油气勘探

塔里木盆地北部地区超深断控油藏关键成藏期

  • 杨率 ,
  • 邬光辉 ,
  • 朱永峰 ,
  • 张银涛 ,
  • 赵星星 ,
  • 鲁子野 ,
  • 张宝收
展开
  • 1.西南石油大学地球科学与技术学院,成都 610500;
    2.中国石油天然气集团有限公司碳酸盐岩储层重点实验室西南石油大学研究分室,成都 610500;
    3.中国石油塔里木油田公司,新疆库尔勒 841000;
    4.中国石油西南油气田公司,成都 610051
杨率(1992-),男,四川南充人,现为西南石油大学在读博士研究生,主要从事构造地质与石油地质研究。地址:四川省成都市新都区新都大道8号,西南石油大学地球科学与技术学院,邮政编码:610500。E-mail:yangshuaiys@126.com

收稿日期: 2021-09-04

  网络出版日期: 2022-03-16

基金资助

国家自然科学基金(91955204); 中国石油-西南石油大学创新联合体科技合作项目(2020CX010101)

Key oil accumulation periods of ultra-deep fault-controlled oil reservoir in northern Tarim Basin, NW China

  • YANG Shuai ,
  • WU Guanghui ,
  • ZHU Yongfeng ,
  • ZHANG Yintao ,
  • ZHAO Xingxing ,
  • LU Ziye ,
  • ZHANG Baoshou
Expand
  • 1. School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, China;
    2. PetroChina Key Laboratory of Carbonate Reservoir, Southwest Petroleum University, Chengdu 610500, China;
    3. Tarim Oilfield Company, PetroChina, Korla 841000, China;
    4. Southwest Oil and Gas Field Company, PetroChina, Chengdu 610051, China

Received date: 2021-09-04

  Online published: 2022-03-16

摘要

塔里木盆地北部地区奥陶系碳酸盐岩发现了埋深大于6 000 m的断控型特大油田,关键成藏期厘定对油气成藏研究与勘探开发具有重要意义。在岩相学精细分析基础上,开展12口井断裂充填方解石的流体包裹体组合(FIA)测试分析,并结合烃源岩及其生油期、断裂与圈闭形成期研究断控油藏成藏期。结果表明,①FIA类型多样,主要存在坳陷区黄色荧光与隆起区黄绿色荧光2类不同成熟度油包裹体,指示2期石油充注;②FIA中盐水包裹体均一温度多遭受升温作用的影响,与油包裹体共生的盐水包裹体最小温度值更接近成藏期温度;③黄色荧光的FIA都检测到低于50 ℃的均一温度,黄绿色荧光的FIA均检测到70~90 ℃的温度数据,揭示中晚加里东期与晚海西期的2期石油成藏期;④中晚奥陶世为走滑断裂、奥陶系碳酸盐岩缝洞体储集层与圈闭的关键形成期;⑤下寒武统主力烃源岩的生油高峰期为晚奥陶世,坳陷区以晚奥陶世成藏为主,隆起区以早二叠世成藏为主。研究认为,塔里木盆地北部地区超深断控油藏关键成藏期为加里东晚期,坳陷区保存了加里东期的原生古油藏,隆起区发育晚海西期从坳陷区调整过来的次生油藏;保存条件是该区走滑断裂带石油富集的关键,阿满过渡带坳陷区油气更富集、勘探开发潜力更大。

本文引用格式

杨率 , 邬光辉 , 朱永峰 , 张银涛 , 赵星星 , 鲁子野 , 张宝收 . 塔里木盆地北部地区超深断控油藏关键成藏期[J]. 石油勘探与开发, 2022 , 49(2) : 249 -261 . DOI: 10.11698/PED.2022.02.04

Abstract

A giant fault-controlled oilfield has been found in the ultra-deep (greater than 6000 m) Ordovician carbonate strata in the northern Tarim Basin. It is of great significance for hydrocarbon accumulation study and oil exploitation to determine the key oil accumulation periods. Based on detailed petrographic analysis, fluid inclusion association (FIA) in calcite samples filling in fractures from 12 wells were analyzed, and key accumulation periods of the strike-slip fault-controlled oilfield was studied by combining oil generation periods of the source rocks, formation periods of the fault and traps, and the fluid inclusion data. (1) There are multiple types of FIA, among them, two types of oil inclusions, the type with yellow fluorescence from the depression area and the type with yellow-green fluorescence from the uplift area with different maturities indicate two oil charging stages. (2) The homogenization temperature of the brine inclusions in FIA is mostly affected by temperature rises, and the minimum temperature of brine inclusions symbiotic with oil inclusions is closer to the reservoir temperature during its forming period. (3) FIA with yellow fluorescence all have homogenization temperatures below 50℃, while the FIA with yellow-green fluorescence have homogenization temperatures of 70-90℃ tested, suggesting two oil accumulation stages in Middle-Late Caledonian and Late Hercynian. (4) The Middle-Late Ordovician is the key formation period of the strike-slip fault, fracture-cave reservoir and trap there. (5) The oil generation peak of the main source rock of the Lower Cambrian is in the Late Ordovician, and the oil accumulation stage is mainly the Late Ordovician in the depression area, but is mainly the Early Permian in the uplift area. The key oil accumulation period of the strike-slip fault-controlled reservoirs is the Late Caledonian, the depression area has preserved the primary oil reservoirs formed in the Caledonian, while the uplift area has secondary oil reservoirs adjusted from the depression area during the Late Hercynian. Oil reservoir preservation conditions are the key factor for oil enrichment in the strike-slip fault zone of northern Tarim, and the Aman transition zone in the depression is richer in oil and gas and has greater potential for exploration and development.

