岩性油气藏 ›› 2022, Vol. 34 ›› Issue (2): 86–94.doi: 10.12108/yxyqc.20220208

• 地质勘探 • 上一篇    下一篇

鄂尔多斯盆地中东部米脂地区奥陶系马五5亚段叠层石白云岩特征及其地质意义

罗振锋1, 苏中堂1,2, 廖慧鸿1, 黄文明3, 马慧1, 佘伟1   

  1. 1. 成都理工大学 沉积地质研究院, 成都 610059;
    2. 油气藏地质及开发工程国家重点实验室, 成都 610059;
    3. 中国石油川庆钻探工程有限公司 苏里格项目经理部, 成都 610051
  • 收稿日期:2021-05-24 修回日期:2021-09-17 出版日期:2022-03-01 发布日期:2022-03-14
  • 第一作者:罗振锋(1998-),男,成都理工大学在读硕士研究生,研究方向为碳酸盐岩储层。地址:(610059)四川省成都市成华区东三路1号成都理工大学。Email:609558795@qq.com。
  • 通信作者: 苏中堂(1981-)男,博士,副教授,主要从事沉积地质学方面的教学与研究工作。Email:suzhongtang2012@cdut.edu.cn。
  • 基金资助:
    国家自然科学青年基金项目“鄂尔多斯盆地天环地区下奥陶统白云岩成因机制分析”（编号：41302087）资助

Characteristics and geological significance of stromatolite dolomite of Ma 55 submember of Ordovician Majiagou Formation in Mizhi area, central-eastern Ordos Basin

LUO Zhenfeng1, SU Zhongtang1,2, LIAO Huihong1, HUANG Wenming3, MA Hui1, SHE Wei1   

  1. 1. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China;
    2. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu 610059, China;
    3. Sulige Project Management Department, Chuanqing Drilling Engineering Co., Ltd., CNPC, Chengdu 610051, China
  • Received:2021-05-24 Revised:2021-09-17 Online:2022-03-01 Published:2022-03-14

PDF (PC)

258

摘要： 鄂尔多斯盆地中东部米脂地区马五5亚段底部发育一套叠层石白云岩，是研究微生物岩及微生物白云岩化作用的良好素材。通过岩石学、矿物学、阴极发光、扫描电镜、碳氧锶同位素及地球化学等分析，对米脂地区奥陶系马五5亚段叠层石白云岩进行了研究，确定了马五5亚段沉积环境，并探讨了该套叠层石白云岩的成因及其地质意义。研究结果表明：①研究区叠层石按形态特征可划分为柱状与枝状，白云石晶体呈微—粉晶，阴极发光为暗红色，扫描电镜下见白云石呈粒状产出。②叠层石白云岩的δ13C值（-4.15‰~-0.80‰）位于同期海水值范围内，δ18O值（-13.19‰~-6.62‰）与同期海水值相比明显偏负；87Sr/86Sr值（0.708 9~0.709 8）较同期海水偏高；Fe，Mn，Na含量均相对较高，Sr含量相对较低，显示其白云石化流体主要为海源性流体，混有大气淡水，为潮间—潮下带的浅埋藏渗透回流作用的产物。③海侵初期海水盐度转换的潮间带为叠层石白云岩油气勘探的有利区域。

关键词: 叠层石白云岩, 渗透回流白云岩化, 潮坪, 马五5亚段, 奥陶系, 米脂地区, 鄂尔多斯盆地

Abstract: A set of stromatolite dolomite developed at the bottom of Ma55 submember of Majiagou Formation in Mizhi area, central-eastern Ordos Basin, which is a good material for studying microbial rocks and microbial dolomitization. The stromatolite dolomite was studied through the analysis of petrology, mineralogy, cathodoluminescence, scanning electron microscope, carbon, oxygen and strontium isotopes, geochemistry, the sedimentary environment of Ma 55 submember was determined, and the genesis and geological significance of this set of stromatolite dolomite were discussed. The research results show that:(1) The stromatolites in the study area can be divided into columnar and dendritic according to the morphological characteristics, the dolomite crystal is microcrystalline, and it is dark red in the cathodoluminescence, and the dolomite is granular under the scanning electron microscope.(2) The δ13C value of stromatolite dolomite(-4.15‰--0.80‰) is generally within the range of seawater value in the same period, and the δ18O value(-13.19‰--6.62‰) is obviously negative compared with the seawater value in the same period. The 87Sr/86Sr value(0.708 9-0.709 8) is higher than that of seawater in the same period. The contents of Fe, Mn, Na of the stromatolite dolomite are relatively high, and the Sr content is relatively low. The dolomitization fluid of the stromatolite dolomite of Ma 55 submember in the study area is mainly marine-derived fluid, mixed with atmospheric fresh water, which is the product of shallow buried infiltration and reflux in the intertidal-subtidal zone.(3) The intertidal zone with seawater salinity conversion in the early stage of transgression is a favorable area for oil and gas exploration of stromatolite dolomite.

