Evaluation and prediction of carbonate karst reservoirs in the Ordovician buried hills beneath the Tarim basin: An example east of the Lungu7 well block
-
摘要: 塔里木盆地奥陶系古潜山碳酸盐岩岩溶储层具有埋藏深、非均质性强的特点。岩溶储集空间主要为后期溶蚀孔、溶洞和溶缝为主。通过古地貌恢复及岩溶垂向分带研究,结合油藏开采动态,对轮古7井区以东地区奥陶系碳酸盐岩岩溶储层评价与预测。研究认为:高产高效井主要位于岩溶缓坡地的峰丘洼地、丘峰洼地及岩溶峰丛谷地的溶丘、溶峰及其边坡部位。垂向上表层岩溶带和垂向渗滤带的上部,开发效果较好,多发育裂缝-孔洞型、洞穴型储层;径流溶蚀带、潜流溶蚀带岩溶发育相对较弱,局部发育小规模溶洞或岩溶管道,岩溶储层以裂缝型或孔洞型为主。在此基础上预测出五个高产高效油气储层岩溶区,为油气勘探与开发提供依据。Abstract: The Ordovician carbonate karst reservoirs are characterized by deep burial and strong heterogeneity in Tarim basin. The karst reservoir space is primarily the later dissolution pores, karst caves and solution fissures. The study on paleogeomorphology restoration and karst vertical zonation, combined with the reservoir production performance permits to evaluate and predict the Ordovician carbonate karst reservoirs east of the Lungu7 well block. The research suggests that high-production and high-efficiency wells are mainly located in karst graves, karst crests, and karst slopes of peak-hill depressions, hill-peak depressions and karst peak cluster valleys. In the vertical direction, surface karst belts and the upper part of vertical infiltration belts are localities with good exploitation effects, where developed crack-hole reservoirs and karst cave reservoirs. In the runoff karst belts and undercurrent karst belts developed weak karst, where small-scale karst caves and karst pipelines are present, and the karst reservoirs are of the fractured- or hole-type. At last, the research predicts five high-efficient oil and gas reservoir areas, which provide the evidence for planning exploration and development of oil and gas in this area.
-
Key words:
- reservoir evaluation /
- reservoir prediction /
- carbonate /
- buried hill
-
[1] 刘伟.洞穴型碳酸盐岩储层识别及预测技术[J].中外能源,2010,15(3):4952. [2] 白果平,世界碳酸盐岩大油气田分布特征[J].古地理学报,2006,8(2):241-250. [3] 吕修祥,金之钧.碳酸盐岩油气田分布规律[J].石油学报,2000,21(3):8-12. [4] 张庆玉,梁彬,曹建文,等. 塔里木盆地轮古西地区奥陶系古潜山岩溶作用机理与发育模式[J].石油实验地质,2015,37(1):1-7. [5] Aguilera R F, Aguilera R. A triple porosity model for petrophysical analysis of naturally fractured reservoirs. Petrophysics[J], 2004,45(2):157-166. [6] 邓兴梁,张庆玉,梁彬,等.塔中Ⅱ区奥陶系鹰山组岩溶古地貌恢复方法研究[J].中国岩溶,2015,34(2):154-158. [7] 赵文智,沈安江,潘文庆,等.碳酸盐岩岩溶储层类型研究及对勘探的指导意义:以塔里木盆地岩溶储层为例[J].岩石学报,2013,29(9):3213-3222. [8] 李振宏,王欣,杨遂正,等.鄂尔多斯盆地奥陶系岩溶储层控制因素分析[J].现代地质,2006,20(2):299-306. [9] 金振奎,邹元荣,蒋春雷,等.大港探区奥陶系岩溶储层发育分布控制因素[J].沉积学报,2001,19(4):530-535. [10] 张达景,吕海涛,张涛,等.塔河油田加里东期岩溶储层特征及分布预测[J].沉积学报,2007,25(2):214-223. [11] 张学丰,李明,陈志勇,等.塔北哈拉哈塘奥陶系碳酸盐岩岩溶储层发育特征及主要岩溶期次[J].岩石学报, 2012,28(3):815-826. [12] 李世银,罗春树,邓兴梁,等.轮古西奥陶系潜山洞穴型岩溶储层发育特征与充填规律[J].海相油气地质,2012,17(2):70-74. [13] 淡永,梁彬,张庆玉,等.塔北哈拉哈塘地区奥陶系碳酸盐岩浅覆盖区岩溶储层特征与形成机理[J].石油物探,2015,54(1):90-98. [14] 刘伟,罗平,顾家裕,等.塔里木盆地西克尔地区古岩溶储层露头表征[J].地质学报,2010,84(8):1215-1222. [15] 吴欣松,魏建新,昌建波,等.碳酸盐岩古岩溶储层预测的难点与对策[J].中国石油大学学报(自然科学版),2009,33(6):16-21. [16] Shu Yong, Yan Jienian. Characterization and prevention of formation damage for fractured carbonate reservoir formations with low permeability. Petroleum Science, 2008,5(4):326-333. [17] Choquette P W, Pray L C. Geologic nomenclature and classification of porosity in sedimentary carbonates. AAPG Bull, 1970,54:207-250. [18] 韩革华,漆立新,李宗杰,等.塔河油田奥陶系碳酸盐岩缝洞型储层预测技术[J].石油与天然气地质,2006, 27(6):860-870,878. [19] 王伟力,刘洛夫,陈利新,等.塔里木盆地轮古东地区奥陶系碳酸盐岩储集层发育控制因素及有利区带预测[J].古地理学报,2010,12(1):107-115. [20] Chen Guangpo, Pan Wenqing, Sa Liming, et al. Application of Prediction Techniques in Carbonate Karst Reservoir in Tarim Basin[J]. Applied geophysics, 2005,2(2):111-118,132. [21] 刘洛夫,李燕,王萍,等.塔里木盆地塔中地区Ⅰ号断裂带上奥陶统良里塔格组储集层类型及有利区带预测[J].古地理学报,2008, 10(3):221-230. [22] 蒋忠诚,袁道先.表层岩溶带的岩溶动力学特征及其环境和资源意义[J].地球学报,1999, 20(3):302-308. [23] 曹建文,梁彬. 轮古7井以东地区前石炭纪古地貌恢复及识别[J].安徽农业科学,2010,38(27):15273-15276. [24] 张庆玉,梁彬,曹建文,等. 塔里木盆地轮古7井区以东奥陶系古岩溶储层碳氧同位素地球化学特征研究[J].地质科技情报,2015,34(2):52-56. [25] 张庆玉,梁彬,曹建文,等.塔中北斜坡奥陶系鹰山组岩溶储层特征及古岩溶发育模式[J].中国岩溶. 2016,35(1):106-113. [26] Loucks R G. Paleocave carbonite reservoirs origins, burial-depth mod-ification, spatial complexity, and reservoir in plications AAPG Bulle-tin,1999,83(11):1795-1834.
点击查看大图
计量
- 文章访问数: 2005
- HTML浏览量: 404
- PDF下载量: 793
- 被引次数: 0