黔东南地区寒武系碳酸盐岩成岩作用分析

邓长瑜; 张秀莲; 陈建文; 王贤

黔东南地区寒武系碳酸盐岩成岩作用分析

1.
北京大学地质系北京 100871;
2.
大庆油田公司第二采油厂黑龙江大庆 163459;
3.
新疆油田公司勘探开发研究院乌鲁木齐 830011

基金项目: 国家自然科学基金项目(批准号:40172046)资助.

详细信息

作者简介:
邓长瑜女 1972年出生硕士岩石学、矿物学及矿床学

中图分类号: P588.24⁺5

计量

文章访问数: 654
HTML全文浏览量: 3
PDF下载量: 881
被引次数: 0

The Analysis of Sequence Stratigraphy and Diagenesis for the Carbonates of Cambrian in the Southeast of Guizhou Province

1.
Department of Geology, Peking University, Beijing100871;
2.
The Second Oil Extraction Factory, Daqing Petroleum Company,Daqing Heilongjiang 163459;
3.
The Exploration and Development Institute of Xinjiang Petroleum Company, Wulumuqi 830011

摘要

摘要: 黔东南地区寒武系地层是典型的碳酸盐岩地层。分布广泛且有较好的储层。为了更好地了解该地层的岩性、孔隙状况等地质特征,以贵州东部三都—丹寨剖面寒武系地层为例,分析了各组段的岩石学特征,确定了其沉积环境,在此基础上对形成现有岩石孔隙等特征的相应的成岩作用进行了分析。指出白云化作用是该区的主要成岩作用,主要表现在中寒武统都柳江组—在准同生白云化作用下形成大套厚层的白云岩。埋藏溶解作用形成的次生溶孔是该区中上寒武统的典型特征,有利于改善碳酸盐岩的储层物性。重结晶作用、压溶作用等对储层孔隙的形成也起到重要作用,并列出了黔东南地区寒武系地层各层组的成岩演化史。
- 黔东南 /
- 寒武系 /
- 碳酸盐岩 /
- 体系域 /
- 滑塌 /
- 白云化 /
- 溶孔
Abstract: The Cambrian in the southeast of Qian is composed of typical carbonate rocks, which are widespread and better reservoirs. In order to understand the lithology, porosity and so on, in this paper, we took the Cambian in Sandu Danzhai to analyze petrographic feature in each layer and concluded the diagenetic environment of every formation of the Carbonate. Based on these study, we obtain the corresponding diagenesis which is responsible for producing the porosity of the rock, point out dolomitization is the main diagenesis in Duliujiang Formation of the mid Cambrian froming the larger and thicker carbonate rock, and dissolution pores produced by the burial dissolution is typical characters of the mid and upper Cambrian in the study area, burial dissolution is favorable for improving the reservoir physical properties. Recrystallization and compaction dissolution have also positive effect in producing porosity within the reservoir. This paper shows clearly the diagenetic evolution history of each formation within the Cambrian in the southeast of Guizhou province.
- the south-east of Guizhou province /
- Cambrian /
- carbonate rock /
- system tract /
- slump /
- dolomitization /
- solution pore

HTML全文

参考文献(17)