Key words: stromatolite dolomite, seepage reflux dolomitization, tidal flat, Ma 55 submember, Ordovician, Mizhi area, Ordos Basin

中图分类号: 

  • TE122.2
[1] 付金华, 范立勇, 刘新社, 等.鄂尔多斯盆地天然气勘探新进展、前景展望和对策措施[J].中国石油勘探, 2019, 24(4):418-430. FU Jinhua, FAN Liyong, LIU Xinshe, et al. New progresses, prospects and countermeasures of natural gas exploration in the Ordos Basin[J]. China Petroleum Exploration, 2019, 24(4):418-430.
[2] 王保全, 强子同, 张帆, 等.鄂尔多斯盆地奥陶系马家沟组马五段白云岩的同位素地球化学特征[J].地球化学, 2009, 38 (5):472-479. WANG Baoquan, QIANG Zitong, ZHANG Fan, et al. Isotope characteristics of dolomite from the fifth member of the Ordovician Majiagou Formation, the Ordos Basin[J]. Geochimica, 2009, 38(5):472-479.
[3] 赵卫卫, 王宝清.鄂尔多斯盆地苏里格地区奥陶系马家沟组马五段白云岩的地球化学特征[J].地球学报, 2011, 32(6):681-690. ZHAO Weiwei, WANG Baoqing. Geochemical characteristics of dolomite from 5th member of the Ordovician Majiagou Formation in Sulige area, Ordos Basin[J]. Acta Geoscientica Sinica, 2011, 32(6):681-690.
[4] 包洪平, 杨帆, 白海峰, 等.细分小层岩相古地理编图的沉积学研究及油气勘探意义:以鄂尔多斯地区中东部奥陶系马家沟组马五段为例[J].岩石学报, 2017, 33(4):1094-1106. BAO Hongping, YANG Fan, BAI Haifeng, et al. Sedimentology study on submember lithofacies paleogeography mapping and its petroleum exploration significance:Taking Ma 5 member of Lower Ordovician Majiagou Formation in central-eastern Ordos Basin for example[J]. Acta Petrologica Sinica, 2017, 33(4):1094-1106.
[5] 张永生.鄂尔多斯地区奥陶系马家沟群中部块状白云岩的深埋藏白云石化机制[J].沉积学报, 2000, 18(4):424-430. ZHANG Yongsheng. Mechanism of deep burial dolomitization of massive dolostones in the middle Majiagou group of the Ordovician, Ordos Basin[J]. Acta Sedimentologica Sinica, 2000, 18(3):424-430.
[6] 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):38-41. 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):38-41.
[7] 刘德良, 孙先如, 李振生, 等.鄂尔多斯盆地奥陶系白云岩碳氧同位素分析[J].石油实验地质, 2006, 28(2):155-161. LIU Deliang, SUN Xianru, LI Zhensheng, et al. Analysis of carbon and oxygen isotope on the Ordovician dolostones in the Ordos Basin[J]. Petroleum Geology & Experiment, 2006, 28(2):155-161.
[8] 黄擎宇, 张哨楠, 丁晓琪, 等.鄂尔多斯盆地西南缘奥陶系马家沟组白云岩成因研究[J].石油实验地质, 2010, 32(2):147-153. HUANG Qingyu, ZHANG Shaonan, DING Xiaoqi, et al. Origin of dolomite of Ordovician Majiagou Formation, western and southern margin of the Ordos Basin[J]. Petroleum Geology & Experiment, 2010, 32(2):147-153.
