吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (2): 509-517.doi: 10.13278/j.cnki.jjuese.20190269

• 沉积盆地分析 • 上一篇    下一篇

塔里木盆地哈拉哈塘地区石炭系东河砂岩段碳酸盐胶结物沉积特征及其成因

陈秀艳1, 王剑2, 张立平1, 马德波1, 周波1   

  1. 1. 中国石油勘探开发研究院, 北京 100083;
    2. 中海油研究总院有限责任公司, 北京 100028
  • 收稿日期:2019-12-10 出版日期:2020-03-26 发布日期:2020-03-31
  • 作者简介:陈秀艳(1979-),女,高级工程师,博士,主要从事层序地层学及沉积储层方面的研究,E-mail:chenxiuyan1004@petrochina.com.cn
  • 基金资助:
    国家油气重大专项(2011ZX05001)

Sedimentary Characteristics and Genesis of Carbonate Cements in Carboniferous Donghe Sandstone Member, Hanilcatam Area of Tarim Basin

Chen Xiuyan1, Wang Jian2, Zhang Liping1, Ma Debo1, Zhou Bo1   

  1. 1. Research Institute of Petroleum Exploration&Development, PetroChina, Beijing 100083, China;
    2. Research Institute Co., Ltd., CNOOC, Beijing 100028, China
  • Received:2019-12-10 Online:2020-03-26 Published:2020-03-31
  • Supported by:
    Supported by National Oil and Gas Major Project(2011ZX05001)

摘要: 塔里木盆地石炭系东河砂岩是我国典型的深埋海相碎屑岩优质储层,储集砂体物性好,但受碳酸盐胶结物影响导致非均质性较强。为了更准确地预测优质储层发育带,通过精细岩心观察、大量薄片鉴定及碳氧同位素和阴极发光资料分析,对哈拉哈塘地区石炭系东河砂岩段碳酸盐胶结物宏观及微观沉积特征和成因进行了研究。研究发现:前滨及上临滨相带砂岩含油性较好,不含油的含碳酸盐胶结物砂层主要有Ⅰ类生物潜穴型、Ⅱ类层理纹层型、Ⅲ类薄层灰质砂岩型和Ⅳ类钙质砂岩团块型4种岩性组合;碳酸盐胶结物主要类型为方解石,其次为铁方解石,主要填充在溶蚀粒间孔及碎屑颗粒粒内溶孔中。东河砂岩储层中碳酸盐胶结物主要为有机酸脱羧成因,常见于Ⅱ、Ⅲ类岩性组合;少量生物成因及沉积暴露成因,主要见于Ⅰ类和Ⅳ类岩性组合。研究区碳酸盐胶结物δ13C较高的关键原因是东侧轮南低凸起的奥陶系碳酸盐岩地层侵蚀溶蚀供给。

关键词: 碳酸盐胶结物, 沉积特征, 碳氧同位素, 东河砂岩, 塔里木盆地

Abstract: The Carboniferous Donghe sandstone in Tarim basin is a typical deep-buried marine clastic reservoir in China, which has good physical properties and strong heterogeneity influenced by carbonate cements. In order to predict the beneficial zones of high quality reservoir more accurately, the authors studied the sedimentary characteristics and genesis of the carbonate cements in Donghe sandstone through core observation, variety of thin section identification, carbon and oxygen isotope, and cathodoluminescence analyses. It indicates the sandstones on foreshore and upper shore face are rich in oil, while the oil-free sandstones contain four types of carbonate cement:Ⅰ-biological burrow type, Ⅱ-bedding-laminae type, Ⅲ-thin calcareous sandstone intercalated in thick sandstone type, and Ⅳ-calcareous sandstone globular type. The carbonate cements include more calcite and some ferro-calcite, which usually fill in the intergranular and intragranular dissolved pores. The genesis of carbonate cements in Donghe sandstone is more organic acid decarboxylation in type Ⅱ and type Ⅲ lithologic associations; and some of the type Ⅰ and type Ⅳ are biogenesis and outcrop sedimentology. The key reason of heavy δ13C in the study area is the erosion and solution of Ordovician carbonate rocks from the eastern Lunnan low salience.

Key words: carbonate cements, sedimentary characteristics, carbon and oxygen isotope, Donghe sandstone, Tarim basin

中图分类号: 

