Xie Huiwen,Chen Yongquan,et al.2014a.Discovery and exploration of Cambrian subsalt dolomite original hydrocarbon reservoir at Zhongshen-1 well in Tarim Basin[J].China Petroleum Exploration,19(2):1~13(in Chinese with English abstract).
Wang Zhaoming,Yang Haijun,Qi Yingmin,et al.2014b.Ordovician gas exploration breakthrough in the Gucheng lower uplift of the Tarim Basin and its enlightenment[J].Natural Gas Industry,34(1):1~9(in Chinese with English abstract).
Xie Xiaomin,Hu Wenxuan,Wang Xiaolin,et al.2009.Sedimentary sequences in Keping area,Xinjiang:Constraints from carbon and oxygen isotope compositions of Cambrian to Ordovician carbonate rocks[J].Geochimica,38(1):75~88(in Chinese with English abstract).
Yao Chunyan,Ma Dongsheng,Ding Haifeng,et al.2011.Reconstruction of the early Cambrian carbonate sedimentary environment in Akesu area of Xinjiang,China:Evidences from trace elements and carbon isotope excursion[J].Geochimica,40(1):63~71(in Chinese with English abstract).
Yun Lu and Zhai Xiaoxian.2008.Discussion on characteristics of the Cambrian reservoirs and hydrocarbon accumulation in well Tashen-1,Tarim Basin[J].Oil&Gas Geology,29(6):726~732(in Chinese with English abstract).
Zhai Xiaoxian,Gu Yi,Qian Yixiong,et al.2007.Geochemical characteristics of the Cambrian oil and gas in well Tashen 1,the Tarim Basin[J].Petroleum Geology&Experiment,29(4):329~333(in Chinese with English abstract).
Zhao Zongju,Luo Jiahong,Zhang Yunbo,et al.2011.Lithofacies paleogeography of Cambrian sequences in the Tarim Basin[J].Acta Petrolei Sinica,32(6):937~948(in Chinese with English abstract).
Zheng Herong,Wu Maobing,Wu Xingwei,et al.2007.Oil-gas exploration prospect of dolomite reservoir in the lower Paleozoic of Tarim Basin[J].Acta Petrolei Sinica,28(2):1~8(in Chinese with English abstract).
Zheng Jianfeng,Shen Anjiang,Liu Yongfu,et al.2013.Main controlling factors and characteristics of Cambrian dolomite reservoirs related to evaporate in Tarim Basin[J].Acta Sedimentologica Sinica,31(1):89~98(in Chinese with English abstract).
Zheng Yongfei,Zhou Gentao and Gong Bin.1997.Theoretical study of oxygen isotope fractionation in carbonate minerals[J].Geological Journal of China Universities,3(3):241~255(in Chinese with English abstract).
Zhu Dongya,Hu Wenxuan,Zhang Xuefeng,et al.2007.Characteristics of burial dissolution in the Ordovician limestone of Tahe Oilfield[J].Acta Petrolei Sinica,28(5):57~62(in Chinese with English abstract).
Zhu Dongya,Jin Zhijun,Hu Wenxuan,et al.2008.Effects of deep fluid on carbonates reservoir in Tarim basin[J].Geological Review,54(3):348~354(in Chinese with English abstract).
Zhu Dongya,Meng Qingqiang,Hu Wenxuan,et al.2012.Deep Cambrian surface-karst dolomite reservoir and its alteration by later fluid in Tarim Basin[J].Geological Review,58(4):691~701(in Chinese with English abstract).
Zhu Dongya,Meng Qingqiang,Jin Zhijun,et al.2014.Fluid environment for preservation of pore spaces in a deep dolomite reservoir[J].Geofluids,1~19.
Zhu Dongya,Meng Qingqiang,Jin Zhijun,et al.2015.Formation mechanism of deep Cambrian dolomite reservoirs in the Tarim basin,northwestern China[J].Marine and Petroleum Geology,59:232~244.
