Formation mechanism for the high-quality reservoir in the Chang 82 Interval of Yanchang Formation in Longdong area, Ordos Basin
Xu Liming1, 2, 3, Li Zhicheng1, Liang Xiaowei2, 3, Ji Youliang1, Niu Xiaobing2, 3, Ye Bo2, 3, Hao Bingying2, 3, Ma Jiye2, 3, You Yuan2, 3
1 State Key Laboratory of Petroleum Resource and Prospecting,College of Geosciences,China University of Petroleum(Beijing),Beijing 102249; 2 National Engineering Laboratory for Exploration and Development of Low-permeability Oil & Gas Field,Xian 710018,Shaanxi; 3 Research Institute of Exploration and Development,Changqing Oilfield Company,PetroChina, Xi#x0ddb3;an 710018,Shaanxi;
Abstract:The reservoirs of the Chang 82 interval of Yanchang Formation in Longdong area of Ordos Basin have low porosity(average 8.8%)and low permeability(average 0.64×10-3 μm2). The strong compaction is the main reason for the poor reservoir properties,and the carbonate cementation further reduces the reservoir physical properties. Although the reservoir physical property is generally poor,the high quality reservoirs have relatively high porosity and permeability are developed on the background of tight reservoirs. The high-quality reservoirs are analyzed and their typical characteristics are summarized. The statistical results show that the high-quality reservoirs have lower plastic component content,pore types are dominated by dissolution pores and residual intergranular pores cemented with chlorite, and pore structures are mainly small-medium pores with fine-medium throats. Based on the above understanding,the formation mechanism of the high quality reservoirs is analyzed. The study suggests that:High energy and thick sandbodies of distributary channel,mouth bar,etc., are conducive to form high-quality reservoirs;relatively low plastic component content and chlorite rim are in favor of preservation of intergranular pores; and dissolution is the most important diagenesis for the formation of secondary pores.
Xu Liming,Li Zhicheng,Liang Xiaowei et al. Formation mechanism for the high-quality reservoir in the Chang 82 Interval of Yanchang Formation in Longdong area, Ordos Basin[J]. JOPC, 2016, 18(2): 237-250.
楚美娟,郭正权,齐亚林,程党性. 2013. 鄂尔多斯盆地延长组长8储集层定量化成岩作用及成岩相分析. 天然气地球科学,24(3):477-484.[Chu M J,Guo Z Q,Qi Y L,Cheng D X. 2013. Quantitative diagenesis and diagenetic facies analysis on Chang 8 reservoir of Yanchang Formation in Ordos Basin. Natural Gas Geoscience,24(3):477-484] 邓秀芹,付金华,姚泾利,庞锦莲,孙勃. 2011. 鄂尔多斯盆地中及上三叠统延长组沉积相与油气勘探的突破. 古地理学报,13(4):443-455.[Deng X Q,Fu J H,Yao J L,Pang J L,Sun B. 2011. Sedimentary facies of the Middle-Upper Triassic Yanchang Formation in Ordos Basin and breakthrough in petroleum exploration. Journal of Palaeogeography(Chinese Edition),13(4):443-455] 丁晓琪,张哨楠,葛鹏莉,万友利. 2010. 鄂南延长组绿泥石环边与储集性能关系研究. 高校地质学报,16(2):247-254.[Ding X Q,Zhang S N,Ge P L,Wan Y L. 2010. Relationship between reservoir properties and chlorite rims:A case study from yanchang formation of South Ordos Basin,North China. Geological Journal of China Universities,16(2):247-254] 窦伟坦,田景春,徐小蓉,朱平,夏青松,倪新锋,张翔,聂永生,杨华,付金华,郭正权,邓秀芹. 2005. 陇东地区延长组长6-长8油层组成岩相研究. 成都理工大学学报(自然科学版),32(2):129-132.