参考文献

[1] 魏国齐, 朱永进, 郑剑锋, 等. 塔里木盆地寒武系盐下构造-岩相古地理、规模源储分布与勘探区带评价[J]. 石油勘探与开发, 2021, 48(6): 1114-1126.
WEI Guoqi, ZHU Yongjin, ZHENG Jianfeng, et al. Tectonic- lithofacies paleogeography, large-scale source-reservoir distribution and exploration zones of Cambrian subsalt formation, Tarim Basin, NW China[J]. Petroleum Exploration and Development, 2021, 48(6): 1114-1126.
[2] 李建忠, 陶小晚, 白斌, 等. 中国海相超深层油气地质条件、成藏演化及有利勘探方向[J]. 石油勘探与开发, 2021, 48(1): 52-67.
LI Jianzhong, TAO Xiaowan, BAI Bin, et al. Geological conditions, reservoir evolution and favorable exploration directions of marine ultra-deep oil and gas in China[J]. Petroleum Exploration and Development, 2021, 48(1): 52-67.
[3] 康玉柱. 中国古生代海相油气田发现的回顾与启示[J]. 石油与天然气地质, 2007, 28(5): 570-575.
KANG Yuzhu. Review and revelation of oil/gas discoveries in the Paleozoic marine strata of China[J]. Oil & Gas Geology, 2007, 28(5): 570-575.
[4] 江同文, 韩剑发, 邬光辉, 等. 塔里木盆地塔中隆起断控复式油气聚集的差异性及主控因素[J]. 石油勘探与开发, 2020, 47(2): 213-224.
JIANG Tongwen, HAN Jianfa, WU Guanghui, et al. Differences and controlling factors of composite hydrocarbon accumulations in the Tazhong uplift, Tarim Basin, NW China[J]. Petroleum Exploration and Development, 2020, 47(2): 213-224.
[5] 王清华, 杨海军, 汪如军, 等. 塔里木盆地超深层走滑断裂断控大油气田的勘探发现与技术创新[J]. 中国石油勘探, 2021, 26(4): 58-71.
WANG Qinghua, YANG Haijun, WANG Rujun, et al. Discovery and exploration technology of fault-controlled large oil and gas fields of ultra-deep formation in strike slip fault zone in Tarim Basin[J]. China Petroleum Exploration, 2021, 26(4): 58-71.
[6] 焦方正. 塔里木盆地顺托果勒地区北东向走滑断裂带的油气勘探意义[J]. 石油与天然气地质, 2017, 38(5): 831-839.
JIAO Fangzheng. Significance of oil and gas exploration in NE strike-slip fault belts in Shuntuoguole area of Tarim Basin[J]. Oil & Gas Geology, 2017, 38(5): 831-839.
[7] 杨海军, 邓兴梁, 张银涛, 等. 塔里木盆地满深1井奥陶系超深断控碳酸盐岩油气藏勘探重大发现及意义[J]. 中国石油勘探, 2020, 25(3): 13-23.
YANG Haijun, DENG Xingliang, ZHANG Yintao, et al. Great discovery and its significance of exploration for Ordovician ultra-deep fault-controlled carbonate reservoirs of Well Manshen 1 in Tarim Basin[J]. China Petroleum Exploration, 2020, 25(3): 13-23.
[8] 漆立新. 塔里木盆地顺北超深断溶体油藏特征与启示[J]. 中国石油勘探, 2020, 25(1): 102-111.
QI Lixin. Characteristics and inspiration of ultra-deep fault-karst reservoir in the Shunbei area of the Tarim Basin[J]. China Petroleum Exploration, 2020, 25(1): 102-111.
[9] 韩剑发, 苏洲, 陈利新, 等. 塔里木盆地台盆区走滑断裂控储控藏作用及勘探潜力[J]. 石油学报, 2019, 40(11): 1296-1310.
HAN Jianfa, SU Zhou, CHEN Lixin, et al. Reservoir-controlling and accumulation-controlling of strike-slip faults and exploration potential in the platform of Tarim Basin[J]. Acta Petrolei Sinica, 2019, 40(11): 1296-1310.
[10] 云露. 顺北东部北东向走滑断裂体系控储控藏作用与突破意义[J]. 中国石油勘探, 2021, 26(3): 41-52.
YUN Lu. Controlling effect of NE strike-slip fault system on reservoir development and hydrocarbon accumulation in the eastern Shunbei area and its geological significance, Tarim Basin[J]. China Petroleum Exploration, 2021, 26(3): 41-52.
[11] LU Z Y, LI Y T, YE N, et al. Fluid inclusions record hydrocarbon charge history in the Shunbei area, Tarim Basin, NW China[J]. Geofluids, 2020, 2020: 8847247.