何治亮,徐宏节,段铁军.2005.塔里木多旋回盆地复合构造样式初步分析[J].地质科学,40(2):153~166.
何登发,贾承造,李德生,等.2005.塔里木多旋回叠合盆地的形成与演化[J].石油与天然气地质,26(1):64~77.
何登发,周新源,张朝军,等.2006.塔里木多旋回叠合盆地地质结构特征[J].中国石油勘探,1:31~41.
胡文瑄,陈琪,王小林,等.2010.白云岩储层形成演化过程中不同流体作用的稀土元素判别模式[J].石油与天然气地质,31(6):810~818.
黄思静.1992.碳酸盐矿物的阴极发光性与其Fe,Mn含量的关系[J].矿物岩石,12(4):74~79.
黄思静.1988.北川甘溪观雾山组碳酸盐岩的阴极发光特征和成岩作用[J].成都地质学院学报,15(1):50~56.
黄思静.1990.海相碳酸盐矿物的阴极发光性与其成岩蚀变的关系[J].岩相古地理,4:9~15.
黄思静,卿海若,胡作维,等.2008.川东三叠系飞仙关组碳酸盐岩的阴极发光特征与成岩作用[J].地球科学(中国地质大学学报),33(1):26~34.
焦存礼,何治亮,邢秀娟,等.2011.塔里木盆地构造热液白云岩及其储层意义[J].岩石学报,27(1):277~284.
康玉柱.2005.中国海相油气田勘探实例之四塔里木盆地塔河油田的发现与勘探[J].海相油气地质,10(4):31~38.
李开开,蔡春芳,蔡璐,等.2010.塔河地区下古生界热液流体及储层发育主控因素探讨---以S88和TS1井为例[J].石油实验地质,32(1):46~51.
蔺军,周芳芳,袁国芬.2010.塔河地区寒武系储层深埋藏白云石化特征[J].石油与天然气地质,31(1):13~21.
刘丽红,黄思静,王春连,等.2010.碳酸盐岩中方解石胶结物的阴极发光环带与微量元素构成的关系---以塔河油田奥陶系碳酸盐岩为例[J].海相油气地质,15(1):55~60.
孟祥豪.2012.塔河深层寒武系优质储层特征及形成机理研究[D].成都:成都理工大学.
孟祥豪,张哨楠,蔺军,等.2009.塔深1井寒武系白云岩储层同位素流体地球化学示踪[J].矿物岩石,29(4):75~82.
孟祥豪,张哨楠,李秀华,等.2010.塔深1井寒武系超深层优质储集空间特征[J].四川地质学报,30(1):31~34.
孟祥豪,张哨楠,蔺军.2011.中国陆上最深井塔深1井寒武系优质储集空间主控因素分析[J].断块油气田,18(1):1~5.
钱一雄,陈跃,陈强路,等.2006.塔中西北部奥陶系碳酸盐岩埋藏溶蚀作用[J].石油学报,27(3):47~52.
乔冀超.2008.塔深1井寒武系白云岩储层特征及其地球化学特征研究[D].成都:成都理工大学.
宋志敏.1993.阴极发光地质学基础[M].武汉:中国地质大学出版社,43~60.
王招明,谢会文,陈永权,等.2014a.塔里木盆地中深1井寒武系盐下白云岩原生油气藏的发现与勘探意义[J].中国石油勘探,19(2):1~13.
王招明,杨海军,齐英敏,等.2014b.塔里木盆地古城地区奥陶系天然气勘探重大突破及其启示[J].天然气工业,34(1):1~9.
王铁冠,宋到福,李美俊,等.2014.塔里木盆地顺南-古城地区奥陶系鹰山组天然气气源与深层天然气勘探前景[J].石油与天然气地质,35(6):753~762.
王小林,胡文瑄,李庆,等.2011.塔里木盆地蓬莱坝剖面寒武系第二统-第三统界线处碳同位素负异常及其地质意义[J].地质论评,57(1):16~23.