  • P588.212
[1] Kantorowicz J D,Bryant I D,Dawans J M.Controls on the Geometry and Distribution of Carbonate Cements in Jurassic Sandstones:BridportSands,Southern England and Viking Group,Troll Field,Norway[C]//Diagenesis of Sedimentary Sequences.London:Geological Society of London,Special Publication,1987:103-118.
[2] Boles J R.Carbonate Cementation in Tertiary Sandstones,SAN Joaquin Basin,California[C]//Carbonate Cementation in Sandstones.London:Blackwell Science,1998:261-283.
[3] 张永旺,曾溅辉,高霞,等. 东营凹陷古近系储层碳酸盐胶结物分布特征及主控因素[J].吉林大学学报(地球科学版),2009,39(1):16-22. Zhang Yongwang, Zeng Jianhui, Gao Xia, et al. Distribution Characteristics and Main Controlling Factors of Carbonate Cements in the Paleogene Reservoirs in Dongying Depression[J]. Journal of Jilin University (Earth Science Edition), 2009,39(1):16-22.
[4] 郭佳,曾溅辉,宋国奇,等. 东营凹陷中央隆起带沙河街组碳酸盐胶结物发育特征及其形成机制[J].地球科学:中国地质大学学报,2014,39(5):565-575. Guo Jia,Zeng Jianhui, Song Guoqi, et al. Characteristics and Origin of Carbonate Cements of Shahejie Formation of Central Uplift Belt in Dongying Depression[J]. Eearth Science:Journal of China University of Geosciences, 2014,39(5):565-575.
[5] 付锁堂,王震亮,张永庶,等. 柴北缘西段鄂博梁构造带储层碳酸盐胶结物成因及其油气地质意义:来自碳、氧同位素的约束[J].沉积学报,2015,33(5):991-999. Fu Suotang, Wang Zhenliang, Zhang Yongshu, et al. Origin of Carbonate Cements in Reservoir Rocks and Its Petroleum Geologic Significance:Eboliang Structure Belt, Northern Margin of Qaidam Basin[J]. Acta Sedimentologica Sinica, 2015,33(5):991-999.
[6] 陈波,陈汾君,马进业,等. 冷湖地区上干柴沟组储层碳酸盐胶结物特征及地质意义[J].大庆石油地质与开发,2016,35(5):28-33. Chen Bo, Chen Fenjun, Ma Jinye, et al. Characteristics and Their Geological Significances of the Carbonate Cements in Shangganchaigou Formation Reservoirs of Lenghu Area[J]. Petroleum Geology and Oilfield Development in Daqing, 2016,35(5):28-33.
[7] 徐北煤,卢冰.硅质碎屑岩中碳酸盐胶结物及其对储层的控制作用的研究[J].沉积学报,1994,12(3):56-63. Xu Beimei,Lu Bing. The Study of Diagenetic Carbonate in Siliciclastic Rock and Its Control on the Reservoir[J]. Acta Sedimentologica Sinica, 1994,12(3):56-63.
[8] 王琪,郝乐伟,陈国俊,等. 白云凹陷珠海组砂岩中碳酸盐胶结物的形成机理[J].石油学报,2010,31(4):553-558. Wang Qi, Hao Lewei, Chen Guojun, et al. Forming Mechanism of Carbonate Cements in Siliciclastic Sandstone of Zhuhai Formation in Baiyun Sag[J]. Acta Petrolei Sinica, 2010,31(4):553-558.
[9] 田亚铭,施泽进,李庭艳,等. 姬塬地区长8油层组碳酸盐胶结物特征与成因[J].西安石油大学学报(自然科学版),2011,26(3):26-30. Tian Yaming, Shi Zejin, Li Tingyan, et al. Characteristics and Origin of the Carbonate Cements of Chang 8 Member in Jiyuan Area, Ordos Basin[J]. Journal of Xi 'an Shiyou University (Natural Science Edition), 2011, 26(3):26-30.
[10] 张新桂,徐国盛,张以明,等. 饶阳凹陷沙河街组碎屑岩储层碳酸盐胶结物形成机制及其对储层质量的影响[J].矿物岩石,2017,37(2):111-119. Zhang Xingui, Xu Guosheng, Zhang Yiming, et al. Formation Mechanism of Carbonate Cements and Its Influence on Reservoir Quality in Clastic Reservoir of Shahejie Formation, Raoyang Sag[J]. Journal of Mineralogy and Petrology,2017,37(2):111-119.
[11] Marco A S, Ronald C S. Diagenetic Heterogeneity and Reservoir Quality:Fluvial, Deltaic, and Turbiditic Sandstone Reservoirs, Potiguar and Reconcavo Rift Basins, Brazil[J]. AAPG Bulletin, 1993, 77:1142-1156.
[12] Sylvia M C, Luiz F D, Rogério S D, et al. Depositional and Diagenetic Controls on the Reservoir Quality of Lower Cretaceous, Pendeencia Sandstones, Potiguar Rift Basin, Brazil[J]. AAPG Bulletin, 2000, 84:1719-1742.
[13] Kitty L M. Diagenetic Heterogeneity in Sandstone at the Outcrop Scale, Breathitt Formation (Pennsylvanian), Eastern Kentucky[J]. AAPG Bulletin, 2001, 85:795-815.
