作者:雷和金;李国蓉;周吉羚;高鱼伟;申滔;符浩;李辉; 时间:2015-01-01 点击数:
雷和金;李国蓉;周吉羚;高鱼伟;申滔;符浩;李辉;
1:成都理工大学能源学院
2:成都理工大学油气藏地质及开发工程国家重点实验室
摘要(Abstract):
利用岩心、薄片资料,结合碳氧同位素地化数据,分析四川盆地南部寒武系碳酸盐岩成岩作用类型并探讨储渗空间的意义.结果表明:研究区成岩作用类型主要为海底胶结作用、白云石化作用、溶蚀作用、压实压溶作用、破裂作用和充填作用等.白云石化作用是优质储层形成的基础,溶蚀作用是关键.埋藏期白云石化形成晶间孔,表生期溶蚀发育膏模孔、晶间溶孔.热液溶蚀形成的热液溶蚀缝洞及热液破裂作用为储层提供有效储渗空间,多期次的白云石化及溶蚀作用为研究区储层形成的主控因素.
关键词(KeyWords):碳酸盐岩;成岩作用;碳氧同位素;储层;寒武系;四川盆地
Abstract:
Keywords:
基金项目(Foundation):国家科技重大专项(2011ZX05005);; 国家自然科学基金项目(41272150)
作者(Author):雷和金;李国蓉;周吉羚;高鱼伟;申滔;符浩;李辉;
Email:
参考文献(References):
[1]Choquette P W,Pray L C.Geologic nomenclature and classification of porosity in sedimentary carbonatese[J].American Association Petroleum Geologists Bulletin,1970,54(2):207-250.
[2]Ahr W M.Early diagenetic microporosity in the Cotton Valley limestone of east Texas[J].Sedimentary Geology,1989,63(3/4):275-292.
[3]Budd D A.Micro-rhombic calcite and microporosity in limestones:A geochemical study of the lower Cretaceous Thamama group,U.A.E[J].Sedimentary Geology,1989,63(3/4):293-311.
[4]Moshier S O.Microporosity in micriticlimestones:A review[J].Sedimentary Geology,1989,63(3/4):191-213.
[5]Heydari E.Porosity loss fluid flow,and mass transfer in limestone reservoirs application to the upper Jurassic smackover formation,mississippi[J].American Association Petroleum Geologists Bulletin,2000,84(1):100-118.
[6]艾华国,兰林英,张克银.塔里木盆地不整合面下的碳酸盐岩成岩作用及孔隙特征[J].新疆石油地质,1998,19(2):112-120.Ai Huaguo,Lan Linying,Zhang Keyin.Origin classification of carbon and hydrogen isotopes and their distribution regular in Tarim basin[J].Xinjiang Petroleum Geology,1998,19(2):112-120.
[7]杜叶龙,李双应,王冰,等.安徽无为—巢湖地区中下二叠统碳酸盐岩成岩作用[J].地质学报,2011,85(4):544-549.Du Yelong,Li Shuangying,Wang Bing,et al.Diagenesis of the Lower-Middle Permian Carbonate in the Wuwei—Chaohu area,Anhui province[J].Acta Geologica Sinica,2011,85(4):544-549.
[8]邹才能,杜金虎,徐春春,等.四川盆地震旦系—寒武系特大型气田形成分布、资源潜力及勘探发现[J].石油勘探与开发,2014,40(3):279-293.Zou Caineng,Du Jinhu,Xu Chunchun,et al.Formation,distribution,resource potential and discovery of the Sinian Cambrian giant gas field,Sichuan basin,SW China[J].Petroleum Exploration and Development,2014,40(3):279-293.
[9]徐春春,沈平,杨跃明,等.乐山—龙女寺古隆起震旦系—下寒武统龙王庙组天然气成藏条件与富集规律[J].天然气工业,2014,34(3):1-6.Xu Chunchun,Shen Ping,Yang Yueming,et al.Accumulation conditions and enrichment patterns of natural gas in the Lower Cambrian Longwangmiao formation reservoirs of the Leshan-Longnusi paleohigh Sichuan basin[J].Natural Gas Industry,2014,34(3):1-6.
[10]袁立,姚君波,李国蓉,等.四川盆地中一七寒武统层序地层划分与沉积模式[J].海相油气地质,2013,18(3):19-27.Yuan Li,Yao Junbo,Li Guorong,et al.Division and sedimentary model of middle-upper Cambrian sequence strata in Sichuan basin[J].Marine Origin Petroleum Geology,2013,18(3):19-27.