[9] 苏中堂, 陈洪德, 徐粉燕, 等.鄂尔多斯盆地马家沟组白云岩地球化学特征及白云岩化机制分析[J].岩石学报, 2011, 27(8):2230-2238. SU Zhongtang, CHEN Hongde, XU Fenyan, et al. Geochemistry and dolomitization mechanism of Majiagou dolomites in Ordovician, Ordos, China[J]. Acta Petrologica Sinica, 2011, 27(8):2230-2238.
[10] 杨华, 王宝清, 孙六一, 等.鄂尔多斯盆地中奥陶统马家沟组碳酸盐岩碳、氧稳定同位素特征[J].天然气地球科学, 2012, 23(4):616-625. YANG Hua, WANG Baoqing, SUN Liuyi, et al. Characteristics of oxygen and carbon stable isotopes for Middle Ordovician Majiagou Formation carbonate rocks in the Ordos Basin[J]. Natural Gas Geoscience, 2012, 23(4):616-625.
[11] 付金华, 吴兴宁, 孙六一, 等.鄂尔多斯盆地马家沟组中组合岩相古地理新认识及油气勘探意义[J].天然气工业, 2017, 37 (3):9-16. FU Jinhua, WU Xingning, SUN Liuyi, et al. New understandings of the lithofacies paleogeography of the middle assemblage of Majiagou Fm in the Ordos Basin and its exploration significance[J]. Natural Gas Industry, 2017, 37(3):9-16.
[12] 包洪平, 杨承运.鄂尔多斯东部奥陶系马家沟组微相分析[J].古地理学报, 2000, 2(1):31-42. BAO Hongping, YANG Chengyun. Study on microfacies of Majiagou Formation, Lower Ordovician, eastern Ordos, North China[J]. Journal of Palaeogeography, 2000, 2(1):31-42.
[13] 黄丽梅, 李建明, 黄正良, 等.鄂尔多斯盆地东部地区早奥陶世马家沟期沉积模式探讨[J].新疆地质, 2012, 30(1):80-84. HUANG Limei, LI Jianming, HUANG Zhengliang, et al. Discussion on the Lower Ordovician Majiagou Formation of eastern Ordos Basin[J]. Xinjiang Geology, 2012, 30(1):80-84.
[14] 付斯一, 陈洪德, 苏中堂, 等.鄂尔多斯盆地奥陶系马家沟组中组合沉积微相特征及演化[J].中国矿业, 2015, 24(3):81-86. FU Siyi, CHEN Hongde, SU Zhongtang, et al. The characteristic and evolution of sedimentary microfacies in the middle Ordovician assemblages in the Ordos Basin[J]. China Mining Magazine, 2015, 24(3):81-86.
[15] 董兆雄, 赵敬松, 方少仙, 等.鄂尔多斯盆地南部奥陶纪末端变陡缓坡沉积模式[J].西南石油学院学报, 2002, 24(1):50-52. DONG Zhaoxiong, ZHAO Jingsong, FANG Shaoxian, et al. Sedimentary model of distally steepening ramp of Ordovician in southern Ordos Basin[J]. Journal of Southwest Petroleum Institute, 2002, 24(1):50-52.
[16] 冯增昭.我国古地理学的形成、发展与展望[J].古地理学报, 1999, 1(2):1-7. FENG Zengzhao. Origin, development and future of palaeogeography of China[J]. Journal of Palaeogeography, 1999, 1(2):1-7.
[17] 冯增昭.我国古地理学的形成、发展、问题和共识[J].古地理学报, 2003, 5(2):129-141. FENG Zengzhao. Origin, development, problems and common viewpoint of palaeogeography of China[J]. Journal of Palaeogeography, 2003, 5(2):129-141.
[18] 冯增昭.单因素分析多因素综合作图法:定量岩相古地理重建[J].古地理学报, 2004, 6(1):3-19. FENG Zengzhao. Single factor analysis and multifactor comprehensive mapping method:Reconstruction of quantitative lithofacies palaeogeography[J]. Journal of Palaeogeography, 2004, 6(1):3-19.
