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:2022-04-01 发布日期:2022-03-14
  • 通讯作者: 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。 E-mail:suzhongtang2012@cdut.edu.cn
  • 作者简介: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。
  • 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:2022-04-01 Published:2022-03-14

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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
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