[14] Shirley P D, Christopher D W, Brian J W, et al. Calcite Cement Distribution and Its Effect on Fluid Flow in a Deltaic Sandstone, Frontier Formation, Wyoming[J]. AAPG Bulletin, 2002, 86:2007-2021.
[15] 赵洪,罗晓容,肖中尧,等. 塔里木盆地哈得逊油田东河砂岩隔夹层特征及其石油地质意义[J].天然气地球科学,2014,25(6):824-833. Zhao Hong, Luo Xiaorong, Xiao Zhongyao, et al. Interlayer Features and Petroleum Geology Meaning of Donghe Sandstones in the Hadson Oilfield[J]. Natural Gas Geoscience, 2014, 25(6):824-833.
[16] 王洋,刘婧,汪建国,等. 塔里木盆地东河1油藏东河砂岩隔夹层形成的主控因素及流体来源[J].石油学报,2015,36(2):174-181. Wang Yang, Liu Jing, Wang Jianguo,et al. Major Controlling Factors for the Formation of Interlayer of Donghe Sandstone of Donghe 1 Reservoir in Tarim Basin and Its Fluid Source[J]. Acta Petrolei Sinica, 2015,36(2):174-181.
[17] 陈秀艳,罗平,贾进华,等. 塔北中部石炭系东河砂岩物源及沉积体系[J].海相油气地质,2013,18(2):23-30. Chen Xiuyan, Luo Ping, Jia Jinhua, et al. Provenances and Sedimentary Facies Distribution in Carboniferous Donghe Sandstone in the Central Part of Northern Tarim Basin[J]. Marine Origin Petroleum Geology, 2013,18(2):23-30.
[18] 陈秀艳,贾进华,崔文娟,等. 塔里木盆地哈拉哈塘地区东河砂岩段成岩作用及对孔渗影响[J].天然气地球科学,2019,30(1):51-60. Chen Xiuyan, Jia Jinhua, Cui Wenjuan, et al. Diagenesis and Its Effect on Pore and Permeability of Donghe Sandstone in Hanilcatam Area, Tarim Basin[J]. Natural Gas Geoscience, 2019,30(1):51-60.
[19] 贾进华,申银民. 塔里木盆地东河砂岩段准层序组特征及岩相古地理与砂体分布[J].石油学报,2017,38(2):135-150. Jia Jinhua,Shen Yinmin. Parasequence Set Division, Lithofacies Paleogeography and Sandbody Distribution of Donghe Sandstone Member in Tarim Basin[J]. Acta Petrolei Sinica, 2017,38(2):135-150.
[20] James N P, Dalrymple R W. Facies Models:4[M]. Newfoundland:Geological Association of Canada, 2010:167-195.
[21] 刘娅铭,姜在兴,朱井泉,等.东河砂岩中碳酸盐胶结物特征及对储层的影响[J].大庆石油地质与开发,2006,25(3):13-15. Liu Yaming, Jiang Zaixing, Zhu Jingquan, et al. Characteristics of Carbonate Cement in Donghe Sandstone and Its Effect on Reservoir[J]. Petroleum Geology & Oilfield Development in Daqing, 2006,25(3):13-15.
[22] 郭宏莉,王大锐. 塔里木油气区砂岩储集层碳酸盐胶结物的同位素组成与成因分析[J]. 石油勘探与开发,1999,26(3):31-32. Guo Hongli,Wang Darui. The Isotopic Composition and Genesis Analysis of Carbonate Cement in Sandstone Reservoir, Tarim Hydrocarbon Area[J]. Petroleum Exploration and Development, 1999,26(3):31-32.
[23] 姚泾利,王琪,张瑞,等. 鄂尔多斯盆地中部延长组砂岩中碳酸盐胶结物成因与分布规律研究[J]. 天然气地球科学,2011,22(6):943-950. Yao Jingli, Wang Qi, Zhang Rui, et al. Origin and Spatial Distribution of Carbonate Cements in Yanchang Fm(Triassic) Sandstones Within the Lacustrine Center of Ordos Basin,NW China[J]. Natural Gas Geoscience, 2011,22(6):943-950.
[24] Keith M L, Weber J N. Carbon and Oxygen Isotopic Composition of Selected Limestones and Fossils[J].Geochimica et Cosmochimica Acta,1964,28(10/11):1786-1816.
[25] Irwin H,Curtis C,Coleman M. Isotopic Evidence for Source of Diagenetic Carbonates Formed During Burial of Organic-Rich Sediments[J].Nature,1977,269:209-213.
[26] Klein J S,Mozley P,Campbell A, et al.Spatial Distribution of Carbon and Oxygen Isotopes in Laterally Extensive Carbonate-Cemented Layers:Implications for Mode of Growth and Subsurface Identification[J].Journal of Sedimentary Research,1999,69:184-191.
[27] 吕成福,李晓燕,陈国俊,等.酒东坳陷下白垩统砂岩中碳酸盐胶结物特征与储层物性[J].沉积学报,2011,29(6):1138-1143. Lü Chengfu, Li Xiaoyan, Chen Guojun. et al. Characteristics of Carbonate Cements and Reservoir Quality of the Lower Cretaceous Sandstone in Jiudong Sag[J]. Acta Sedimentologica Sinica,2011,29(6):1138-1143.
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