[1]	杨惠民,等. 滇黔桂海相碳酸盐地区最佳油气保存单元的评价与选择. 贵阳:贵州科技出版社,1999.163～177[Yang Huimin, et al. The Evaluation and Choice of the Best Oil and Gas Reserve Unit in Dian Qian Gui Marine Carbonate Rocks Area. Guiyang: Guizhou Science and Technology Press, 1999.163～177]
[2]	张秀莲. 论斜坡相碳酸盐岩的含油气性. 见:李茂松. 北京大学国际地质科技学术研讨会论文集. 北京: 地震出版社,1988.684～692[ Zhang Xiulian. The Discussion of Petroliferous Characteristics for Carbonate Rocks of Slope Facies In:Li Maosong. The Thesis Collection of International Geology Science and Technology Academic Symposium in Peking University. Beijing:Earthquake Press, 1988.684～692]
[3]	张秀莲. 碳酸盐岩中氧、碳稳定同位素与古盐度、古水温的关系.沉积学报, 1985, 3(4) : 17～28[Zhang Xiulian. Relationship between carbon and oxygen stable isotope in carbonate rocks and paleosalinity and paleotemperature of seawater. Acta Sedimentologica Sinica,1985,3(4):17～28]
[4]	王英华, 黄志诚, 王国忠, 梁百和. 中、下扬子区海相碳酸盐岩成岩作用研究. 北京: 科学技术文献出版社,1991.4～11 [Wang Yinghua, Huang Zhicheng, Wang Guozhong, Liang Baihe. The Study of Diageneses of Marine Carbonate Rocks in the Lower-Middle Yangtze Region. Beijing:Science Technology Reference Press, 1991.4～11]
[5]	张秀莲,于德龙,王贤.湖北宜昌地区寒武系碳酸盐岩岩石学特征及沉积环境. 古地理学报, 2003, 5(2):152～161[Zhang Xiulian, Yu Delong, Wang Xian. The petrographic characteristics and sedimentary environments of carbonate rocks of the Cambrian in Yichang area, Hubei Province. Journal of Palaeogeography, 2003,5(2):152～161]
[6]	王英华, 张秀莲, 杨承运. 华北地区早古生代碳酸盐岩岩石学. 北京: 地震出版社,1988.73～101 [Wang Yinghua, Zhang Xiulian, Yang Chengyun. The Petrographic of Carbonate Rocks of earlier Palaeozoic in Hua Bei Area. Beijing: Earthquake Press, 1988.73～101]
[7]	Zhang Xiulian. Types and spatio-temporal distribution of the shoal facies in the lower middle Yangtze area,China. Scientia Geologica Sinica 2000,9,71～79
[8]	Zhang Xiulian, Jiang Lingzhi. Diagenesis and reservoir characteristics of shoal facies in the Middle and Lower Yangtze Area. Scientia Geologica Sinica.2000,9: 295～302
[9]	Zhang Xiulian, Jiang Lingzhi. Research on diagenesis of Cambrian shoal facies carbonate rocks in the Xidong Area, Hubei Province. Acta Geologica Sinica, 2001,75:161～174
[10]	翟永红,郭建华,刘生国.塔中地区石炭系碳酸盐岩成岩作用与储层评价. 江汉石油学院学报,1995, 17(3):13～18 [Zhai Yonghong, Guo Jianhua, Liu Shengguo.Diagenesis and reservoir evaluation of Carboniferous carbonate reservoirs in Tazhong area. Journal of Jianghan Petroleum Institute, 1995,17(3):13～18]
[11]	杜森官.中国南方东部震旦系碳酸盐岩成岩作用. 安徽地质,1997, 7(2):2～6[Du Senguan. The character of diagenesis of the Sinian carbonate rock in the eastern part of south China. Anhui Geology, 1997,7(2):2～6]
[12]	胡明毅,高振中,李建明. 中上扬子区古生界深水斜坡及台地边缘碳酸盐岩成岩作用. 石油实验地质, 1998,20(3):241～247[Hu Mingyi, Gao Zhenzhong, Li Jianming.Diagenesis of carbonate rocks on platform margin and deep water slope in the Upper Sinian-Ordovician in the middle to upper Yangtze area. Experimental Petroleum Geology, 1998,20(3):239～247]
[13]	翟永红,郭成贤. 中扬子台地北缘灯影组碳酸盐岩成岩作用序列及成岩模式. 地质地球化学,1997, 2(2):45～52[Zhai Yonghong, Guo Chengxian. The carbonate diagenetic model and sequence of the Dengkying Formation (Upper Sinian) on the northern margin of the middle Yangtze Platform. Geology-Geochemistry, 1997, 2(2):45～52]
[14]	胡恒,陈景山. 塔北地区下奥陶统碳酸盐岩成岩作用及孔隙演化. 成都理工学院学报(增刊), 1996,23:104～110[Hu Heng, Chen Jingshan.Diagenesis of the Lower Ordovician carbonate in the North of Tarim Basin. Journal of Chengdu Institute of Technology, 1996,23:104～110]
[15]	Zhang Xiulian, Wang Yinghua, Chen Xiaolong. Diagenesis and porosity of the Cambrian-Ordovician carbonate shoal facies at Yangjiaping, Shimen, Hunan. Acta Geologica Sinica, 2000,74: 29～45
[16]	朱梅湘,张秀莲,王英华. 中下扬子区三叠纪海相碳酸盐岩成岩作用和成岩环境. 古地理学报,2000,2(4):43～50[ Zhu Meixiang, Zhang Xiulian, Wang Yinghua. The diageneses and diagenetic environments of marine carbonate rocks of the Triassic in the Lower-Middle Yangtze region. Journal of Palaeogeography, 2000,2(4):43～50]
[17]	张秀莲.碳酸盐岩成岩研究的新方法:成岩综合柱状图. 地质科学,1995, 30(4):402～413[Zhang Xiulian. A new method in the study of carbonate diagenesis-Composite column of diagenesis. Scientia Geologica Sinica,1995,30(4):402～413]

