靖边气田马五1-4亚段沉积微相和成岩作用研究

雷卞军

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靖边气田马五1-4亚段沉积微相和成岩作用研究

雷卞军

文章导航 > 沉积学报 > 2010 > 28(6): 1153-1164

雷卞军. 靖边气田马五1-4亚段沉积微相和成岩作用研究[J]. 沉积学报, 2010, 28(6): 1153-1164.

引用本文:

雷卞军. 靖边气田马五1-4亚段沉积微相和成岩作用研究[J]. 沉积学报, 2010, 28(6): 1153-1164.

LEI Bianjun. Research on the Sedimentary Microfacies and Diageneses of Ma5 1-4 Submember in Jingbian Gas Field[J]. Acta Sedimentologica Sinica, 2010, 28(6): 1153-1164.

Citation:

LEI Bianjun. Research on the Sedimentary Microfacies and Diageneses of Ma5 1-4 Submember in Jingbian Gas Field[J]. Acta Sedimentologica Sinica, 2010, 28(6): 1153-1164.

雷卞军. 靖边气田马五1-4亚段沉积微相和成岩作用研究[J]. 沉积学报, 2010, 28(6): 1153-1164.

引用本文:

雷卞军. 靖边气田马五1-4亚段沉积微相和成岩作用研究[J]. 沉积学报, 2010, 28(6): 1153-1164.

LEI Bianjun. Research on the Sedimentary Microfacies and Diageneses of Ma5 1-4 Submember in Jingbian Gas Field[J]. Acta Sedimentologica Sinica, 2010, 28(6): 1153-1164.

Citation:

LEI Bianjun. Research on the Sedimentary Microfacies and Diageneses of Ma5 1-4 Submember in Jingbian Gas Field[J]. Acta Sedimentologica Sinica, 2010, 28(6): 1153-1164.

靖边气田马五1-4亚段沉积微相和成岩作用研究

雷卞军

1.
西南石油大学成都 610050; 2.长庆油田分公司勘探开发研究院西安710021

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雷卞军

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Research on the Sedimentary Microfacies and Diageneses of Ma5 1-4 Submember in Jingbian Gas Field

LEI Bianjun

1.
Southwest Petroleum University, Chengdu 610500

More Information

Corresponding author: LEI Bianjun

摘要

摘要: 鄂尔多斯盆地靖边气田马五1~4亚段属于陆表海蒸发碳酸盐潮坪相。潮上带（含）石膏结核白云岩和潮间带上部的含石膏晶模白云岩最有利于形成储层。马五1－4亚段碳酸盐岩经历了复杂的成岩作用，准同生期白云石化和膏化作用奠定了储层的物质基础；表生岩溶期选择性溶解作用构筑了储层的轮廓；埋藏期溶解作用和各种矿物充填作用，决定早期溶孔能否保存和储层最终状况。引入“负胶结物孔隙度”概念，更直观地反映了沉积作用对马五1－4亚段储层发育的控制作用。将沉积微相和成岩相研究有机地结合在一起,以简约的方式，用一套数字组合符号半定量地表达沉积微相和成岩相，在开发区块储层评价和预测上获得了良好效果。
- 靖边气田 /
- 马五1-4亚段 /
- 沉积微相 /
- 成岩作用
Abstract: Majiagou Formation of the middle part of Ordos Basin belong to epeiric sea carbonatites and evaporates. Majiagou Formation have Ma1 Ma6 Member(from bottom to top), Ma1, Ma3, Ma5 Members are micritefine powder dolomite, gyprock and saline. Ma2, Ma4, Ma6 Members are mainly micrite limestone or wackestone. Caledonian event uplift North China Platform since last stage of Middle Ordovician. The top of Majiagou Formation in Ordos Basin udergo weather worn in 1300 million endurance. Weathered crust dolomite reservoir of the top of Ma5 Member are produced by dissolution of ancient karst. Ma5 member divided into Ma510, Ma59…Ma51 from bottom to top. The producing pay allocation in Ma51－4〗submember which are top of weather crust. Ma514 submember have thick 80~110 m, are dolomite, argillaceous dolomite, minor gypseous dolomite andtuffaceous mudstone. The reservoir rock of Ma514 submember are mainly corrosion pore and hole dolomite, valid reservoir are grand total 2~10 m, which initial rock are gypseous micritefine powder dolomite. 
Ma 51－4 submember of Jinbian Gas Field in Ordos Basin belong to evaporated carbonate tidal flat facies,which divided into three subfacies: supratital zone, intertital zone,infratital zone, and 18 microfacies. The microfacies that are favour of developing reservoirs are supratidal zone dolomite which have anhydrite noddle and upper part intertidal zone dolomite which have anhydrite crystal. Ma514 Submember had undergone various diageneses. Penecontemporaneous dolomitization and gypsification that settled material base of reservoirs. Epidiagenesis selective dissolution of gypseous dolomite constructs the ambit of reservoirs. anhydrite noddle and crystal in dolomite selectively dissolved by meteoric fresh water and create pore and hole. Dissolved pore and hole what partly fill by one or some mineral form reservoirs. Early stage dissolution pore and hole are reconstructed by burial period dissolution, fill mineral sort and amount that determine the preservation condition of dissolution pore and the feature of reservoirs. 
Call in “minus cement porosity”, it directly reflects sedimentary that control reservoir Ma514 Submember. Combining of research microfacies and diagenesis facies, use concise numerical symbol that express semiquantitatively sedimentary microfacies and diagenesis facies. Used that in compilation microfacies chart and diagenesis partition chart, beneficial area for reservoir is so clearly. That method acquire approved effect on the evaluation and forecasing reservoir of Jingbian Gas Field.
- Jingbian Gas Field /
- Ma51-4 submember /
- sedimentary microfacies /
- diagenesis

