塔中地区北坡中-下奥陶统早成岩岩溶作用及储层形成模式

doi:10.7623/syxb201610003

石油学报 ›› 2016, Vol. 37 ›› Issue (10): 1231-1246.DOI: 10.7623/syxb201610003

塔中地区北坡中-下奥陶统早成岩岩溶作用及储层形成模式

陈红汉¹, 吴悠², 朱红涛¹, 鲁子野¹, 曹自成³, 云露³

1. 中国地质大学资源学院石油地质系湖北武汉 430074;
2. 长江大学地球科学学院湖北武汉 432100;
3. 中国石油化工股份有限公司西北油田分公司新疆乌鲁木齐 830011

收稿日期:2016-02-24 修回日期:2016-06-30 出版日期:2016-10-25 发布日期:2016-11-09
通讯作者: 陈红汉,男,1962年9月生,1985年获武汉地质学院石油及天然气地质学专业学士学位,1995年获中国地质大学博士学位,现为中国地质大学(武汉)资源学院石油地质系教授、博士生导师,主要从事油气成藏过程研究和流体包裹体系统分析。Email:hhchen@cug.edu.cn
作者简介:陈红汉,男,1962年9月生,1985年获武汉地质学院石油及天然气地质学专业学士学位,1995年获中国地质大学博士学位,现为中国地质大学(武汉)资源学院石油地质系教授、博士生导师,主要从事油气成藏过程研究和流体包裹体系统分析。Email:hhchen@cug.edu.cn
基金资助:
国家重点基础研究发展计划（973）项目（2012CB214804）和国家重大科技专项（2008ZX05008-003-30）资助。

Eogenetic karstification and reservoir formation model of the Middle-Lower Ordovician in the northeast slope of Tazhong uplift,Tarim Basin

Chen Honghan¹, Wu You², Zhu Hongtao¹, Lu Ziye¹, Cao Zicheng³, Yun Lu³

1. Department of Petroleum Geology, Faculty of Earth Resources, China University of Geosciences, Hubei Wuhan 430074, China;
2. School of Geosciences, Yangtze University, Hubei Wuhan 432100, China;
3. Sinopec Northwest Oil Company, Xinjiang Urumqi 830011, China

Received:2016-02-24 Revised:2016-06-30 Online:2016-10-25 Published:2016-11-09

摘要/Abstract

摘要：

高频层序界面下发育的多种类型早成岩岩溶与埋藏阶段沿着断裂带发育的深成岩溶叠加作用，成为深层—超深层碳酸盐岩储层发育的关键要素。在梳理岩溶作用概念的基础上，通过对塔中地区北坡顺南地区深层—超深层中—下奥陶统岩心、薄片岩石学和阴极发光观察以及流体包裹体和稳定氧、碳同位素分析，结合3D地震均方根振幅和古地貌恢复，不仅从微观上识别出了高位体系域上部同生岩溶和层间岩溶作用类型，并从宏观上建立了这种早成岩岩溶储层“准层状”发育模式，认为受控于古地貌和断裂的早成岩岩溶型储层因后续碳酸盐胶结物充填严重，平均残留孔隙度仅约2.0%，但叠加深成岩溶改造了的储层的最高平均孔隙度可达约19%。因此，早成岩岩溶叠加深成岩溶型储层将成为研究区深层—超深层下古生界斜坡带勘探的重要目标。

关键词: 早成岩岩溶, 同生岩溶作用, 准同生岩溶作用, 层间岩溶作用, 中-下奥陶统, 塔里木盆地

Abstract:

Superimposition of multiple types of eogenetic karsts developing under high-frequency sequence boundary and hypogenic karsts developing along fault belts during burial diagenesis becomes a key factor of deep-ultradeep carbonate reservoir development. Based on an outline of karstification concept, deep-ultradeep Middle-Lower Ordovician strata in Shunnan area in the northern slope of Tazhong uplift, Tarim Basin were studied by means of core observation, thin-section petrological observation, cathodoluminescene imaging, fluid inclusion measurement, stable oxygen and carbon isotope analyses, as well as RMS amplitude computation for 3D seismic data and paleotopography restoration; not only syngenetic karst and interstratal karst types in the upper highstand system tract were microscopically identified, but also a "quasi-layered" development model for such eogenetic karst reservoir was established macroscopically. It is believed that, being seriously filled with subsequent carbonate cement, the eogenetic karst-type reservoir controlled by paleotopography and paleofault had a mean residual porosity of just about 2.0%, whereas the reservoir transformed by hypogenic karst superimposition had a maximum mean porosity up to about 19%. Therefore, reservoirs with eogenetic karsts superimposed by hypogenic karsts will become important targets of exploration in deep-ultradeep Lower Paleozoic ramp zone in the study area.