王小林,金之钧,胡文瑄,等.2009.塔里木盆地下古生界白云石微区REE配分特征及其成因研究[J].中国科学(D辑:地球科学),39(6):721~733.
谢小敏,胡文瑄,王小林,等.2009.新疆柯坪地区寒武纪-奥陶纪碳酸盐岩沉积旋回的碳氧同位素研究[J].地球化学,38(1):75~88.
姚春彦,马东升,丁海峰,等.2011.新疆阿克苏地区早寒武世碳酸盐岩沉积环境:微量元素和碳同位素证据[J].地球化学,40(1):63~71.
云露,翟晓先.2008.塔里木盆地塔深1井寒武系储层与成藏特征探讨[J].石油与天然气地质,29(6):726~732.
翟晓先,顾忆,钱一雄,等.2007.塔里木盆地塔深1井寒武系油气地球化学特征[J].石油实验地质,29(4):329~333.
赵宗举,罗家洪,张运波,等.2011.塔里木盆地寒武纪层序岩相古地理[J].石油学报,32(6):937~948.
郑和荣,吴茂炳,邬兴威,等.2007.塔里木盆地下古生界白云岩储层油气勘探前景[J].石油学报,28(2):1~8.
郑剑锋,沈安江,刘永福,等.2013.塔里木盆地寒武系与蒸发岩相关的白云岩储层特征及主控因素[J].沉积学报,31(1):89~98.
郑永飞,周根陶,龚冰.1997.碳酸盐矿物氧同位素分馏的理论研究[J].高校地质学报,3(3):241~255.
朱东亚,胡文瑄,张学丰,等.2007.塔河油田奥陶系灰岩埋藏溶蚀作用特征[J].石油学报,28(5):57~62.
朱东亚,金之钧,胡文瑄,等.2008.塔里木盆地深部流体对碳酸盐岩储层影响[J].地质论评,54(3):348~354.
朱东亚,孟庆强,胡文瑄,等.2012.塔里木盆地深层寒武系地表岩溶型白云岩储层及后期流体改造作用[J].地质论评,58(4):691~701.
Gillhaus A,Richter D K,Meijer J,et al.2001.Quantitative high resolution cathodoluminescence spectroscopy of diagenetic and hydrothermal dolomites[J].Sedimentary Geology,140:191~199.
Habermann D,Meijer J,Neuser R D,et al.1999.Micro-PIXE and quantitative cathodoluminescence spectroscopy:combined high resolution trace element analyses in minerals[J].Nuclear Instruments and Methods in Physics Research,B150:470~477.
Habermann D,Neuser R D and Richter D K.1998.Low limit of Mn2+-activated cathodoluminescence of calcite:state of the art[J].Sedimentary Geology,116:13~24.
He Zhiliang,Xu Hongjie and Duan Tiejun.2005.A preliminary analysis on compound structural styles in the Tarim polycyclic basin[J].Chinese Journal of Geology,40(2):153~166(in Chinese with English abstract).
He Dengfa,Jia Chengzao,Li Desheng,et al.2005.Formation and evolution of polycyclic superimposed Tarim Basin[J].Oil&Gas Geology,26(1):64~77(in Chinese with English abstract).
He Dengfa,Zhou Xinyuan,Zhang Chaojun,et al.2006.Characteristics of geologic framework of multicycle superimposed basin in Tarim Basin[J].China Petroleum Exploration,1:31~41(in Chinese with English abstract).
Hu Wenxuan,Chen Qi,Wang Xiaolin,et al.2010.REE models for the discrimination of fluids in the formation and evolution of dolomite reservoirs[J].Oil&Gas Geology,31(6):810~818(in Chinese with English abstract).
Huang Sijing.1992.Relationship between cathodoluminescence and concentration of iron and manganese in carbonate minerals[J].Mineralogy and Petrology,12(4):74~79(in Chinese with English abstract).