[19] 梅冥相, 高金汉, 孟庆芬, 等.天津蓟县中元古界雾迷山组微指状叠层石及其对 1 250 Ma±叠层石衰减事件的响应[J].古地理学报, 2008, 10(5):495-509. MEI Mingxiang, GAO Jinhan, MENG Qingfen, et al. Microdigital stromatolites and their response to stromatolite decline at 1 250 Ma ±for the Mesoproterozoic Wumishan Formation at Jixian section in Tianjin[J]. Journal of Palaeogeography, 2008, 10(5):495-509.
[20] WALTER M R. Stromatolites, developments in sedimentology[M]. Amsterdam:Elsevier, 1976.
[21] 李翔, 王建功, 李飞, 等.柴达木盆地西部始新统湖相微生物岩沉积特征:以西岔沟和梁东地区下干柴沟组为例[J].岩性油气藏, 2021, 33(3):63-73. LI Xiang, WANG Jiangong, LI Fei, et al. Sedimentary characteristics of Eocene lacustrine microbialites in western Qaidam Basin:A case study from Xiaganchaigou Formation in Xichagou and Liangdong areas[J]. Lithologic Reservoirs, 2021, 33(3):63-73.
[22] BURNE R V, MOORE L S. Microbialites:Organosedimentary deposits of benthic microbial communities[J]. Palaios, 1987, 2 (3):241-254.
[23] 钟寿康, 李凌, 谭秀成, 等.鄂尔多斯盆地中东部马五段中粗晶白云岩成因及成岩演化[J].成都理工大学学报(自然科学版), 2020, 47(6):691-710. ZHONG Shoukang, LI Ling, TAN Xiucheng, et al. Study on the genesis and diagenesis of medium-coarse crystal dolomite of the member 5 of Majiagou Formation in the central-eastern Ordos Basin, China[J]. Journal of Chengdu University of Technology (Science & Technology Edition), 2020, 47(6):691-710.
[24] 魏千盛, 庞强, 江磊, 等.苏里格中区奥陶系喀斯特古地貌恢复及其在"大井丛、工厂化"模式中的应用[J].石油化工应用, 2017, 36(12):98-105. WEI Qiansheng, PANG Qiang, JIANG Lei, et al. Application of restoration of Ordovician karst palaeo geomorphology in the model of "dajing plexus, factory-like" in Sulige central section[J]. Petrochemical Industry Application, 2017, 36(12):98-105.
[25] 冯增昭, 鲍志东, 康祺发, 等.鄂尔多斯奥陶纪古构造[J].古地理学报, 1999, 1(3):83-94. FENG Zengzhao, BAO Zhidong, KANG Qifa, et al. Palaeotectonics of Ordovician in Ordos[J]. Journal of Palaeogeography, 1999, 1(3):83-94.
[26] 苏中堂, 佘伟, 罗静兰, 等.鄂尔多斯盆地奥陶系马五5亚段沉积微相与古地理演化[J].沉积学报, 2021, 39(6):1344-1356. SU Zhongtang, SHE Wei, LUO Jinglan, et al. Microfacies and Paleogeographic evolution of Ma 55 member in the Ordovician, Ordos Basin[J]. Acta Sedimentologica Sinica, 2021, 39(6):1344-1356.
[27] 杨华, 付金华, 魏新善, 等.鄂尔多斯盆地奥陶系海相碳酸盐岩天然气勘探领域[J].石油学报, 2011, 32(5):733-740. YANG Hua, FU Jinhua, WEI Xinshan, et al. Natural gas exploration domains in Ordovician marine carbonates, Ordos Basin[J]. Acta Petrolei Sinica, 2011, 32(5):733-740.