[1]	刘媛媛, 王子晨, 明鑫雨, 姜磊. 震旦系—下寒武统白云岩优势成岩—成储效应深层白云岩成因及差异成储 . 沉积学报, 2024, 42(6): 2159-2173. doi: 10.14027/j.issn.1000-0550.2023.041
[2]	陈吉涛. 再论华北寒武系竹叶状灰岩丘成因 . 沉积学报, 2023, 41(6): 1662-1672. doi: 10.14027/j.issn.1000-0550.2023.071
[3]	樊爱萍, 李诚, 杨仁超, 韩作振, 吴祥生. 岩相特征对海平面升降的响应 . 沉积学报, 2023, 41(4): 1040-1053. doi: 10.14027/j.issn.1000-0550.2022.060
[4]	辛浩, 肖恩照, 王龙, 李屹尧, 张震武. 肥城邓家庄剖面寒武系微生物碳酸盐岩沉积序列 . 沉积学报, 2020, 38(1): 64-75. doi: 10.14027/j.issn.1000-0550.2019.071
[5]	刘梦瑶, 齐永安, 史云鹤, 高星, 苏中堂, 张立军. 华北寒武纪—奥陶纪豹皮状碳酸盐岩系生物扰动成因 . 沉积学报, 2020, 38(1): 91-103. doi: 10.14027/j.issn.1000-0550.2019.042
[6]	余晶洁, 宋金民, 刘树根, 杨迪, 王瀚, 赵聪, 邓双林, 何宇, 李立基. 川东北地区下寒武统龙王庙组白云岩成因分析 . 沉积学报, 2020, 38(6): 1284-1295. doi: 10.14027/j.issn.1000-0550.2019.108
[7]	李峰峰, 郭睿, 刘立峰, 余义常, 宋世琦. 伊拉克M油田白垩系Mishrif组层序构型及储层展布 . 沉积学报, 2020, 38(4): 838-850. doi: 10.14027/j.issn.1000-0550.2019.078
[8]	袁静, 钟剑辉, 宋明水, 张宇, 向奎, 赵永福, 俞国鼎, 李欣尧. 沾化凹陷孤岛西部斜坡带沙三段重力流沉积特征与源-汇体系 . 沉积学报, 2018, 36(3): 542-556. doi: 10.14027/j.issn.1000-0550.2018.076
[9]	付超, 于兴河, 金丽娜, 董亦思, 单新, 何玉林. 琼东南盆地莺歌海组重力流沉积演化过程 . 沉积学报, 2017, 35(3): 552-560. doi: 10.14027/j.cnki.cjxb.2017.03.013
[10]	贾连奇, 蔡春芳, 李红霞, 汪天凯, 张文, 孔令武. 塔中地区热化学硫酸盐还原作用对深埋白云岩储层的改造 . 沉积学报, 2016, 34(6): 1057-1067. doi: 10.14027/j.cnki.cjxb.2016.06.005
[11]	王鹏万, 斯春松, 张润合, 李娴静, 马立桥, 黄羚, 徐云俊, 鲁慧丽. 滇黔北坳陷寒武系碳酸盐岩古海洋环境特征及地质意义 . 沉积学报, 2016, 34(5): 811-818. doi: 10.14027/j.cnki.cjxb.2016.05.001
[12]	樊爱萍, 杨仁超, 韩作振, 崔明明, 蔡娜. 鲁西地区张夏组碳酸盐岩成岩系统 . 沉积学报, 2015, 33(1): 67-78. doi: 10.14027/j.cnki.cjxb.2015.01.007
[13]	. 塔里木盆地寒武系鞍状白云石孔隙充填物差异与成因 . 沉积学报, 2014, 32(2): 253-259.
[14]	. 湘鄂西寒武系烃源岩地球化学特征与沉积环境分析 . 沉积学报, 2013, 31(6): 1122-1132.
[15]	郭建军. 塔里木盆地寒武系烃源岩的研究新进展 . 沉积学报, 2008, 26(3): 518-524.
[16]	陈景山. 塔里木盆地奥陶系碳酸盐岩古岩溶作用与储层分布 . 沉积学报, 2007, 25(6): 858-868.
[17]	李双应, 岳书仓. 安徽巢湖二叠系栖霞组碳酸盐岩斜坡沉积 . 沉积学报, 2002, 20(1): 7-12.
[18]	陈发亮, 朱晖, 李绪涛, 苗翠芝. 东濮凹陷下第三系沙河街组层序地层划分及盐岩成因探讨 . 沉积学报, 2000, 18(3): 384-388,394.
[19]	赖健清, 易诗军, 杨楚雄, 丁传谱. 广东凡口地区泥盆系碳酸盐岩化学成岩作用 . 沉积学报, 1997, 15(4): 143-147.
[20]	叶德胜. 塔里木盆地北部寒武──奥陶系碳酸盐岩的深部溶蚀作用 . 沉积学报, 1994, 12(1): 66-71.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 654
HTML全文浏览量: 3
PDF下载量: 881
被引次数: 0