Huang Sijing.1988.The cathodoluminescence and diagenesis of the carbonates of Guanwushan formation,middle Devonian,Ganxi,northwestern Sichuan[J].Journal of Chendu College of Geology,15(1):50~56(in Chinese with English abstract).
Huang Sijing.1990.Cathodoluminescence and diagenetic alteration of marine carbonate minerals[J].Sedimentary Facies and Palaeogeography,4:9~15(in Chinese with English abstract).
Huang Sijing,Qing Hairuo,Hu Zuowei,et al.2008.Cathodoluminescence and diagenesis of the carbonate rocks in Feixianguan formation of Triassic,eastern Sichuan Basin of China[J].Earth ScienceJournal of China University of Geoscience,33(1):26~34(in Chinese with English abstract).
Jiao Cunli,He Zhiliang,Xing Xiujuan,et al.2011.Tectonic hydrothermal dolomite and its significance of reservoirs in Tarim Basin[J].Acta Petrologica Sinica,27(1):277~284(in Chinese with English abstract).
Kang Yuzhu.2005.Cases of discovery and exploration of marine fields in China(part 4):Tahe oilfield in Tarim Basin[J].Marine Origin Petroleum Geology,10(4):31~38(in Chinese with English abstract).
Li Sumei,Alon Amrani,Pang Xiongqi,et al.2015.Origin and quantitative source assessment of deep oils in the Tazhong Uplift,Tarim Basin[J].Organic Geochemistry,78:1~22.
Li Kaikai,Cai Chunfang,Cai Liulu,et al.2010.Hydrothermal fluid activities and main controlling factors of deep reservoir development in the lower Paleozoic of the Tahe oilfield[J].Petroleum Geology&Experiment,32(1):46~51(in Chinese with English abstract).
Lin Jun,Zhou Fangfang and Yuan Guofen.2010.Features of deep-burial dolomitization of the Cambrian reservoirs in Tahe region[J].Oil&Gas Geology,31(1):13~21(in Chinese with English abstract).
Liu Lihong,Huang Sijing,Wang Chunlian,et al.2010.Cathodoluminescence zonal texture of calcite cement in carbonate rock and its relationship with trace element composition:a case of Ordovician carbonate rock of Tahe oilfield,Tarim Basin[J].Marine Origin Petroleum Geology,15(1):55~60(in Chinese with English abstract).
Marshall J D.1988.Cathodoluminescence of Geological Materials[M].Boston:Unwin Hyman,146.
Meng Xianghao.2012.A research of the deep Cambrian high-quality reservoir characteristics and formation mechanism in Tahe area[D].Cheng Du:Chengdu University of Technology(in Chinese with English abstract).
Meng Xianghao,Zhang Shaonan,Li Xiuhua,et al.2010.Reservoir space in the Cambrian in the ultradeep well No.1,Tarim Basin[J].Acta Geologica Sinica of Sichuang,30(1):31~34(in Chinese with English abstract).
Meng Xianghao,Zhang Shaonan,Lin Jun,et al.2009.Geochemical tracing of istopic fluid of the Cambrian dolomite reservoir in well Tashen 1[J].Mineralogy and Petrology,29(4):75~82(in Chinese with English abstract).
Meng Xianghao,Zhang Shaonan,Lin Jun,et al.2011.Analysis on main controlling factors of Cambrian reservoir space with high quality for Well Tashen 1,the deepest subaerial well in China[J].Fault-Block Oil&Gas Field,18(1):1~5(in Chinese with English abstract).
Pagel M,Barbin V,Blanc P,et al.2000.Cathodoluminescence in Geosciences[M].Berlin Heidelberg New York Tokyo:Springer,514.
Qian Yixiong,Chen Yue,Chen Qianlu,et al.2006.General characteristics of burial dissolution for Ordovician carbonate reservoirs in the northwest of Tazhong area[J].Acta Petrolei Sinica,27(3):47~52(in Chinese with English abstract).