[Dou W T,Tian J C,Xu X R,Zhu P,Xia Q S,Ni X F,Zhang X,Nie Y S,Yang H,Fu J H,Guo Z Q,Deng X Q. 2005. Diagenetic facies study on Chang 6-8 oil formations of Triassic Yanchang Formation in Ordos Basin,China. Journal of Chengdu University of Technology(Science and Technology Edition),32(2):129-132] 付晶,吴胜和,李桢,刘科如. 2013. 陇东地区延长组层序格架内储集层质量差异及其控制因素. 中南大学学报(自然科学版),20(8):3293-3301.[Fu J,Wu S H,Li Z,Liu K R. 2013. Differences and controlling factors of reservoir quality within sequence stratigraphic framework of Yanchang Formation in Longdong Area,Ordos Basin. Journal of Central South University(Science and Technology),20(8):3293-3301] 黄思静,谢连文,张萌,武文慧,沈立成,刘洁. 2004. 中国三叠系陆相砂岩中自生绿泥石的形成机制及其与储集层孔隙保存的关系. 成都理工大学学报(自然科学版),31(3):273-281.[Huang S J,Xie L W,Zhang M,Wu W H,Shen L C,Liu J. 2004. Formation mechanism of authigenic chlorite and relation to preservation of porosity in nonmarine Triassic reservoir sandstones,Ordos Basin and Sichuan Basin,China. Journal of Chengdu University of Technology(Science and Technology Edition),31(3):273-281] 李红,柳益群,刘林玉. 2006. 鄂尔多斯盆地西峰油田延长组长81低渗透储集层成岩作用. 石油与天然气地质,27(2):209-217.[Li H,Liu Y Q,Liu L Y. 2006. Diagenesis of Chang 81 reservoir with low permeability in Xifeng oilfield, Ordos Basin. Oil & Gas Geology,27(2):209-217] 李弘,王芙蓉,戴世立,樊浩. 2008. 绿泥石膜对储集层孔隙度的影响:以鄂尔多斯盆地M油田延长组2段为例. 岩性油气藏,20(4):71-74.[Li H,Wang F R,Dai S L,Fan H. 2008. Influence of chlorite film on reservoir porosity:A case study from the second member of Yanchang Formation in Ordos Basin. Lithologic Reservoirs,20(4):71-74] 李文厚,庞军刚,曹红霞,肖丽,王若谷. 2009. 鄂尔多斯盆地晚三叠世延长期沉积体系及岩相古地理演化. 西北大学学报(自然科学版),39(3):501-506.[Li W H,Pang J G,Cao H X,Xiao L,Wang R G. 2009. Depositional system and paleogeographic evolution of the late Triassic Yanchang Stage in Ordos Basin. Journal of Northwest University(Natural Science Edition),39(3):501-506] 林煜,吴胜和,徐樟有,倪玉强. 2012. 川西丰谷构造须家河组四段钙屑砂岩优质储集层控制因素. 天然气地球科学,23(4):691-699.[Lin Y,Wu S H,Xu Z Y,Ni Y Q. 2012. Controlling factors for T3x4 calcarenaceous sandstone in Fenggu structure western Sichuan basin. Natural Gas Geoscience,23(4):691-699] 刘金库,彭军,刘建军,汪彦,刘建锋. 2009. 绿泥石环边胶结物对致密砂岩孔隙的保存机制:以川中—川南过渡带包界地区须家河组储集层为例. 石油与天然气地质,30(1):53-58.[Liu J K,Peng J,Liu J J,Wang Y,Liu J F. 2009. Pore-preserving mechanism of chlorite rims in tight sandstone—an example from the T3x, Formation of Baojie area in the transitional zone from the central to southern Sichuan Basin. Oil & Gas Geology,30(1):53-58] 罗静兰,李忠兴,史成恩,李建,韩永林,王海宏,李进步,王成玉. 2008. 鄂尔多斯盆地西南部上三叠统延长组长8、长6油层组的沉积体系与物源方向. 地质通报,27(1):101-111.[Luo J L,Li Z X,Shi C E,Li J,Han Y L,Wang H H,Li J B,Wang C Y. 2008. Depositional systems and provenance directions for the Chang 6 and Chang 8 reservoir groups of the Upper Triassic Yanchang Formation in the southwestern Ordos basin,China. Geological Bulletin of China,27(1):101-111] 王金鹏,彭仕宓,史基安,王琪,郭雪莲. 2008. 鄂尔多斯盆地陇东地区长6—长8段储集层特征及其主控因素. 新疆地质,26(2):163-166.[Wang J P,Peng S B,Shi J A,Wang Q,Guo X L. 2008. Reservoir characteristics and its main controlling factors of Chang 6-Chang 8 Formation in Longdong,Ordos Basin. Xinjiang Geology,26(2):163-166] 王岚,李文厚,林潼,王若谷. 2012. 鄂尔多斯盆地上三叠统延长组长6油层组储集层成岩作用及其影响因素. 古地理学报,14(3):311-320.