柯坪—巴楚露头区蓬莱坝组白云岩特征及孔隙成因

doi:10.7623/syxb201404006

石油学报 ›› 2014, Vol. 35 ›› Issue (4): 664-672.DOI: 10.7623/syxb201404006

柯坪—巴楚露头区蓬莱坝组白云岩特征及孔隙成因

郑剑锋^1,2, 沈安江^1,2, 乔占峰^1,2, 吴兴宁², 张天付^1,2

1. 中国石油天然气集团公司碳酸盐岩储层重点实验室浙江杭州 310023;
2. 中国石油天然气股份有限公司杭州地质研究院浙江杭州 310023

收稿日期:2014-01-04 修回日期:2014-04-25 出版日期:2014-07-25 发布日期:2014-08-05
通讯作者: 郑剑锋，男，1977年7月生，2001年获江汉石油学院学士学位，2004年获长江大学硕士学位，现为中国石油天然气股份有限公司杭州地质研究院高级工程师，主要从事碳酸盐岩沉积、储层研究。Email：zhengjf_hz@petrochina.com.cn
作者简介:郑剑锋，男，1977年7月生，2001年获江汉石油学院学士学位，2004年获长江大学硕士学位，现为中国石油天然气股份有限公司杭州地质研究院高级工程师，主要从事碳酸盐岩沉积、储层研究。Email：zhengjf_hz@petrochina.com.cn
基金资助:
国家重大科技专项（2011ZX05004-002）资助。

Characteristics and pore genesis of dolomite in the Penglaiba Formation in Keping-Bachu outcrop area

Zheng Jianfeng^1,2, Shen Anjiang^1,2, Qiao Zhanfeng^1,2, Wu Xingning², Zhang Tianfu^1,2

1. CNPC Key Laboratory of Carbonate Reservoir, Zhejiang Hangzhou 310023, China;
2. PetroChina Hangzhou Research Institute of Geology, Zhejiang Hangzhou 310023, China

Received:2014-01-04 Revised:2014-04-25 Online:2014-07-25 Published:2014-08-05

摘要/Abstract

摘要：

塔里木盆地下奥陶统蓬莱坝组白云岩是重要的潜在勘探领域，但因其勘探、研究程度低，导致目前的认识无法满足油气勘探需求，而其孔隙成因及发育规律是非常重要的制约因素之一。通过对柯坪水泥厂剖面及巴楚达坂塔格剖面的精细岩石特征描述，发现研究区蓬莱坝组白云岩孔隙主要发育于细—粗晶白云岩中，孔隙类型以晶间孔、晶间溶孔为主，且相对均质，一般孔隙度3%~5%。微量元素、稀土元素及氧、碳、锶同位素特征反映白云石化作用主要发生于早—中埋藏期，局部受到晚埋藏期热液的改造，白云石化流体主要为海源地层水。在对重点白云岩层段进行精细岩相、高频层序地层分析及利用显微、荧光技术恢复白云岩原岩结构的基础上，认为蓬莱坝组白云岩孔隙的发育具有成层性和旋回性，台内高能滩是孔隙发育的优势相带，六级或五级高频旋回向上变浅序列的上部为有利孔隙发育位置。白云石化作用并不直接产生孔隙，而是使原岩孔隙得到继承，并起保护孔隙的作用。

关键词: 柯坪—巴楚地区, 蓬莱坝组, 露头, 白云岩, 孔隙成因, 下奥陶统

Abstract:

Dolomite of Penglaiba Formation in Tarim Basin provides a potentially important exploration field. With low degree of relevant exploration and research, the current understandings cannot meet the needs for dolomite exploration in Penglaiba Formation, and study on the genesis and distribution of dolomite is one of the important limiting factors. This study detailed the characteristics of dolomite in Keping and Dabantage sections, indicating that pores mainly exist in fine-coarse crystalline dolomite, including the major types of intercrystalline pore and intercrystalline solution pore (average porosity, approx. 3% ~5%). Trace elements, rear earth elements, and oxygen, carbon, and strontium isotope elements were analyzed, and the results reflected that dolomitization mainly took place in the early-middle buried stage and was partially modified by hydrothermal fluid in the later buried stage, with formation water of sea source as the main dolomitization fluid. Additionally, the lithofacies and high frequency sequence stratigraphy of selected dolomite intervals were analyzed and the original dolomite rock structure was reconstructed by microscopy and fluorescence technique. It was found that the development of dolomite pores featured stratification and cyclicity, for which high energy platform shoal was the favorable facies and the top of sixth- or fifth-order cycle was the favorable place. Dolomitization did not product pores directly but mainly inherited and protected the pores from the original rocks.