Qiao Jichao.2008.Research about the reservoir characteristics of the Cambrian dolomite in TS1 well,and its geochemical characteristics[D].Cheng Du:Chengdu University of Technology(in Chinese with English abstract).
Richter D K,G9tte T H,G9tze J,et al.2003.Progress in application of cathodoluminescence(CL)in sedimentary petrology[J].Mineralogy and Petrology,79:127~166.
Song Zhimin.1993.Cathololuminescence of Geology Basis[M].Wuhan:China University of Geoscience Press,43~60(in Chinese with English abstract).
Wang Lichao,Hu Wenxuan,Wang Xiaolin,et al.2014.Seawater normalized REE patterns of dolomites in Geshan and Panlongdong sections,China:Implications for tracing dolomitization and diagenetic fluids[J].Marine and Petroleum Geology,56:63~73.
Wang Tieguan,Song Daofu,Li Meijun,et al.2014.Natural gas source and deep gas exploration potential of the Ordovician Yingshan Formation in the Shunnan-Gucheng region,Tarim Basin[J].Oil&Gas Geology,35(6):753~762(in Chinese with English abstract).
Wang Xiaolin,Hu Wenxuan,Li Qing,et al.2011.Negative carbon isotope excursion on the Cambrian series 2-series 3 boundary for Penglaiba section in Tarim Basin and its significances[J].Geological Review,57(1):16~23(in Chinese with English abstract).
Wang Xiaolin,Jin Zhijun,Hu Wenxuan,et al.2009.Using in situ REEanalysis to study the origin and diagenesis of dolomite of lower Paleozoic,Tarim Basin[J].Sci.China Ser.D-Earth Sci.,39(6):721~733(in Chinese with English abstract).
Wang Zhaoming,Xie Huiwen,Chen Yongquan,et al.2014a.Discovery and exploration of Cambrian subsalt dolomite original hydrocarbon reservoir at Zhongshen-1 well in Tarim Basin[J].China Petroleum Exploration,19(2):1~13(in Chinese with English abstract).
Wang Zhaoming,Yang Haijun,Qi Yingmin,et al.2014b.Ordovician gas exploration breakthrough in the Gucheng lower uplift of the Tarim Basin and its enlightenment[J].Natural Gas Industry,34(1):1~9(in Chinese with English abstract).
Xie Xiaomin,Hu Wenxuan,Wang Xiaolin,et al.2009.Sedimentary sequences in Keping area,Xinjiang:Constraints from carbon and oxygen isotope compositions of Cambrian to Ordovician carbonate rocks[J].Geochimica,38(1):75~88(in Chinese with English abstract).
Yao Chunyan,Ma Dongsheng,Ding Haifeng,et al.2011.Reconstruction of the early Cambrian carbonate sedimentary environment in Akesu area of Xinjiang,China:Evidences from trace elements and carbon isotope excursion[J].Geochimica,40(1):63~71(in Chinese with English abstract).
Yun Lu and Zhai Xiaoxian.2008.Discussion on characteristics of the Cambrian reservoirs and hydrocarbon accumulation in well Tashen-1,Tarim Basin[J].Oil&Gas Geology,29(6):726~732(in Chinese with English abstract).
Zhai Xiaoxian,Gu Yi,Qian Yixiong,et al.2007.Geochemical characteristics of the Cambrian oil and gas in well Tashen 1,the Tarim Basin[J].Petroleum Geology&Experiment,29(4):329~333(in Chinese with English abstract).
Zhao Zongju,Luo Jiahong,Zhang Yunbo,et al.2011.Lithofacies paleogeography of Cambrian sequences in the Tarim Basin[J].Acta Petrolei Sinica,32(6):937~948(in Chinese with English abstract).
Zheng Herong,Wu Maobing,Wu Xingwei,et al.2007.Oil-gas exploration prospect of dolomite reservoir in the lower Paleozoic of Tarim Basin[J].Acta Petrolei Sinica,28(2):1~8(in Chinese with English abstract).