姓名
邮箱
手机号码
标题
留言内容
验证码

留言板

黔东南地区寒武系碳酸盐岩成岩作用分析

作者简介:
邓长瑜女 1972年出生硕士岩石学、矿物学及矿床学

计量

The Analysis of Sequence Stratigraphy and Diagenesis for the Carbonates of Cambrian in the Southeast of Guizhou Province

计量

目录

黔东南地区寒武系碳酸盐岩成岩作用分析

1. 北京大学地质系北京 100871;

2. 大庆油田公司第二采油厂黑龙江大庆 163459;

3. 新疆油田公司勘探开发研究院乌鲁木齐 830011

作者简介:
邓长瑜女 1972年出生硕士岩石学、矿物学及矿床学

English Abstract

The Analysis of Sequence Stratigraphy and Diagenesis for the Carbonates of Cambrian in the Southeast of Guizhou Province

1. Department of Geology, Peking University, Beijing100871;

2. The Second Oil Extraction Factory, Daqing Petroleum Company,Daqing Heilongjiang 163459;

3. The Exploration and Development Institute of Xinjiang Petroleum Company, Wulumuqi 830011

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

黔东南地区寒武系碳酸盐岩成岩作用分析

作者简介: 邓长瑜 女 1972年出生 硕士 岩石学、矿物学及矿床学

计量

出版历程

The Analysis of Sequence Stratigraphy and Diagenesis for the Carbonates of Cambrian in the Southeast of Guizhou Province

计量

出版历程

目录

黔东南地区寒武系碳酸盐岩成岩作用分析

1. 北京大学地质系 北京 100871; 2. 大庆油田公司第二采油厂 黑龙江大庆 163459; 3. 新疆油田公司勘探开发研究院 乌鲁木齐 830011

作者简介: 邓长瑜 女 1972年出生 硕士 岩石学、矿物学及矿床学

English Abstract

The Analysis of Sequence Stratigraphy and Diagenesis for the Carbonates of Cambrian in the Southeast of Guizhou Province

1. Department of Geology, Peking University, Beijing100871; 2. The Second Oil Extraction Factory, Daqing Petroleum Company,Daqing Heilongjiang 163459; 3. The Exploration and Development Institute of Xinjiang Petroleum Company, Wulumuqi 830011

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
邓长瑜女 1972年出生硕士岩石学、矿物学及矿床学

1. 北京大学地质系北京 100871;

2. 大庆油田公司第二采油厂黑龙江大庆 163459;

3. 新疆油田公司勘探开发研究院乌鲁木齐 830011

作者简介:
邓长瑜女 1972年出生硕士岩石学、矿物学及矿床学

1. Department of Geology, Peking University, Beijing100871;

2. The Second Oil Extraction Factory, Daqing Petroleum Company,Daqing Heilongjiang 163459;

3. The Exploration and Development Institute of Xinjiang Petroleum Company, Wulumuqi 830011