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[1]	朱柏宇, 印森林, 郭海平, 唐攀, 赵俊威, 陈旭, 雷章树. 陆相混合细粒岩沉积微相及其对甜点的控制作用 . 沉积学报, 2024, 42(3): 839-856. doi: 10.14027/j.issn.1000-0550.2023.051
[2]	熊连桥, 李建平, 谢晓军, 蔡露露, 廖计华, 许晓明. 湖相碳酸盐岩沉积微相类型及沉积模式 . 沉积学报, 2021, 39(3): 767-780. doi: 10.14027/j.issn.1000-0550.2020.025
[3]	王乾右, 杨威, 葛云锦, 宋岩, 姜振学, 罗群, 左如斯, 李耀华, 刘聃, 张帆, 王耀华, 鲁健康. 不同沉积微相致密储层的成岩响应及其控储机理 . 沉积学报, 2021, 39(4): 841-862. doi: 10.14027/j.issn.1000-0550.2020.112
[4]	李泯星, 屈海洲, 程曦, 杨迅, 杨东凡, 张本健, 张云峰, 李晓. 火山作用对碳酸盐岩沉积及成岩的影响 . 沉积学报, 2020, 38(4): 810-825. doi: 10.14027/j.issn.1000-0550.2019.098
[5]	伊硕, 黄文辉, 金振奎, 高白水. 滨里海盆地东缘石炭系KT-II层碳酸盐岩微相特征与沉积环境研究——以扎纳若尔地区为例 . 沉积学报, 2017, 35(1): 139-150. doi: 10.14027/j.cnki.cjxb.2017.01.014
[6]	郑庆华, 柳益群. 鄂尔多斯盆地镇北地区延长组长4+5致密油层成岩作用及成岩相 . 沉积学报, 2015, 33(5): 1000-1012. doi: 10.14027/j.cnki.cjxb.2015.05.016
[7]	肖笛, 谭秀成, 山述娇, 彭浩, 陈虹宇, 万伟超, 熊鹰, 李顺. 四川盆地南部中二叠统茅口组二段沉积微相研究 . 沉积学报, 2015, 33(6): 1182-1191. doi: 10.14027/j.cnki.cjxb.2015.06.011
[8]	宋国奇, 刘鹏, 刘雅利. 渤南洼陷沙河街组四段下亚段成岩作用与储层孔隙演化 . 沉积学报, 2014, 32(5): 941-948.
[9]	. 准噶尔盆地乌尔禾油田高自然伽马砂砾岩特征及其沉积微相研究——以乌36井区百口泉组为例 . 沉积学报, 2014, 32(4): 734-743.
[10]	孟元林. 储层孔隙度预测与孔隙演化史模拟方法探讨——以辽河拗陷双清地区为例 . 沉积学报, 2008, 26(5): 780-788.
[11]	漆滨汶. 山东省牛庄洼陷古近系沙河街组沙三中亚段储集层成岩作用研究 . 沉积学报, 2007, 25(1): 99-109.
[12]	于兴河. 珠江口盆地番禺气田沉积特征与成岩演化研究 . 沉积学报, 2007, 25(6): 876-884.
[13]	孟元林. 渤海湾盆地西部凹陷南段成岩相分析与优质储层预测 . 沉积学报, 2006, 24(2): 185-192.
[14]	颜佳新, 伍明, 李方林, 方念乔. 湖北省巴东栖霞组沉积成岩作用地球化学特征研究 . 沉积学报, 1998, 16(4): 78-83.
[15]	赵永胜, 朱永铭, 杨世民, 王震, 车翔飞. 碎屑岩沉积微相工业制图方法及应用探讨——以辽河欢喜岭油田齐108块莲花油层为例 . 沉积学报, 1998, 16(2): 102-107.
[16]	于兴河, 郑浚茂, 宋立衡, 肖海燕, 张玉明. 构造、沉积与成岩综合一体化模式的建立——以松南梨树地区后五家户气田为例 . 沉积学报, 1997, 15(3): 8-13.
[17]	宋春晖, 武安斌. 西成矿田中泥盆统碳酸盐岩沉积微相、微相组及其环境分析 . 沉积学报, 1993, 11(2): 34-42.
[18]	何海清, 晋慧娟. 准噶尔盆地陆1井砂岩成岩作用及其对储层的影响 . 沉积学报, 1991, 9(4): 69-77.
[19]	高仁祥. 川南地区下三叠统碳酸盐岩的沉积成岩作用 . 沉积学报, 1991, 9(3): 50-58.
[20]	李元元, 方少仙, 陈景山. 自然伽玛数字判别法研究沉积微相——以东濮盆地文留地区沙四段为例 . 沉积学报, 1991, 9(4): 59-68.