Zheng Jianfeng,Shen Anjiang,Liu Yongfu,et al.2013.Main controlling factors and characteristics of Cambrian dolomite reservoirs related to evaporate in Tarim Basin[J].Acta Sedimentologica Sinica,31(1):89~98(in Chinese with English abstract).
Zheng Yongfei,Zhou Gentao and Gong Bin.1997.Theoretical study of oxygen isotope fractionation in carbonate minerals[J].Geological Journal of China Universities,3(3):241~255(in Chinese with English abstract).
Zhu Dongya,Hu Wenxuan,Zhang Xuefeng,et al.2007.Characteristics of burial dissolution in the Ordovician limestone of Tahe Oilfield[J].Acta Petrolei Sinica,28(5):57~62(in Chinese with English abstract).
Zhu Dongya,Jin Zhijun,Hu Wenxuan,et al.2008.Effects of deep fluid on carbonates reservoir in Tarim basin[J].Geological Review,54(3):348~354(in Chinese with English abstract).
Zhu Dongya,Meng Qingqiang,Hu Wenxuan,et al.2012.Deep Cambrian surface-karst dolomite reservoir and its alteration by later fluid in Tarim Basin[J].Geological Review,58(4):691~701(in Chinese with English abstract).
Zhu Dongya,Meng Qingqiang,Jin Zhijun,et al.2014.Fluid environment for preservation of pore spaces in a deep dolomite reservoir[J].Geofluids,1~19.
Zhu Dongya,Meng Qingqiang,Jin Zhijun,et al.2015.Formation mechanism of deep Cambrian dolomite reservoirs in the Tarim basin,northwestern China[J].Marine and Petroleum Geology,59:232~244.
何治亮,徐宏节,段铁军.2005.塔里木多旋回盆地复合构造样式初步分析[J].地质科学,40(2):153~166.
何登发,贾承造,李德生,等.2005.塔里木多旋回叠合盆地的形成与演化[J].石油与天然气地质,26(1):64~77.
何登发,周新源,张朝军,等.2006.塔里木多旋回叠合盆地地质结构特征[J].中国石油勘探,1:31~41.
胡文瑄,陈琪,王小林,等.2010.白云岩储层形成演化过程中不同流体作用的稀土元素判别模式[J].石油与天然气地质,31(6):810~818.
黄思静.1992.碳酸盐矿物的阴极发光性与其Fe,Mn含量的关系[J].矿物岩石,12(4):74~79.
黄思静.1988.北川甘溪观雾山组碳酸盐岩的阴极发光特征和成岩作用[J].成都地质学院学报,15(1):50~56.
黄思静.1990.海相碳酸盐矿物的阴极发光性与其成岩蚀变的关系[J].岩相古地理,4:9~15.
黄思静,卿海若,胡作维,等.2008.川东三叠系飞仙关组碳酸盐岩的阴极发光特征与成岩作用[J].地球科学(中国地质大学学报),33(1):26~34.
焦存礼,何治亮,邢秀娟,等.2011.塔里木盆地构造热液白云岩及其储层意义[J].岩石学报,27(1):277~284.
康玉柱.2005.中国海相油气田勘探实例之四塔里木盆地塔河油田的发现与勘探[J].海相油气地质,10(4):31~38.
李开开,蔡春芳,蔡璐,等.2010.塔河地区下古生界热液流体及储层发育主控因素探讨---以S88和TS1井为例[J].石油实验地质,32(1):46~51.
蔺军,周芳芳,袁国芬.2010.塔河地区寒武系储层深埋藏白云石化特征[J].石油与天然气地质,31(1):13~21.
刘丽红,黄思静,王春连,等.2010.碳酸盐岩中方解石胶结物的阴极发光环带与微量元素构成的关系---以塔河油田奥陶系碳酸盐岩为例[J].海相油气地质,15(1):55~60.