Key words: Keping-Bachu area, Penglaiba Formation, outcrop area, dolomite, pore genesis, Lower Ordovician

中图分类号:

TE112.23

郑剑锋, 沈安江, 乔占峰, 吴兴宁, 张天付. 柯坪—巴楚露头区蓬莱坝组白云岩特征及孔隙成因[J]. 石油学报, 2014, 35(4): 664-672.

Zheng Jianfeng, Shen Anjiang, Qiao Zhanfeng, Wu Xingning, Zhang Tianfu. Characteristics and pore genesis of dolomite in the Penglaiba Formation in Keping-Bachu outcrop area[J]. ACTA PETROLEI SINICA, 2014, 35(4): 664-672.

参考文献

[1] Zenger D H,Dunham J B,Ethington R L.Concepts and models of dolomitization[M].SEPM Special Publication, 1980,28:1-320.
[2] Sun S Q.A reappraisal of dolomite abundance and occurrence in the Phanerozoic[J].Journal of Sedimentary Research Section,1996,64(2):396-404.
[3] 马锋,杨柳明,顾家裕,等.世界白云岩油气田勘探综述[J].沉积学报,2011,29(5):1010-1021.
Ma Feng,Yang Liuming,Gu Jiayu,et al.The summary on exploration of the dolomite oilfields in the world[J].Acta Sedimentologica Sinica,2011,29(5):1010-1021.
[4] 顾家裕.塔里木盆地下奥陶统白云岩特征及成因[J].新疆石油地质,2000,21(2):120-122.
Gu Jiayu.Characteristics and origin analysis of dolomite in Lower Ordovician of Tarim Basin[J].Xinjiang Petroleum Geology,2000,21(2):120-122.
[5] 杨威,王清华,刘效曾.塔里木盆地和田河气田下奥陶统白云岩成因[J].沉积学报,2000,18(4):544-548.
Yang Wei,Wang Qinghua,Liu Xiaozeng.Dolomite origin of Lower Ordovician in Hetian River Gas Field,Tarim Basin[J].Acta Sedimentologica Sinica,2000,18(4):544-548.
[6] 郑剑锋,沈安江,刘永福,等.多参数综合识别塔里木盆地下古生界白云岩成因[J].石油学报,2012,32(增刊2):145-153.
Zheng Jianfeng,Shen Anjiang,Liu Yongfu,et al.Multi-parameter comprehensive identification of the genesis of Lower Paleozoic dolomite in Tarim Basin,China [J].Acta Petrolei Sinica,2012,32(Supplement 2):145-153.
[7] 张德民,鲍志东,潘文庆,等.塔里木盆地下古生界白云岩类型及成因[J].古地理学报,2013,15(5):693-706.
Zhang Demin,Bao Zhidong,Pan Wenqing,et al.Type and origin of the Lower Paleozoic dolostones in Tarim Basin[J].Journal of Palaeogeography,2013,15(5):693-706.
[8] 郑和荣,吴茂炳,邬兴威,等.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,2007,28(2):1-8.
Zheng Herong,Wu Maobing,Wu Xingwei,et al.Oil-gas exploration prospect of dolomite reservoir in the Lower Paleozoic of Tarim Basin[J].Acta Petrolei Sinica,2007,28(2):1-8.
[9] 张新华,黄文辉,王安甲,等.塔里木盆地下古生界白云岩储层发育控制因素分析[J].西北大学学报:自然科学版,2009,39(2):288-292.
Zhang Xinhua,Huang Wenhui,Wang Anjia,et al.Analysis of the reservoir development controlling factors of the Cambro-Lower Ordovician dolomite in Tarim Basin[J].Journal of Northwest University:Natural Science Edition,2009,39(2):288-292.
[10] 沈安江,郑剑锋,潘文庆,等.塔里木盆地下古生界白云岩储层类型及特征[J].海相油气地质,2009,14(4):1-9.
Shen Anjiang,Zheng Jianfeng,Pan Wenqing,et al.A research on dolomite reservoirs types and their characteristics from Palaeozoic carbonate,located in Tarim Basin,Western China[J].Marine Origin Petroleum Geology,2009,14(4):1-9.