[28] 代金友, 何顺利.鄂尔多斯盆地中部气田奥陶系古地貌研究[J].石油学报, 2005, 26(3):37-39. DAI Jinyou, HE Shunli. Ordovician paleokarst landform of central gas field in Ordos Basin[J]. Acta Petrolei Sinica, 2005, 26(3):37-39.
[29] 孙玉景, 周立发.鄂尔多斯盆地马五段膏盐岩沉积对天然气成藏的影响[J].岩性油气藏, 2018, 30(6):67-75. SUN Yujing, ZHOU Lifa. Influences of gypsum-salt deposition on gas accumulation of the fifth member of Majiagou Formation in Ordos Basin[J]. Lithologic Reservoirs, 2018, 30(6):67-75.
[30] 张道锋, 姚泾利, 高星, 等.鄂尔多斯盆地奥陶系马五5亚段白云岩储层形成机理与展布规律[J].天然气地球科学, 2019, 30(1):74-82. ZHANG Daofeng, YAO Jingli, GAO Xing, et al. Formation mechanism and distribution regularity of Ordovician Ma 55 dolomite reservoir in Ordos Basin[J]. Natural Gas Geoscience, 2019, 30 (1):74-82.
[31] 张永生, 邢恩袁, 王卓卓, 等.鄂尔多斯盆地奥陶纪马家沟期岩相古地理演化与成钾意义[J].地质学报, 2015, 89(11):1921-1935. ZHANG Yongsheng, XING Enyuan, WANG Zhuozhuo, et al. Evolution of lithofacies paleogeography in the Ordos Basin and its implication of potash formation[J]. Acta Geologica Sinica, 2015, 89(11):1921-1935.
[32] RAABEN M E, SINBAA K, SHARMA M. Precambrian stromatolites of India and Russia[M]. Lucknow:Birbal Sahni Institute of Palaeobotany, 2001:1-4.
[33] 韩晓涛, 鲍征宇, 谢淑云.四川盆地西南中二叠统白云岩的地球化学特征及其成因[J].地球科学, 2016, 41(1):167-176. HAN Xiaotao, BAO Zhengyu, XIE Shuyun. Origin and geochemical characteristics of dolomites in the Middle Permian Formation, SW Sichuan Basin, China[J]. Earth Science, 2016, 41(1):167-176.
[34] 贺训云, 寿建峰, 沈安江, 等.白云岩地球化学特征及成因:以鄂尔多斯盆地靖西马五段中组合为例[J].石油勘探与开发, 2014, 41(3):375-384. HE Xunyun, SHOU Jianfeng, SHEN Anjiang, et al. Geochemical characteristics and origin of dolomite:A case study from the middle assemblage of Majiagou Formation member 5 of the west of Jingbian gas field, Ordos Basin, North China[J]. Petroleum Exploration and Development, 2014, 41(3):375-384.
[35] 由雪莲, 孙枢, 朱井泉, 等.微生物白云岩模式研究进展[J].地学前缘, 2011, 18(4):52-64. YOU Xuelian, SUN Shu, ZHU Jingquan, et al. Progress in the study of microbial dolomite model[J]. Earth Science Frontiers, 2011, 18(4):52-64.
[36] FOLK R L. SEM imaging of bacteria and nanobacteria in carbonate sediments and rocks[J]. Journal of Sedimentary Research, 1993, 63(5):990-999.
[37] BONTOGNALI T R, VASCONCELOS R, WARTHMANN R J, et al. Microbes produce nanobacteria-like structures, avoiding cell entombment[J]. Geology, 2008, 36(8):663-666.
[38] 朱士兴, 黄学光.13亿年前叠层石的生长节律和地-日-月动力学[J].微体古生物学报, 2003, 20(1):23-30. ZHU Shixing, HUANG Xueguang. The earth-sun-moon dynamics form growth rhythms of 1 300 Ma stromatolites[J]. Acta Micropalaeontologica Sinica, 2003, 20(1):23-30.