[Wang L,Li W H,Lin T,Wang R G. 2012. Diagenesis and its influencing factors of the Chang 6 interval of Upper Triassic Yanchang Formation in Ordos Basin. Journal of Palaeogeography(Chinese Edition),14(3):311-320] 王新民,郭彦如,付金华,刘化清,陈启林,李天顺,廖建波,张春雷. 2005. 鄂尔多斯盆地延长组长8段相对高孔渗砂岩储集层的控制因素分析. 石油勘探与开发,32(2):35-38.[Wang X M,Guo Y R,Fu J H,Liu H Q,Chen Q L,Li T S,Liao J B,Zhang C L. 2005. Control factors for forming higher porosity and permeability sandstone reservoirs in Chang 8member of Yanchang Formation,Ordos Basin. Petroleum Exploration and Development,32(2):35-38] 武富礼,李文厚,李玉宏,席胜利. 2004. 鄂尔多斯盆地上三叠统延长组三角洲沉积及演化. 古地理学报,6(3):307-315.[Wu F L,Li W H,Li Y H,Xi S L. 2004. Delta sediments and evolution of the Yanchang Formation of Upper Triassic in Ordos Basin. Journal of Palaeogeography(Chinese Edition),6(3):307-315] 谢武仁,杨威,赵杏媛,魏国齐,谢增业,金惠,陈刚. 2010. 川中地区须家河组绿泥石对储集层物性的影响. 石油勘探与开发,37(6):674-679.[Xie W R,Yang W,Zhao X Y,Wei G Q,Xie Z Y,Jin H,Chen G. 2010. Influences of chlorite on reservoir physical properties of the Xujiahe Formation in the central part of Sichuan Basin. Pertroleum Exploration and Development,37(6):674-679] 杨巍,陈国俊,张铭杰,李程善,吕成福,李超. 2012. 鄂尔多斯盆地镇北地区长8油层组自生绿泥石对储集层物性的影响. 岩性油气藏,24(3):27-32.[Yang W,Chen G J, Zhang M J,Li C S,Lü C F,Li C. 2012. Influence of authigenic chlorite on reservoir properties of Chang 8 oil reservoir set in Zhenbei Area,Ordos Basin. Lithologic Reservoirs,24(3):27-32] 姚泾利,王琪,张瑞,李树同. 2011. 鄂尔多斯盆地华庆地区延长组长6砂岩绿泥石膜的形成机理及其环境指示意义. 沉积学报,29(1):72-79.[Yao J L,Wang Q,Zhang R,Li S T. 2011 Forming mechanism and their environmental implications of chlorite-coatings in Chang 6 sandstone(Upper Triassic)of Hua-Qing Area,Ordos Basin. Acta Sedimentologica Simica,29(1):72-79] 姚泾利,楚美娟,白嫦娥,袁晓明,郭正权. 2014. 鄂尔多斯盆地延长组长82小层厚层砂体沉积特征及成因分析. 岩性油气藏,26(6):40-45.[Yao J L,Chu M J,Bai C E,Yuan X M,Guo Z Q. 2014. Sedimentary characteristics and genesis of thick layer sand body of Chang 82 sublayer in Ordos Basin. Lithologic Reservoirs,26(6):40-45] 张晓莉,谢正温. 2006. 鄂尔多斯盆地陇东地区三叠系延长组长8储集层特征. 矿物岩石,26(4):83-88.[Zhang X L,Xie Z W. 2006. Reservoir Characteristics of Chang 8 of Yan Chang formation(Triassic)in Longdong Area,Ordos Basin. Mineral Petrology,26(4):83-88] 钟大康,周立建,孙海涛,姚泾利,刘显阳,罗安湘,邓秀芹. 2013. 鄂尔多斯盆地陇东地区延长组砂岩储集层岩石学特征. 地学前缘,20(2):52-60.[Zhong D K,Zhou L J,Sun H T,Yao J L,Liu X Y,Luo A X,Deng X Q. 2013. Petrology of sandstone reservoirs in Longdong Area,Ordos Basin. Earth Science Frontiers,20(2):52-60]
Berger A,Gier S,Krois P. 2009. Porosity-preserving chlorite cements in shallow-marine volcaniclastic sandstones:Evidence from Cretaceous sandstones of the Sawan gas field,Pakistan. AAPG Bulletin,93:595-615. Bloch S,Lander K,Bonnel L. 2002. Anomalously high porosity and permeability in deeply buried sandstone reservoirs:Origin and Predictability. AAPG Bulletin,86:301-328. Ehrenberg S N. 1993. Preservation of anomalously high porosity in deeply buried sandstones by grain-coating chlorite;Examples from the Norwegian Continental Shelf. AAPG Bulletin,77(7):1260-1286. Feng Z Z,Bao H P,Jia J H,Wang Y G,Deng X Q. 2013. Lithofacies palaeogeography as a guide to petroleum exploration. Journal of Palaeogeography,2(2):109-126.庞凌云