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靖边气田马五1-4亚段沉积微相和成岩作用研究

雷卞军

1. 西南石油大学成都 610050; 2.长庆油田分公司勘探开发研究院西安710021

通讯作者: 雷卞军

收稿日期: 1900-01-01
修回日期: 1900-01-01
刊出日期: 2010-12-10

关键词:

摘要: 鄂尔多斯盆地靖边气田马五1~4亚段属于陆表海蒸发碳酸盐潮坪相。潮上带（含）石膏结核白云岩和潮间带上部的含石膏晶模白云岩最有利于形成储层。马五1－4亚段碳酸盐岩经历了复杂的成岩作用，准同生期白云石化和膏化作用奠定了储层的物质基础；表生岩溶期选择性溶解作用构筑了储层的轮廓；埋藏期溶解作用和各种矿物充填作用，决定早期溶孔能否保存和储层最终状况。引入“负胶结物孔隙度”概念，更直观地反映了沉积作用对马五1－4亚段储层发育的控制作用。将沉积微相和成岩相研究有机地结合在一起,以简约的方式，用一套数字组合符号半定量地表达沉积微相和成岩相，在开发区块储层评价和预测上获得了良好效果。

English Abstract

Research on the Sedimentary Microfacies and Diageneses of Ma5 1-4 Submember in Jingbian Gas Field

LEI Bianjun

1. Southwest Petroleum University, Chengdu 610500

Corresponding author: LEI Bianjun

Received Date: 1900-01-01
Rev Recd Date: 1900-01-01
Publish Date: 2010-12-10

Keywords:

Abstract: Majiagou Formation of the middle part of Ordos Basin belong to epeiric sea carbonatites and evaporates. Majiagou Formation have Ma1 Ma6 Member(from bottom to top), Ma1, Ma3, Ma5 Members are micritefine powder dolomite, gyprock and saline. Ma2, Ma4, Ma6 Members are mainly micrite limestone or wackestone. Caledonian event uplift North China Platform since last stage of Middle Ordovician. The top of Majiagou Formation in Ordos Basin udergo weather worn in 1300 million endurance. Weathered crust dolomite reservoir of the top of Ma5 Member are produced by dissolution of ancient karst. Ma5 member divided into Ma510, Ma59…Ma51 from bottom to top. The producing pay allocation in Ma51－4〗submember which are top of weather crust. Ma514 submember have thick 80~110 m, are dolomite, argillaceous dolomite, minor gypseous dolomite andtuffaceous mudstone. The reservoir rock of Ma514 submember are mainly corrosion pore and hole dolomite, valid reservoir are grand total 2~10 m, which initial rock are gypseous micritefine powder dolomite. 
Ma 51－4 submember of Jinbian Gas Field in Ordos Basin belong to evaporated carbonate tidal flat facies,which divided into three subfacies: supratital zone, intertital zone,infratital zone, and 18 microfacies. The microfacies that are favour of developing reservoirs are supratidal zone dolomite which have anhydrite noddle and upper part intertidal zone dolomite which have anhydrite crystal. Ma514 Submember had undergone various diageneses. Penecontemporaneous dolomitization and gypsification that settled material base of reservoirs. Epidiagenesis selective dissolution of gypseous dolomite constructs the ambit of reservoirs. anhydrite noddle and crystal in dolomite selectively dissolved by meteoric fresh water and create pore and hole. Dissolved pore and hole what partly fill by one or some mineral form reservoirs. Early stage dissolution pore and hole are reconstructed by burial period dissolution, fill mineral sort and amount that determine the preservation condition of dissolution pore and the feature of reservoirs. 
Call in “minus cement porosity”, it directly reflects sedimentary that control reservoir Ma514 Submember. Combining of research microfacies and diagenesis facies, use concise numerical symbol that express semiquantitatively sedimentary microfacies and diagenesis facies. Used that in compilation microfacies chart and diagenesis partition chart, beneficial area for reservoir is so clearly. That method acquire approved effect on the evaluation and forecasing reservoir of Jingbian Gas Field.

雷卞军. 靖边气田马五1-4亚段沉积微相和成岩作用研究[J]. 沉积学报, 2010, 28(6): 1153-1164.

引用本文:

雷卞军. 靖边气田马五1-4亚段沉积微相和成岩作用研究[J]. 沉积学报, 2010, 28(6): 1153-1164.

LEI Bianjun. Research on the Sedimentary Microfacies and Diageneses of Ma5 1-4 Submember in Jingbian Gas Field[J]. Acta Sedimentologica Sinica, 2010, 28(6): 1153-1164.

Citation:

LEI Bianjun. Research on the Sedimentary Microfacies and Diageneses of Ma5 1-4 Submember in Jingbian Gas Field[J]. Acta Sedimentologica Sinica, 2010, 28(6): 1153-1164.

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靖边气田马五1-4亚段沉积微相和成岩作用研究

通讯作者:
雷卞军

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Research on the Sedimentary Microfacies and Diageneses of Ma5 1-4 Submember in Jingbian Gas Field

Corresponding author: LEI Bianjun

计量

目录

靖边气田马五1-4亚段沉积微相和成岩作用研究

1. 西南石油大学成都 610050; 2.长庆油田分公司勘探开发研究院西安710021

通讯作者: 雷卞军

English Abstract

Research on the Sedimentary Microfacies and Diageneses of Ma5 1-4 Submember in Jingbian Gas Field

1. Southwest Petroleum University, Chengdu 610500

Corresponding author: LEI Bianjun

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靖边气田马五1-4亚段沉积微相和成岩作用研究

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Research on the Sedimentary Microfacies and Diageneses of Ma5 1-4 Submember in Jingbian Gas Field

Corresponding author: LEI Bianjun

计量

出版历程

目录

靖边气田马五1-4亚段沉积微相和成岩作用研究

1. 西南石油大学成都 610050; 2.长庆油田分公司勘探开发研究院西安710021

通讯作者: 雷卞军

English Abstract

Research on the Sedimentary Microfacies and Diageneses of Ma5 1-4 Submember in Jingbian Gas Field

1. Southwest Petroleum University, Chengdu 610500

Corresponding author: LEI Bianjun

全文HTML

目录

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期刊在线

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通讯作者:
雷卞军