Key words: eogenetic karst, syngenetic karst, penesyngenetic karst, interstratal karst, the Middle-Lower Ordovician, Tarim Basin

中图分类号:

TE122

陈红汉, 吴悠, 朱红涛, 鲁子野, 曹自成, 云露. 塔中地区北坡中-下奥陶统早成岩岩溶作用及储层形成模式[J]. 石油学报, 2016, 37(10): 1231-1246.

Chen Honghan, Wu You, Zhu Hongtao, Lu Ziye, Cao Zicheng, Yun Lu. Eogenetic karstification and reservoir formation model of the Middle-Lower Ordovician in the northeast slope of Tazhong uplift,Tarim Basin[J]. Acta Petrolei Sinica, 2016, 37(10): 1231-1246.

参考文献

[1] 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——以四川普光气田为例[J].地质学报,2010,84(8):1087-1094.
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.
[2] 马永生,蔡勋育,赵培荣.深层、超深层碳酸盐岩油气储层形成机理研究综述[J].地学前缘,2011,18(4):181-192.
Ma Yongsheng,Cai Xunyu,Zhao Peirong.The research status and advances in porosity evolution and diagenesis of deep carbonate reservoir[J].Earth Science Frontiers,2011,18(4):181-192.
[3] 贾承造,庞雄奇.深层油气地质理论研究进展与主要发展方向[J].石油学报,2015,36(12):1457-1469.
Jia Chengzao,Pang Xiongqi.Research processes and main development directions of deep hydrocarbon geological theories[J].Acta Petrolei Sinica,2015,36(12):1457-1469.
[4] 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.
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.
[5] 淡永,梁彬,曹建文,等.碳酸盐岩早成岩岩溶作用及油气地质意义[J].中国岩溶,2015,34(2):126-135.
Dan Yong,Liang Bin,Cao Jianwen,et al.Eogenetic karstification in carbonatite and its significance for hydrocarbon geology[J].Carsologica Sinica,2015,34(2):126-135.
[6] Moore C H.Carbonate reservoirs:porosity,evolution and diagenesis in a sequence stratigraphic framework[M].Amsterdam:Elsevier,2001:443.
[7] 潘文庆,王招明,孙崇浩,等.塔里木盆地下古生界碳酸盐岩层序界面类型划分及其意义[J].石油与天然气地质,2011,32(4):531-541.
Pan Wenqing,Wang Zhaoming,Sun Chonghao,et al.Classifications of sequence boundaries in the Lower Paleozoic carbonates in Tarim Basin and their significances[J].Oil & Gas Geology,2011,32(4):531-541.
[8] 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.
Zhao Wenzhi,Shen Anjiang,Pan Wenqing,et al.A research on carbonate karst reservoirs classification and its implication on hydrocarbon exploration:cases studies from Tarim Basin[J].Acta Petrologica Sinica,2013,29(9):3213-3222.
[9] 何治亮,高志前,张军涛,等.层序界面类型及其对优质碳酸盐岩储层形成与分布的控制[J].石油与天然气地质,2014,35(6):853-859.
He Zhiliang,Gao Zhiqian,Zhang Juntao,et al.Types of sequence boundaries and their control over formation and distribution of quality carbonate reservoirs[J].Oil & Gas Geology,2014,35(6):853-859.
[10] Godet A.Drowning unconformities:palaeoenvironmental significance and involvement of global processes[J].Sedimentary Geology,2013,293:45-66.
[11] 李思田,焦养泉.碳酸盐台地边缘带沉积体系露头研究及储层建模[M].北京:地质出版社,2014.
Li Sitian,Jiao Yangquan.Outcrop depositional system research of the carbonate platform margin belts and reservoir modeling[M].Beijing:Geological Publishing House,2014.
[12] 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.
Shen Anjiang,Pan Wenqing,Zheng Xingping,et al.Types and characteristics of lower palaeozoic karst reservoirs in Tarim Basin[J].Marine Origin Petroleum Geology,2010,15(2):20-29.
[13] Loucks R G.Paleocave carbonate reservoirs; origins,burial-depth modifications,spatial complexity,and reservoir implications[J].AAPG Bulletin,1999,83(11):1795-1834.