[11]徐世琦,张光荣,王欣.古隆起带寒武系洗象池群油气勘探前景分析[J].天然气勘探与开发,2006,29(4):4-8.Xu Shiqi,Zhang Guangrong,Wang Xin.Oil-gas exploration prospect analysis of Cambrian Xixiangchi group in paleouplift belt[J].Petroleum Exploration and Development,2006,29(4):4-8.
[12]范筱聪,孟祥豪,徐梅桂,等.巴麦地区石炭系小海子组储层特征及控制因素分析[J].东北石油大学学报,2012,36(4):19-23.Fan Xiaocong,Meng Xianghao,Xu Meigui,et al.Reservior characteristics of Carboniferous Xiaohaizi formation in Bamai region and their main control factors[J].Journal of Northest Petroleum University,2012,36(4):19-23.
[13]邓长瑜,张秀莲,陈建文,等.黔东南地区寒武系碳酸盐岩成岩作用分析[J].沉积学报,2004,22(4):590-594.Deng Changyu,Zhang Xiulian,Chen Jianwen,et al.The analysis of sequence stratigraphy and diagenesis for the carbonates of Cambrian in the southeast of Guizhou province[J].Scta Sedimentologica Sinica,2004,22(4):590-594.
[14]黄文明,刘树根,马文辛,等.深层海相碳酸盐岩优质储层的形成、保存和破坏机制——以四川盆地震旦系一志留系为例[J].地质科学,2011,46(3):875-895.Huang Wenming,Liu Shugen,Ma Wenxin,et al.Lower paleozoic carbonate diagenesis feature and controlling over reservoirs in southern north China[J].Chines Journal of Geology,2011,46(3):875-895.
[15]姜超,邓爱居,李凤群,等.饶阳凹陷武强地区沙二—沙三段储层成岩作用分析[J].东北石油大学学报,2014,38(5):1-6.Jiang Chao,Deng Aiju,Li Fengqun,et al.Diagenesis analysis of reservoirs in Es2and Es3in Wuqiang area of Raoyang sag[J].Journal of Northest Petroleum University,2014,38(5):1-6.
[16]林小兵,李国忠,田景春,等.黔南石炭系层序地层格架中碳酸盐岩成岩作用研究[J].成都理工大学学报:自然科学版,2007,34(3):268-271.Lin Xiaobing,Li Guozhong,Tian Jingchun,et al.Study on diagenesis of the carbonate rocks in the Carboniferous sequence stratigraphic framework of south Guizhou[J].Journal of Chengdu University of Technology:Science&Technology Edition,2007,34(3):268-271.
[17]杨伟,胡明毅,宋海敬,等.四川盆地南部中一上寒武统储层成岩作用[J].海相油气地质,2008,13(4):30-35.Yang Wei,Hu Mingyi,Song Haijing,et al.Diagenesis of middleand upper Cambrian reservoirs in southern part of Sichuan basin[J].Marine Origin Petroleum Geology,2008,13(4):30-35.
[18]时国,田景春,吴永良,等.南华北地区下古生界碳酸盐岩成岩作用及其对储层的影响[J].地质科技情报,2010,29(2):11-14.Shi Guo,Tian Jingchun,Wu Yongliang,et al.Lower Paleozoic carbonate diagenesis feature and controlling over reservoirs in southern north China[J].Geological Science and Technology Information,2010,29(2):11-14.
[19]黄擎宇,刘迪,叶宁,等.塔里木盆地寒武系白云岩储层特征及成岩作用[J].东北石油大学学报,2013,36(6):63-74.Huang Qingyu,Liu Di,Ye Ning,et al.Reservoir characteristics and diagenesis of Cambrain dolomite in Tarim basin[J].Journal of Northest Petroleum University,2013,36(6):63-74.
[20]张学丰,胡文瑄,张军涛,等.塔里木盆地下奥陶统白云岩化流体来源的地球化学分析[J].地学前缘,2008,15(2):80-89.Zhang Xuefeng,Hu Wenxuan,Zhang Juntao,et al.Geochemical analyses on dolomitizing fluids of lower Ordovician carbonate reservoir in Tarim basin[J].Earth Science Frontiers,2008,15(2):80-89.