[39] 蒋传杰, 杜孝华, 张浩, 等.苏里格气田东区下奥陶统马五5亚段白云岩成因[J].新疆石油地质, 2017, 38(1):41-48. JIANG Chuanjie, DU Xiaohua, ZHANG Hao, et al. Genesis of dolomite in the Lower Ordovician Ma-55 submember in eastern area of Sulige gas field[J]. Xinjiang Petroleum Geology, 2017, 38(1):41-48.
[40] 黄昊源, 田亚铭, 曾韬, 等.川南地区下奥陶统桐梓组白云岩特征及成因分析[J].矿物岩石, 2020, 40(2):92-103. HUANG Haoyuan, TIAN Yaming, ZENG Tao, et al. Characteristics and genesis of Lower Ordovician Tongzi Formation dolomite in southern Sichuan Basin[J]. Mineral and Petrology, 2020, 40(2):92-103.
[41] 杨雨然, 张亚, 谢忱, 等.川西北地区中二叠统栖霞组热液作用及其对储层的影响[J].岩性油气藏, 2019, 31(6):44-53. YANG Yuran, ZHANG Ya, XIE Chen, et al. Hydrothermal action of Middle Permian Qixia Formation in northwestern Sichuan Basin and its effect on reservoirs[J]. Lithologic Reservoirs, 2019, 31(6):44-53.
[42] 王振峰, 时志强, 张道军, 等.西沙群岛西科 1井中新统-上新统白云岩微观特征及成因[J].地球科学——中国地质大学学报, 2015, 40(4):633-644. WANG Zhenfeng, SHI Zhiqiang, ZHANG Daojun, et al. Microscopic features and genesis for Miocene to Pliocene dolomite in well Xike-1, Xisha islands[J]. Earth Science-Journal of China University of Geosciences, 2015, 40(4):633-644.
[43] LOGAN B W, REZAK R, GINSBURG R N. Classification and environmental significance of algal stromatolites[J]. The Journal of Geology, 1964, 72(1):68-83.
[44] 钱迈平, 袁训来, 徐学思, 等.徐淮地区新元古代叠层石组合[J].古生物学报, 2002, 41(3):403-418. QIAN Maiping, YUAN Xunlai, XU Xuesi, et al. An assemblage of the Neoproterozoic stromatolite from the Xuzhou-Huaian region[J]. Acta Palaeontologica Sinica, 2002, 41(3):403-418.
[45] 温志峰, 钟建华, 刘云田, 等.柴达木盆地中新世叠层石沉积特征及其环境和构造意义[J].地质科学, 2005, 40(4):99-109. WEN Zhifeng, ZHONG Jianhua, LIU Yuntian, et al. Sedimentary features and tectono-environmental significance of the Miocene stromatolite in western Qaidam Basin[J]. Chinese Journal of Geology, 2005, 40(4):99-109.
[46] 曹瑞骥, 袁训来.中国叠层石研究进展[J].古生物学报, 2009, 48(3):314-321. CAO Ruiji, YUAN Xunlai. Advances of stromatolite study in China[J]. Acta Palaeontologica Sinica, 2009, 48(3):314-321.
[47] 常玉光, 齐永安, 郑伟, 等.中国豫西寒武系馒头组叠层石的沉积特征及其古环境意义[J].沉积学报, 2013, 31(1):10-19. CHANG Yuguang, QI Yong'an, ZHENG Wei, et al. Sedimentary characteristics and palaeoenvironmental significance on stromatolites of Mantou Formation in Cambrian, western Henan, China[J]. Acta Sedimentologica Sinica, 2013, 31(1):10-19.