[14] Klimchouk A B.Evolution of intrastratal karst and caves in gypsum[M]//Shroder J,Frumkin A.Treatise on Geomorphology.San Diego,CA:Academic Press,2013:438-450.
[15] Ford D C,Williams P W.Karst geomorphology and hydrology[M].Netherlands:Springer,1989.
[16] Andreychouk V,Dublyansky Y,Ezhov Y,et al.Karst in the earth's crust:its distribution and principal types[R].Sosnowiec-Symferopol,2009.
[17] 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.
[18] 贾疏源,冯先智.川南阳新灰岩中首次发现层间古岩溶[J].成都地质学院学报,1986,16(4):30.
Jia Shuyuan,Feng Xianzhi.First discovery of interstratal karst in Yangxin limestone of South Sichuan[J].Journal of Chengdu College of Geology,1986,16(4):30.
[19] 刘伟方,罗春树,高建虎,等.塔中82井区层间岩溶成因探讨[J].物探化探计算技术,2009,31(3):253-257.
Liu Weifang,Luo Chunshu,Gao Jianhu,et al.Research on interlayer karstification pattern in well TZ82 region[J].Computing Techniques for Geophysical and Geochemical Exploration,2009,31(3):253-257.
[20] 倪新锋,王招明,杨海军,等.塔北地区奥陶系碳酸盐岩储层岩溶作用[J].油气地质与采收率,2010,17(5):11-16.
Ni Xinfeng,Wang Zhaoming,Yang Haijun,et al.Formation mechanism of Ordovician carbonate karst reservoir in the Northern Tarim Basin[J].Petroleum Geology and Recovery Efficiency,2010,17(5):11-16.
[21] 袁圣强,贾承造,高日胜,等.塔中北斜坡中-下奥陶统碳酸盐岩沉积储层特征及地质模式[J].石油学报,2012,33(增刊1):80-88.
Yuan Shengqiang,Jia Chengzao,Gao Risheng,et al.Sedimentation characteristics and reservoir geological model of Mid-Lower Ordovician carbonate rock in Tazhong northern slope[J].Acta Petrolei Sinica,2012,33(Supplement 1):80-88.
[22] 吉云刚,韩剑发,张正红,等.塔里木盆地塔中北斜坡奥陶系鹰山组深部优质岩溶储层的形成与分布[J].地质学报,2012,86(7):1163-1174.
Ji Yungang,Han Jianfa,Zhang Zhenghong,et al.Formation and distribution of deep high quality reservoirs of Ordovician Yingshan Formation in the Northern slope of the Tazhong area in Tarim Basin[J].Acta Geologica Sinica,2012,86(7):1163-1174.
[23] 孙崇浩,于红枫,王怀盛,等.塔里木盆地塔中地区奥陶系鹰山组碳酸盐岩孔洞发育规律研究[J].天然气地球科学,2012,23(2):230-236.
Sun Chonghao,Yu Hongfeng,Wang Huaisheng,et al.Vugular formation of carbonates in Ordovician Yingshan reservoir in Tazhong northern slope of Tarim Basin[J].Natural Gas Geoscience,2012,23(2):230-236.
[24] 郑剑,林新,王振宇,等.塔中北斜坡地区奥陶系鹰山组储层差异性分析[J].岩性油气藏,2012,24(5):89-93.
Zheng Jian,Lin Xin,Wang Zhenyu,et al.Reservoir differences of the Ordovician Yingshan Formation in the northern slope of Tazhong[J].Lithologic Reservoirs,2012,24(5):89-93.
[25] 王宇,于红枫,苏劲,等.塔中北斜坡流体复杂区油气富集规律——以中古51井区奥陶系鹰山组为例[J].新疆石油地质,2012,33(6):664-667.
Wang Yu,Yu Hongfeng,Su Jin,et al.Hydrocarbon accumulation mechanism of fluid complicated zone in northern slope of Tazhong area,Tarim Basin-an example from the Ordovician Yingshan Formation in Zhonggu-51 wellblock[J].Xinjiang Petroleum Geology,2012,33(6):664-667.
[26] 胡昊,王振宇,张云峰.塔中北斜坡鹰山组碳酸盐岩层间岩溶储集层特征[J].新疆石油地质,2013,34(3):277-281.
Hu Hao,Wang Zhenyu,Zhang Yunfeng.Characteristics of carbonate interlayer karst reservoir of Yingshan Formation in Tazhong northern slope,Tarim Basin[J].Xinjiang Petroleum Geology,2013,34(3):277-281.
[27] Feng Renwei,Ouyang Cheng,Pang Yanjun,et al.Evolution modes of interbedded weathering crust karst:a case study of the 1st and 2nd members of Ordovician Yingshan Formation in EPCC block,Tazhong,Tarim Basin[J].Petroleum Exploration and Development,2014,41(1):49-59.