[11] 张静,罗平.塔里木盆地奥陶系孔隙型白云岩储层成因[J].石油实验地质,2010,32(5):470-474.
Zhang Jing,Luo Ping.Genesis of ordovician Matrix-porosity dolomite reservoir in the Tarim Basin[J].Petroleum Geology & Experiment,2010,32(5):470-474.
[12] 张学丰,刘波,蔡忠贤,等.白云岩化作用与碳酸盐岩储层物性[J].地质科技情报,2010,29(3):79-85.
Zhang Xuefeng,Liu Bo,Cai Zhongxian,et al.Dolomitization and carbonate reservoir formation[J].Geological Science and Technology Information,2010,29(3):79-85.
[13] 贾承造.中国塔里木盆地构造特征与油气[M].北京:石油工业出版社,1997:1-438.
Jia Chengzhao.Tectonic characteristics and petroleum of Tarim Basin,China[M].Beijing:Petroleum Industry Press, 1997:1-438.
[14] 冯增昭,鲍志东,吴茂炳,等.塔里木地区奥陶纪岩相古地理[J].古地理学报,2007,9(5):447-460.
Feng Zengzhao,Bao Zhidong,Wu Maobing,et al.Lithofacies palaeogeography of the Ordovician in Tarim area[J].Journal of Palaeogeography,2007,9(5):447-460.
[15] 赵宗举,吴兴宁,潘文庆,等.塔里木盆地奥陶纪层序岩相古地理[J].沉积学报,2009,27(5):939-955.
Zhao Zongju,Wu Xingning,Pan Wenqing,et al.Sequence lithofacies paleogeography of Ordovician in Tarim Basin[J].Acta Sedimentologica Sinica,2009,27(5):939-955.
[16] 赵俊兴,陈洪德,张锦泉,等.鄂尔多斯盆地中部马五段白云岩成因机理研究[J].石油学报,2005,26(5):38-47.
Zhao Junxing,Chen Hongde,Zhang Jinquan,et al.Genesis of dolomite in the fifth member of Majiagou Formation in the middle Ordos Basin[J].Acta Petrolei Sinica,2005,26(5):38-47.
[17] Tucker M E,Wright V P,Dickson J A D.Carbonate sedimentology[M].Oxford:Blackwell Science,1990:379-382.
[18] 李鹏春,陈广浩,曾乔松,等.塔里木盆地塔中地区下奥陶统白云岩成因[J].沉积学报,2011,29(5):842-856.
Li Pengchun,Chen Guanghao,Zeng Qiaosong,et al.Genesis of Lower Ordovician dolomite in central Tarim Basin[J].Acta Sedimentologica Sinica,2011,29(5):842-856.
[19] 强子同.碳酸盐岩储层地质学[M].北京:石油大学出版社,1998:207-257.
Qiang Zitong.Carbonate reservoir geology[M].Beijing:China University of Petroleum Press,1998:207-257.
[20] 胡文瑄,陈琪,王小林,等.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,2010,31(6):810-818.
Hu Wenxuan,Chen Qi,Wang Xiaolin,et al.REE models for the discrimination of fluids in the formation and evolution of dolomite reservoirs[J].Oil & Gas Geology,2010,31(6):810-818.
[21] 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.
[22] 郑荣才,党录瑞,郑超,等.川东-渝北黄龙组碳酸盐岩储层的成岩系统[J].石油学报,2010,31(2):237-245.
Zheng Rongcai,Dang Lurui,Zheng Chao,et al.Diagenetic system of carbonate reservoir in Huanglong Formation from East Sichuan to North Chongqing area[J].Acta Petrolei Sinica,2010,31(2):237-245.
[23] 彭苏萍,何宏,邵龙义,等.塔里木盆地∈-O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 Shuping,He Hong,Shao Longyi,et al.Carbon isotopic compositions of the Cambrian-Ordovician carbonates in Tarim Basin[J].Journal of China University of Mining & Technology,2002,31(4):353-357.
[24] 朱东亚,金之钧,胡文瑄.塔中地区热液改造型白云岩储层[J].石油学报,2009,30(5):698-704.