[12] 王斌, 赵永强, 何生, 等. 塔里木盆地顺北5号断裂带北段奥陶系油气成藏期次及其控制因素[J]. 石油与天然气地质, 2020, 41(5): 965-974.
WANG Bin, ZHAO Yongqiang, HE Sheng, et al. Hydrocarbon accumulation stages and their controlling factors in the northern Ordovician Shunbei 5 fault zone, Tarim Basin[J]. Oil & Gas Geology, 2020, 41(5): 965-974.
[13] 韩强, 云露, 蒋华山, 等. 塔里木盆地顺北地区奥陶系油气充注过程分析[J]. 吉林大学学报(地球科学版), 2021, 51(3): 645-658.
HAN Qiang, YUN Lu, JIANG Huashan, et al. Marine oil and gas filling and accumulation process in the north of Shuntuoguole area in northern Tarim Basin[J]. Journal of Jilin University (Earth Science Edition), 2021, 51(3): 645-658.
[14] 常象春, 王铁冠, 李启明, 等. 哈拉哈塘凹陷新垦区块奥陶系油气成藏的地球化学证据[J]. 中国石油大学学报(自然科学版), 2013, 37(3): 44-49.
CHANG Xiangchun, WANG Tieguan, LI Qiming, et al. Hydrocarbon entrapment and accumulation for Ordovician reservoirs from Xinken block of Halahatang Depression as constrained from oil geochemistry[J]. Journal of China University of Petroleum (Edition of Natural Science), 2013, 37(3): 44-49.
[15] XIAO Z Y, LI M J, HUANG S Y, et al. Source, oil charging history and filling pathways of the Ordovician carbonate reservoir in the Halahatang oilfield, Tarim Basin, NW China[J]. Marine and Petroleum Geology, 2016, 73: 59-71.
[16] GE X, SHEN C B, SELBY D, et al. Petroleum evolution within the Tarim Basin, northwestern China: Insights from organic geochemistry, fluid inclusions, and rhenium-osmium geochronology of the Halahatang oil field[J]. AAPG Bulletin, 2020, 104(2): 329-355.
[17] LI J F, ZHANG Z Y, ZHU G Y, et al. The origin and accumulation of ultra-deep oil in Halahatang area, northern Tarim Basin[J]. Journal of Petroleum Science and Engineering, 2020, 195: 107898.
[18] 陈红汉, 吴悠, 丰勇, 等. 塔河油田奥陶系油气成藏期次及年代学[J]. 石油与天然气地质, 2014, 35(6): 806-819.
CHEN Honghan, WU You, FENG Yong, et al. Timing and chronology of hydrocarbon charging in the Ordovician of Tahe oilfield, Tarim Basin, NW China[J]. Oil & Gas Geology, 2014, 35(6): 806-819.
[19] WANG Y Y, CHEN J F, PANG X Q, et al. Faulting controls on oil and gas composition in the Yingmai 2 oilfield, Tarim Basin, NW China[J]. Organic Geochemistry, 2018, 123: 48-66.
[20] GOLDSTEIN R H. Petrographic analysis of fluid inclusions[M]// SAMSON I, ANDERSON A, MARSHALL D. Fluid inclusions: Analysis and interpretation. Ottawa: Mineralogical Association of Canada, 2003: 9-53.
[21] 池国祥, 卢焕章. 流体包裹体组合对测温数据有效性的制约及数据表达方法[J]. 岩石学报, 2008, 24(9): 1945-1953.
CHI Guoxiang, LU Huanzhang. Validation and representation of fluid inclusion microthermometric data using the fluid inclusion assemblage (FIA) concept[J]. Acta Petrologica Sinica, 2008, 24(9): 1945-1953.
[22] 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.
JIA Chengzao. Tectonic characteristics and petroleum, Tarim Basin[M]. Beijing: Petroleum Industry Press, 1997.
[23] 杨海军, 邬光辉, 韩剑发, 等. 塔里木克拉通内盆地走滑断层构造解析[J]. 地质科学, 2020, 55(1): 1-16.
YANG Haijun, WU Guanghui, HAN Jianfa, et al. Structural analysis of strike-slip faults in the Tarim intracratonic basin[J]. Chinese Journal of Geology, 2020, 55(1): 1-16.
[24] WU G H, YUAN Y J, HUANG S Y, et al. The dihedral angle and intersection processes of a conjugate strike-slip fault system in the Tarim Basin, NW China[J]. Acta Geologica Sinica, 2018, 92(1): 74-88.