[28] Lace M J,Mylroie J E.Coastal karst landforms[M].Netherlands:Springer,2013.
[29] Vacher H L,Mylroie J E.Eogenetic karst from the perspective of an equivalent porous medium[J].Carbonates and Evaporites,2002,17(2):182-196.
[30] Frank E F,Mylroie J E,Troester J,et al.Karst development and speleogenesis,Isla de Mona,Puerto Rico[J].Journal of Cave and Karst Studies,1998,60(2):73-83.
[31] Baceta J I,Wright V P,Beavington-Penney S J,et al.Palaeohydrogeological control of palaeokarst macro-porosity genesis during a major sea-level lowstand:danian of the Urbasa-Andia plateau,Navarra,North Spain[J].Sedimentary Geology,2007,199(3/4):141-169.
[32] Choquette P W,James N P.Diagenesis #12.Diagenesis in limestones-3.The deep burial environment[J].Geoscience Canada,1987,14(1):3-35.
[33] Wright V P,Smart P L.Paleokarst (dissolution diagenesis):its occurrence and hydrocarbon exploration significance[M]//Wolf K H,Chilingarian G V.Diagenesis,IV.Developments in Sedimentology.Amsterdam:Elsevier,1994:477-517.
[34] 吴熙纯,李培华,金香福,等.鄂尔多斯南部奥陶系古岩溶带对天然气储层的控制[J].石油与天然气地质,1997,18(4):294-299.
Wu Xichun,Li Peihua,Jin Xiangfu,et al.Control of Ordovician paleokarst zones in South Ordos on gas reservoirs[J].Oil & Gas Geology,1997,18(4):294-299.
[35] 杨威,王清华,赵仁德,等.和田河气田碳酸盐岩储集层的岩溶作用[J].新疆石油地质,2002,23(2):124-126.
Yang Wei,Wang Qinghua,Zhao Rende,et al.Karstification of carbonate reservoir in Hetian River gas field of Tarim Basin[J].Xinjiang Petroleum Geology,2002,23(2):124-126.
[36] Zhao Wenzhi,Shen Anjiang,Zhou Jingao,et al.Types,characteristics,origin and exploration significance of reef-shoal reservoirs:a case study of Tarim Basin,NW China and Sichuan Basin,SW China[J].Petroleum Exploration and Development,2014,41(3):283-293.
[37] 赵宗举,潘文庆,张丽娟,等.塔里木盆地奥陶系层序地层格架[J].大地构造与成矿学,2009,33(1):175-188.
Zhao Zongju,Pan Wenqing,Zhang Lijuan,et al.Sequence stratigraphy in the Ordovician in the Tarim Basin[J].Geotectonica et Metallogenia,2009,33(1):175-188.
[38] Carlson E H.Reactivated interstratal karst-example from the Late Silurian rocks of western Lake Erie (U.S.A.)[J].Sedimentary Geology,1992,76(3/4):273-283.
[39] Genç Y.Genesis of the Neogene interstratal karst-type P hrenk fluorite-barite (±lead) deposit (K1r?ehir,Central Anatolia,Turkey)[J].Ore Geology Reviews,2006,29(2):105-117.
[40] Immenhauser A,Rameil N.Interpretation of ancient epikarst features in carbonate successions-a note of caution[J].Sedimentary Geology,2011,239(1/2):1-9.
[41] Gutiérrez F,Carbonel D,Guerrero J,et al.Late Holocene episodic displacement on fault scarps related to interstratal dissolution of evaporites (Teruel Neogene Graben,NE Spain)[J].Journal of Structural Geology,2012,34:2-19.
[42] Guerrero J,Gutiérrez F,Galve J P.Large depressions,thickened terraces,and gravitational deformation in the Ebro River valley (Zaragoza area,NE Spain):evidence of glauberite and halite interstratal karstification[J].Geomorphology,2013,196:162-176.
[43] Sanz E,Ayora C,Carrera J.Calcite dissolution by mixing waters:geochemical modeling and flow-through experiments[J].Geologica Acta,2011,9(1):67-77.