Zhu Dongya,Jin Zhijun,Hu Wenxuan.Hydrothermal alteration dolomite reservoir in Tazhong area[J].Acta Petrolei Sinica,2009,30(5):698-704.
[25] 黄文辉,杨敏,于炳松,等.塔中地区寒武系-奥陶系碳酸盐岩Sr元素和Sr同位素特征[J].地球科学——中国地质大学学报,2006,31(6):839-845.
Huang Wenhui,Yang Min,Yu Bingsong,et al.Strontium isotope composition and its characteristics analysis of Cambrian-Ordovician carbonate in Tazhong district,Tarim Basin[J].Earth Science:Journal of China University of Geosciences,2006,31(6):839-845.
[26] 郑荣才,耿威,郑超,等.川东北地区飞仙关组优质白云岩储层的成因[J].石油学报,2008,29(6):815-821.
Zheng Rongcai,Geng Wei,Zheng Chao,et al.Genesis of dolostone reservoir of Feixianguan Formation in Lower Triassic of northeast Sichuan Basin[J].Acta Petrolei Sinica,2008,29(6):815-821.
[27] 蔡春芳,李开开,李斌,等.塔河地区奥陶系碳酸盐岩缝洞充填物的地球化学特征及其形成流体分析[J].岩石学报,2009,25(10):2399-2404.
Cai Chunfang,Li Kaikai,Li Bin,et al.Geochemical characteristics and origins of fracture-and vug-fillings of the Ordovician in Tahe oilfield,Tarim Basin[J].Acta Petrologica Sinica,2009,25(10):2399-2404.
[28] 黄智斌,罗任辉,赖生华,等.塔里木油田野外地质考察基地建设(柯坪-巴楚)[R].库尔勒:中国石油塔里木油田公司,2008:9-11.
Huang Zhibin,Luo Renhui,Lai Shenghua,et al.Construction of the research base in Tarim Basin (Keping and Bachu Area)[R].Korla:PetroChina Tarim Oilfield Company,2008:9-11.
[29] 赵文智,沈安江,胡素云,等.塔里木盆地寒武-奥陶系白云岩储层类型与分布特征[J].岩石学报,2012,28(3):758-768.
Zhao Wenzhi,Shen Anjiang,Hu Suyun,et al.Types and distributional features of Cambrian-Ordovician dolostone reservoirs in Tarim Basin,northwestern China[J].Acta Petrologica Sinica,2012,28(3):758-768.
[30] Moore C H.Carbonate Reservoirs-Porosity evolution and digenesis in a sequence stratigraphic framework[M].Amsterdam:Elsevier,2001:145-183.
[31] Weyl P K.Porosity through dolomitization:conservation-of-mass requirements[J].Journal of Sedimentary Petrology,1960,30(1):85-90.
[32] Murray R C.Origin of porosity in carbonate rocks[J].Journal of Sedimentary Petrology,1960,30(1):59-84.
[33] Qing Sun.Dolomite reservoirs:porosity evolution and reservoir characteristics[J].AAPG Bulletin,1995,79(2):186-204.
[34] Warren J.Dolomite:oceurrence,evolution and economically important associations[J].Earth-Science Review, 2000,52(1/3):1-81.
[35] Lucia F J.Lower Paleozoic cavern development,collapse,and dolomitization,Franklin Mountains[J].AAPG Memoir,1995,63:279-300.
[36] Glover J E.Significance of stylolites in dolomitic limestones[J].Nature,1968,217(5131):835-836.
[37] Hugman R H H,Friedman G M.Effects of texture and composition on mechanical behaviour of experimentally deformed carbonate rocks[J].AAPG Bulletin,1979,63(9):1478-1489.

柯坪—巴楚露头区蓬莱坝组白云岩特征及孔隙成因

Characteristics and pore genesis of dolomite in the Penglaiba Formation in Keping-Bachu outcrop area

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