孟祥豪.2012.塔河深层寒武系优质储层特征及形成机理研究[D].成都:成都理工大学.
孟祥豪,张哨楠,蔺军,等.2009.塔深1井寒武系白云岩储层同位素流体地球化学示踪[J].矿物岩石,29(4):75~82.
孟祥豪,张哨楠,李秀华,等.2010.塔深1井寒武系超深层优质储集空间特征[J].四川地质学报,30(1):31~34.
孟祥豪,张哨楠,蔺军.2011.中国陆上最深井塔深1井寒武系优质储集空间主控因素分析[J].断块油气田,18(1):1~5.
钱一雄,陈跃,陈强路,等.2006.塔中西北部奥陶系碳酸盐岩埋藏溶蚀作用[J].石油学报,27(3):47~52.
乔冀超.2008.塔深1井寒武系白云岩储层特征及其地球化学特征研究[D].成都:成都理工大学.
宋志敏.1993.阴极发光地质学基础[M].武汉:中国地质大学出版社,43~60.
王招明,谢会文,陈永权,等.2014a.塔里木盆地中深1井寒武系盐下白云岩原生油气藏的发现与勘探意义[J].中国石油勘探,19(2):1~13.
王招明,杨海军,齐英敏,等.2014b.塔里木盆地古城地区奥陶系天然气勘探重大突破及其启示[J].天然气工业,34(1):1~9.
王铁冠,宋到福,李美俊,等.2014.塔里木盆地顺南-古城地区奥陶系鹰山组天然气气源与深层天然气勘探前景[J].石油与天然气地质,35(6):753~762.
王小林,胡文瑄,李庆,等.2011.塔里木盆地蓬莱坝剖面寒武系第二统-第三统界线处碳同位素负异常及其地质意义[J].地质论评,57(1):16~23.
王小林,金之钧,胡文瑄,等.2009.塔里木盆地下古生界白云石微区REE配分特征及其成因研究[J].中国科学(D辑:地球科学),39(6):721~733.
谢小敏,胡文瑄,王小林,等.2009.新疆柯坪地区寒武纪-奥陶纪碳酸盐岩沉积旋回的碳氧同位素研究[J].地球化学,38(1):75~88.
姚春彦,马东升,丁海峰,等.2011.新疆阿克苏地区早寒武世碳酸盐岩沉积环境:微量元素和碳同位素证据[J].地球化学,40(1):63~71.
云露,翟晓先.2008.塔里木盆地塔深1井寒武系储层与成藏特征探讨[J].石油与天然气地质,29(6):726~732.
翟晓先,顾忆,钱一雄,等.2007.塔里木盆地塔深1井寒武系油气地球化学特征[J].石油实验地质,29(4):329~333.
赵宗举,罗家洪,张运波,等.2011.塔里木盆地寒武纪层序岩相古地理[J].石油学报,32(6):937~948.
郑和荣,吴茂炳,邬兴威,等.2007.塔里木盆地下古生界白云岩储层油气勘探前景[J].石油学报,28(2):1~8.
郑剑锋,沈安江,刘永福,等.2013.塔里木盆地寒武系与蒸发岩相关的白云岩储层特征及主控因素[J].沉积学报,31(1):89~98.
郑永飞,周根陶,龚冰.1997.碳酸盐矿物氧同位素分馏的理论研究[J].高校地质学报,3(3):241~255.
朱东亚,胡文瑄,张学丰,等.2007.塔河油田奥陶系灰岩埋藏溶蚀作用特征[J].石油学报,28(5):57~62.
朱东亚,金之钧,胡文瑄,等.2008.塔里木盆地深部流体对碳酸盐岩储层影响[J].地质论评,54(3):348~354.
朱东亚,孟庆强,胡文瑄,等.2012.塔里木盆地深层寒武系地表岩溶型白云岩储层及后期流体改造作用[J].地质论评,58(4):691~701.