[48] 张伟.贵州瓮安灯影组叠层石磷块岩特征及形成机制研究[D].贵州:贵州大学, 2016. ZHANG Wei. Sedimentary character and metallogenic mechanism of stromatolitic phosphorite of Dengying Formation, Weng'an county of Guizhou province, China[D]. Guizhou:Guizhou University, 2016.
[49] 曹瑞骥, 袁训来.叠层石[M].合肥:中国科学技术大学出版社, 2006. CAO Ruiji, YUAN Xunlai. Stromatolites[M]. Hefei:Press of China University of Science and Technology, 2006.
[50] 周丽清, 邵德艳, 林承焰, 等.中上元古界柱状叠层石生长过程浅析[J].石油大学学报(自然科学版), 1993, 17(2):121-125. ZHOU Liqing, SHAO Deyan, LIN Chengyan, et al. Analysis of the growing process of Middle and Upper Proterozoic columnar stromatolites[J]. Journal of China University of Petroleum(Edition of Natural Sciences), 1993, 17(2):121-125.
[51] 肖传桃, 吴彭珊, 李沫汝, 等.湖北松滋地区下奥陶统叠层石沉积特征[J].沉积学报, 2018, 36(5):853-863. XIAO Chuantao, WU Pengshan, LI Moru, et al. Sedimentary characteristics of Lower Ordovician stromatolites in Songzi area, Hubei province[J]. Acta Sedimentologica Sinica, 2018, 36(5):853-863.
[52] 乔丹, 时国, 任玥, 等.浙江江山地区震旦系灯影组叠层石特征及沉积环境分析[J].地球科学与环境学报, 2019, 41(6):734-747. QIAO Dan, SHI Guo, REN Yue, et al. Stromatolite characteristics and sedimentary environment analysis of Sinian Dengying Formation in Jiangshan area of Zhejiang, China[J]. Journal of Earth Sciences and Environment, 2019, 41(6):734-747.
[53] 李增学, 常象春, 赵秀丽.岩相古地理学[M].北京:地质出版社, 2010:45-46. LI Zengxue, CHANG Xiangchun, ZHAO Xiuli. Lithofacies and Paleogeography[M]. Beijing:Geological Publishing House, 2010:45-46.
[54] 朱莲芳, 马宝林.塔里木盆地阿克苏-柯坪地区寒武系-奥陶系的沉积环境[J].沉积学报, 1991, 9(2):55-62. ZHU Lianfang, MA Baolin. The sedimentary environment of Cambrian-Ordovician in the Aksu and Keping areas of Tarim Basin[J]. Acta Sedimentologica Sinica, 1991, 9(2):55-62.
[55] FELDMANN M. MCKENZIC J A. Stromatolite-thrombolite associations in a modern environment, Lee Stocking Island, Bahamas[J]. Palaios, 1998, 13(2):201-212.
[56] 唐鑫萍, 黄文辉, 邓宏文, 等.山东平邑盆地古近系湖相微生物碳酸盐岩形成机理[J].古地理学报, 2012, 14(3):355-364. TANG Xinping, HUANG Wenhui, DENG Hongwen, et al. Formation mechanisms of the Paleogene lacustrine microbial carbonate rocks in Pingyi Basin, Shandong province[J]. Journal of Palaeogeography, 2012, 14(3):355-364.
[57] 翟秀芬, 汪泽成, 罗平, 等.四川盆地高石梯东部地区震旦系灯影组微生物白云岩储层特征及成因[J].天然气地球科学, 2017, 28(8):1199-1210. ZHAI Xiufen, WANG Zecheng, LUO Ping, et al. Characteristics and origin of microbial dolomite reservoirs in Upper Sinian Deingying Formation, eastern Gaoshiti area, Sichuan Basin, SW China[J]. Natural Gas Geoscience, 2017, 28(8):1199-1210.
[1] 关蕴文, 苏思羽, 蒲仁海, 王启超, 闫肃杰, 张仲培, 陈硕, 梁东歌. 鄂尔多斯盆地南部旬宜地区古生界天然气成藏条件及主控因素[J]. 岩性油气藏, 2024, 36(6): 77-88.