[44] 黄太柱.塔里木盆地塔中北坡构造解析与油气勘探方向[J].石油实验地质,2014,36(3):257-267.
Huang Taizhu.Structural interpretation and petroleum exploration targets in northern slope of middle Tarim Basin[J].Petroleum Geology & Experiment,2014,36(3):257-267.
[45] 杨圣彬,刘军,李慧莉,等.塔中北围斜区北东向走滑断裂特征及其控油作用[J].石油与天然气地质,2013,34(6):797-802.
Yang Shengbin,Liu Jun,Li Huili,et al.Characteristics of the NE-trending strike-slip fault system and its control on oil accumulation in north peri-cline area of the Tazhong paleouplift[J].Oil & Gas Geology,2013,34(6):797-802.
[46] 吴斌,何登发,孙方源.塔里木盆地古城低凸起下古生界的断裂特征及成因机制[J].天然气地球科学,2015,26(5):871-879.
Wu Bin,He Dengfa,Sun Fangyuan.Fault characteristic and genetic mechanism of the Lower Paleozoic in Gucheng Lower Uplift,Tarim Basin[J].Natural Gas Geoscience,2015,26(5):871-879.
[47] 朱长见,肖中尧,张宝民,等.塔里木盆地古城4井区上寒武统-奥陶系储集层特征[J].石油勘探与开发,2008,35(2):175-181.
Zhu Changjian,Xiao Zhongyao,Zhang Baomin,et al.Upper Cambrian-Ordovician reservoir characteristics in Well Gucheng-4 area,Tarim Basin[J].Petroleum Exploration and Development,2008,35(2):175-181.
[48] 林畅松,杨海军,蔡振中,等.塔里木盆地奥陶纪碳酸盐岩台地的层序结构演化及其对盆地过程的响应[J].沉积学报,2013,31(5):907-919.
Lin Changsong,Yang Haijun,Cai Zhenzhong,et al.Evolution of depositional architecture of the Ordovician carbonate platform in the Tarim Basin and its response to basin processes[J].Acta Sedimentologica Sinica,2013,31(5):907-919.
[49] 赵宗举.全球海平面变化指标及海相构造层序研究方法——以塔里木盆地奥陶系为例[J].石油学报,2015,36(3):262-273.
Zhao Zongju.Indicators of global sea-level change and research methods of marine tectonic sequences:take Ordovician of Tarim Basin as an example[J].Acta Petrolei Sinica,2015,36(3):262-273.
[50] 邓胜徽,黄智斌,景秀春,等.塔里木盆地西部奥陶系内部不整合[J].地质论评,2008,54(6):741-747.
Deng Shenghui,Huang Zhibin,Jing Xiuchun,et al.Unconformities in the Ordovician of western Tarim Basin,NW China[J].Geological Review,2008,54(6):741-747.
[51] 蔡习尧,李越.新疆塔中南坡奥陶系的地层缺失和沉积相变化[J].地层学杂志,2008,32(4):353-362.
Cai Xiyao,Li Yue.Ordovician lithofacies and stratigraphic lacunae in the southern part of the Central Tarim,Xinjiang[J].Journal of Stratigraphy,2008,32(4):353-362.
[52] 何碧竹,焦存礼,许志琴,等.不整合结构构造与构造古地理环境——以加里东中期青藏高原北缘及塔里木盆地为例[J].岩石学报,2013,29(6):2184-2198.
He Bizhu,Jiao Cunli,Xu Zhiqin,et al.Unconformity structural architecture and tectonic paleo-geographic environment:a case of the Middle Caledonian on the northern margin of Tibet Plateau and Tarim Basin[J].Acta Petrologica Sinica,2013,29(6):2184-2198.
[53] 欧阳永林,曾庆才,郭晓龙,等.塔中地区鹰山组储层分布规律与地震预测[J].天然气地球科学,2015,26(5):893-903.
Ouyang Yonglin,Zeng Qingcai,Guo Xiaolong,et al.Reservoirs distribution and seismic prediction of the lower Ordovician Yingshan Formation at the Tazhong area[J].Natural Gas Geoscience,2015,26(5):893-903.
[54] 陈红汉,鲁子野,曹自成,等.塔里木盆地塔中地区北坡奥陶系热液蚀变作用[J].石油学报,2016,37(1):43-63.
Chen Honghan,Lu Ziye,Cao Zicheng,et al.Hydrothermal alteration of Ordovician reservoir in northeastern slope of Tazhong uplift,Tarim Basin[J].Acta Petrolei Sinica,2016,37(1):43-63.

塔中地区北坡中-下奥陶统早成岩岩溶作用及储层形成模式

Eogenetic karstification and reservoir formation model of the Middle-Lower Ordovician in the northeast slope of Tazhong uplift,Tarim Basin

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