[25] WU G H, KIM Y S, SU Z, et al. Segment interaction and linkage evolution in a conjugate strike-slip fault system from the Tarim Basin, NW China[J]. Marine and Petroleum Geology, 2020, 112: 104054.
[26] 邬光辉, 马兵山, 韩剑发, 等. 塔里木克拉通盆地中部走滑断裂形成与发育机制[J]. 石油勘探与开发, 2021, 48(3): 510-520.
WU Guanghui, MA Bingshan, HAN Jianfa, et al. Origin and growth mechanisms of strike-slip faults in the central Tarim cratonic basin, NW China[J]. Petroleum Exploration and Development, 2021, 48(3): 510-520.
[27] YANG P, WU G H, NURIEL P, et al. In situ LA-ICPMS U-Pb dating and geochemical characterization of fault-zone calcite in the central Tarim Basin, northwest China: Implications for fluid circulation and fault reactivation[J]. Chemical Geology, 2021, 568: 120125.
[28] QIU N S, CHANG J, ZUO Y H, et al. Thermal evolution and maturation of Lower Paleozoic source rocks in the Tarim Basin, northwest China[J]. AAPG Bulletin, 2012, 96(5): 789-821.
[29] WU G H, XIE E, ZHANG Y F, et al. Structural diagenesis in carbonate rocks as identified in fault damage zones in the northern Tarim Basin, NW China[J]. Minerals, 2019, 9(6): 360.
[30] PING H W, CHEN H H, JIA G H. Petroleum accumulation in the deeply buried reservoirs in the northern Dongying Depression, Bohai Bay Basin, China: New insights from fluid inclusions, natural gas geochemistry, and 1-D basin modeling[J]. Marine and Petroleum Geology, 2017, 80: 70-93.
[31] 韩剑发, 邬光辉, 肖中尧, 等. 塔里木盆地寒武系烃源岩分布的重新认识及其意义[J]. 地质科学, 2020, 55(1): 17-29.
HAN Jianfa, WU Guanghui, XIAO Zhongyao, et al. Recognition of the distribution of Cambrian source rocks and its significance for exploration in Tarim Basin[J]. Chinese Journal of Geology, 2020, 55(1): 17-29.
[32] ZHU G Y, LI T T, ZHANG Z Y, et al. Distribution and geodynamic setting of the Late Neoproterozoic-Early Cambrian hydrocarbon source rocks in the South China and Tarim Blocks[J]. Journal of Asian Earth Sciences, 2020, 201: 104504.
[33] 杨海军, 于双, 张海祖, 等. 塔里木盆地轮探1井下寒武统烃源岩地球化学特征及深层油气勘探意义[J]. 地球化学, 2020, 49(6): 666-682.
YANG Haijun, YU Shuang, ZHANG Haizu, et al. Geochemical characteristics of Lower Cambrian sources rocks from the deepest drilling of Well LT-1 and their significance to deep oil gas exploration of the Lower Paleozoic system in the Tarim Basin[J]. Geochimica, 2020, 49(6): 666-682.
[34] 谷茸, 云露, 朱秀香, 等. 塔里木盆地顺北油田油气来源研究[J]. 石油实验地质, 2020, 42(2): 248-254, 262.
GU Rong, YUN Lu, ZHU Xiuxiang, et al. Oil and gas sources in Shunbei oilfield, Tarim Basin[J]. Petroleum Geology and Experiment, 2020, 42(2): 248-254, 262.
[35] NURIEL P, ROSENBAUM G, UYSAL T I, et al. Formation of fault-related calcite precipitates and their implications for dating fault activity in the East Anatolian and Dead Sea fault zones[J]. Geological Society, London, Special Publications, 2011, 359(1): 229-248.
[36] YANG H J, WU G H, SCARSELLI N, et al. Characterization of reservoirs, fluids, and productions from the Ordovician carbonate condensate field in the Tarim Basin, northwestern China[J]. AAPG Bulletin, 2020, 104(7): 1567-1592.
文章导航

/