[2] 周刚, 杨岱林, 孙奕婷, 严威, 张亚, 文华国, 和源, 刘四兵. 四川盆地及周缘寒武系沧浪铺组沉积充填过程及油气地质意义[J]. 岩性油气藏, 2024, 36(5): 25-34.
[3] 王子昕, 柳广弟, 袁光杰, 杨恒林, 付利, 王元, 陈刚, 张恒. 鄂尔多斯盆地庆城地区三叠系长7段烃源岩特征及控藏作用[J]. 岩性油气藏, 2024, 36(5): 133-144.
[4] 尹虎, 屈红军, 孙晓晗, 杨博, 张磊岗, 朱荣幸. 鄂尔多斯盆地东南部三叠系长7油层组深水沉积特征及演化规律[J]. 岩性油气藏, 2024, 36(5): 145-155.
[5] 牟蜚声, 尹相东, 胡琮, 张海峰, 陈世加, 代林锋, 陆奕帆. 鄂尔多斯盆地陕北地区三叠系长7段致密油分布特征及控制因素[J]. 岩性油气藏, 2024, 36(4): 71-84.
[6] 段逸飞, 赵卫卫, 杨天祥, 李富康, 李慧, 王嘉楠, 刘钰晨. 鄂尔多斯盆地延安地区二叠系山西组页岩气源储特征及聚集规律[J]. 岩性油气藏, 2024, 36(3): 72-83.
[7] 程静, 闫建平, 宋东江, 廖茂杰, 郭伟, 丁明海, 罗光东, 刘延梅. 川南长宁地区奥陶系五峰组—志留系龙马溪组页岩气储层低电阻率响应特征及主控因素[J]. 岩性油气藏, 2024, 36(3): 31-39.
[8] 王宏波, 张雷, 曹茜, 张建伍, 潘星. 鄂尔多斯盆地二叠系盒8段河流扇沉积模式及勘探意义[J]. 岩性油气藏, 2024, 36(3): 117-126.
[9] 曹江骏, 王茜, 王刘伟, 李诚, 石坚, 陈朝兵. 鄂尔多斯盆地合水地区三叠系长7段夹层型页岩油储层特征及主控因素[J]. 岩性油气藏, 2024, 36(3): 158-171.
[10] 李启晖, 任大忠, 甯波, 孙振, 李天, 万慈眩, 杨甫, 张世铭. 鄂尔多斯盆地神木地区侏罗系延安组煤层微观孔隙结构特征[J]. 岩性油气藏, 2024, 36(2): 76-88.
[11] 陈叔阳, 何云峰, 王立鑫, 尚浩杰, 杨昕睿, 尹艳树. 塔里木盆地顺北1号断裂带奥陶系碳酸盐岩储层结构表征及三维地质建模[J]. 岩性油气藏, 2024, 36(2): 124-135.
[12] 雷涛, 莫松宇, 李晓慧, 姜楠, 朱朝彬, 王桥, 瞿雪姣, 王佳. 鄂尔多斯盆地大牛地气田二叠系山西组砂体叠置模式及油气开发意义[J]. 岩性油气藏, 2024, 36(2): 147-159.
[13] 翟咏荷, 何登发, 开百泽. 鄂尔多斯盆地及邻区中—晚二叠世构造-沉积环境与原型盆地演化[J]. 岩性油气藏, 2024, 36(1): 32-44.
[14] 龙盛芳, 侯云超, 杨超, 郭懿萱, 张杰, 曾亚丽, 高楠, 李尚洪. 鄂尔多斯盆地西南部庆城地区三叠系长7段—长3段层序地层特征及演化规律[J]. 岩性油气藏, 2024, 36(1): 145-156.
[15] 杜江民, 崔子豪, 贾志伟, 张毅, 聂万才, 龙鹏宇, 刘泊远. 鄂尔多斯盆地苏里格地区奥陶系马家沟组马五5亚段沉积特征[J]. 岩性油气藏, 2023, 35(5): 37-48.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
[1] 杨占龙, 张正刚, 陈启林, 郭精义,沙雪梅, 刘文粟. 利用地震信息评价陆相盆地岩性圈闭的关键点分析[J]. 岩性油气藏, 2007, 19(4): 57 -63 .
[2] 方朝合, 王义凤, 郑德温, 葛稚新. 苏北盆地溱潼凹陷古近系烃源岩显微组分分析[J]. 岩性油气藏, 2007, 19(4): 87 -90 .
[3] 林承焰, 谭丽娟, 于翠玲. 论油气分布的不均一性(Ⅰ)———非均质控油理论的由来[J]. 岩性油气藏, 2007, 19(2): 16 -21 .
[4] 王天琦, 王建功, 梁苏娟, 沙雪梅. 松辽盆地徐家围子地区葡萄花油层精细勘探[J]. 岩性油气藏, 2007, 19(2): 22 -27 .
[5] 王西文,石兰亭,雍学善,杨午阳. 地震波阻抗反演方法研究[J]. 岩性油气藏, 2007, 19(3): 80 -88 .
[6] 何宗斌,倪　静,伍　东,李　勇,刘丽琼,台怀忠. 根据双TE 测井确定含烃饱和度[J]. 岩性油气藏, 2007, 19(3): 89 -92 .
[7] 袁胜学,王　江. 吐哈盆地鄯勒地区浅层气层识别方法研究[J]. 岩性油气藏, 2007, 19(3): 111 -113 .
[8] 陈斐，魏登峰，余小雷，吴少波. 鄂尔多斯盆地盐定地区三叠系延长组长2 油层组沉积相研究[J]. 岩性油气藏, 2010, 22(1): 43 -47 .
[9] 徐云霞，王山山，杨帅. 利用沃尔什变换提高地震资料信噪比[J]. 岩性油气藏, 2009, 21(3): 98 -100 .
[10] 李建明，史玲玲，汪立群，吴光大. 柴西南地区昆北断阶带基岩油藏储层特征分析[J]. 岩性油气藏, 2011, 23(2): 20 -23 .

陇ICP备17006252号
版权所有© 2018 中国石油集团西北地质研究所有限公司《岩性油气藏》编辑部

地址：甘肃省兰州市城关区雁儿湾路535号(陇ICP备17006252号)    电话：0931-8686158;8686058;8686288    邮箱：yxyqc@petrochina.com.cn

甘公网安备 62010202002827号

本系统由北京玛格泰克科技发展有限公司设计开发