[21]李倩文,金振奎,姜福杰.白云岩成因碳氧同位素分析方法初探——以北京燕山地区元古界白云岩为例[J].岩性油气藏,2014,26(4):118-121.Li Qianwen,Jin Zhenkui,Jiang Fujie.Carbon and oxygen isotope analysis method for dolomite formation mechanism:A case study from Proterozoic dolomite in Yanshan area[J].Lithologic Reservoirs,2014,26(4):118-121.
[22]郭福生,潘家永,刘林清,等.浙江江山石炭—二叠系碳酸盐岩碳氧同位素特征研究[J].地球化学,2004,33(1):l-8.Guo Fusheng,Pan Jiayong,Liu Linqing,et al.Carbon and oxygen characteristics of carbonate rocks of Carboniferous—Permian in Jiangshan,Zhejiang province[J].Geochimica,2004,33(1):l-8.
[23]彭苏萍,何宏,邵龙义,等.塔里木盆地碳酸盐岩碳同位素组成特征[J].中国矿业大学学报,2002,31(4):353-357.Peng Suping,He Hong,Shao Longyi,et al.Carbon isotopic compositions of the Cambrian—Ordovician carbonates in Tarim basin[J].Joumal of China University of Mining&Technology,2002,31(4):353-357.
[24]杜小弟,刘万洙,王东坡.碳氧同位素与海平面变化——以新疆柯坪地区上震旦统—奥陶系碳氧同位素剖面为例[J].世界地质,1994,13(3):120-123.Du Xiaodi,Liu Wanzhu,Wang Dongpo.Carbon,oxygen isotope and sea level changes:A case study ofδ13 C、δ18 O section of upper Sinian to Ordovician in Keping area,Xinjiang[J].Global geology,1994,13(3):120-123(in chinese).
[25]李辉,李国蓉,罗韵,等.塔河地区奥陶系碳酸盐岩储层深部热液特征分析[J].东北石油大学学报,2014,38(6):12-16.Li Hui,Li Guorong,Luo Yun,et al.Analysis of characteristics of deep hydrothermal fluids in Ordovician carbonate reservoir in Tahe area[J].Journal of Northest Petroleum University,2014,38(6):12-16.
[26]黄文明,刘树根,张长俊,等.四川盆地寒武系储层特征及优质储层形成机理[J].石油与天然气地质,2009,30(5):566-575.Huang Wenming,Liu Shugen,Zhang Changjun,et al.Reservoir characteristics and formation mechanism of the high quality Cambrain reservoirs in Sichuan basin[J].Oil&Gas Geology,2009,30(5):566-575.
[27]刘树根,黄文明,张长俊,等.四川盆地白云岩成因的研究现状及存在问题[J].岩性油气藏,2008,20(2):7-10.Liu Shugen,Huang Wenming,Zhang Changjun,et al.Research status of dolomite genesis and its problems in Sichuan basin[J].Ithologic Reservoirs,2008,20(2):7-10.
[28]盛贤才,郭战峰,刘新民.秦岭—大别造山带南侧兴山地区中上寒武统白云岩储层特征[J].石油实验地质,2009,31(2):172-176.Sheng Xiancai,Guo Zhanfeng,Liu Xinmin.Characteristics of middle-upper Cambrian dolomite reservior in the Xingshan area of the southern margin of Qinling and Dabie orogenic belt[J].Petroleum Geology Experiment,2009,31(2):172-176.
[29]陈永权,周新源,杨文静.塔里木盆地寒武系白云岩的主要成因类型及其储层评价[J].海相油气地质,2009,14(4):10-17.Chen Yongquan,Zhou Xinyuan,Yang Wenjing.Genesis of Cambrian dolostone and the reservoir evaluation in Tarim basin[J].Marine Origin Petroleum Geology,2009,14(4):10-17.
[30]Badiozamani K.The dorag dolomitization model:Application to the middle Ordovician of Wisconsin[J].J.Sediment Petrol,1973,43(4):965-984.
[31]Davies G R,Smith L B.Structurally controlled hydrothermal dolomite reservoir facies:Anoverriew[J].AAPG Bulletin,2006,90(11):1641-1690.
2019 版权所有©东北石油大学 | 地址:黑龙江省大庆市高新技术产业开发区学府街99号 | 邮政编码:163318
信息维护:学报 | 技术支持:现代教育技术中心
网站访问量: