苏盖特布拉克剖面肖尔布拉克组储层建模研究及其勘探意义

郑剑锋; 陈永权; 黄理力; 严威; 倪新锋; 李保华; 郭晓燕

doi:10.14027/j.issn.1000-0550.2018.142

ISSN 1000-0550 CN 62-1038/P

高级搜索

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

苏盖特布拉克剖面肖尔布拉克组储层建模研究及其勘探意义

郑剑锋, 陈永权, 黄理力, 严威, 倪新锋, 李保华, 郭晓燕

文章导航 > 沉积学报 > 2019 > 37(3): 601-609

郑剑锋, 陈永权, 黄理力, 严威, 倪新锋, 李保华, 郭晓燕. 苏盖特布拉克剖面肖尔布拉克组储层建模研究及其勘探意义[J]. 沉积学报, 2019, 37(3): 601-609. doi: 10.14027/j.issn.1000-0550.2018.142

引用本文:

ZHENG JianFeng, CHEN YongQuan, HUANG LiLi, YAN Wei, NI XinFeng, LI BaoHua, Guo XiaoYan. Reservoir Modeling of the Lower Cambrian Xiaoerblak Formation in the Sugaitblak Section and Its Significance for Exploring Regions in the Tarim Basin, NW China[J]. Acta Sedimentologica Sinica, 2019, 37(3): 601-609. doi: 10.14027/j.issn.1000-0550.2018.142

Citation:

ZHENG JianFeng, CHEN YongQuan, HUANG LiLi, YAN Wei, NI XinFeng, LI BaoHua, Guo XiaoYan. Reservoir Modeling of the Lower Cambrian Xiaoerblak Formation in the Sugaitblak Section and Its Significance for Exploring Regions in the Tarim Basin, NW China[J]. Acta Sedimentologica Sinica, 2019, 37(3): 601-609. doi: 10.14027/j.issn.1000-0550.2018.142

引用本文:

Citation:

ZHENG JianFeng, CHEN YongQuan, HUANG LiLi, YAN Wei, NI XinFeng, LI BaoHua, Guo XiaoYan. Reservoir Modeling of the Lower Cambrian Xiaoerblak Formation in the Sugaitblak Section and Its Significance for Exploring Regions in the Tarim Basin, NW China[J]. Acta Sedimentologica Sinica, 2019, 37(3): 601-609. doi: 10.14027/j.issn.1000-0550.2018.142

苏盖特布拉克剖面肖尔布拉克组储层建模研究及其勘探意义

doi: 10.14027/j.issn.1000-0550.2018.142

1.
中国石油集团碳酸盐岩储层重点实验室, 杭州 310023;
2.
中国石油杭州地质研究院, 杭州 310023;
3.
中国石油塔里木油田分公司, 新疆库尔勒 841000

基金项目: 国家重大科技专项（2016ZX05004002）；中国石油天然气股份有限公司科技项目（2016B-0402）

详细信息

作者简介:
郑剑锋,男,1977年出生,硕士,高级工程师,碳酸盐岩沉积储层,E-mail:zhengjf_hz@petrochina.com.cn

中图分类号: P618.13;P628⁺.3TE319

计量

文章访问数: 493
HTML全文浏览量: 29
PDF下载量: 321
被引次数: 0

Reservoir Modeling of the Lower Cambrian Xiaoerblak Formation in the Sugaitblak Section and Its Significance for Exploring Regions in the Tarim Basin, NW China

1.
Key Laboratory of Carbonate Reservoir, CNPC, Hangzhou 310023, China;
2.
PetroChina Hangzhou Research Institute of Geology, Hangzhou 310023, China;
3.
Tarim Oil field Company, PetroChina, Korla, Xinjiang 841000, China

Funds: National Science and Technology Major Project, No. 2016ZX05004002; Petro China Science and Technology Project, No. 2016B-0402

摘要

摘要: 明确塔里木盆地肖尔布拉克组储层的品质、规模及分布规律对指导寒武系盐下领域的勘探具有重要意义。通过对柯坪地区苏盖特布拉克剖面的解剖，阐明了肖尔布拉克组主要发育与藻（蓝细菌）有关的微生物白云岩（层纹石白云岩、凝块石白云岩、叠层石白云岩和藻格架白云岩）、黏结藻屑白云岩、藻砂屑白云岩、泥-粉晶白云岩和含砂屑泥-粉晶白云岩，自下而上的岩相组合指示缓坡型台地沉积特征；孔隙类型主要为溶蚀孔洞，粒（晶）间溶孔和藻格架溶孔，总体具有中高孔-中低渗的特征，孔隙的发育与岩相具有明显的相关性，其中藻砂屑白云岩和具有格架结构的微生物白云岩储层物性最好；通过二维地质建模及基于数字露头的三维地质建模，揭示了肖尔布拉克组储层具有较好的层位性、相控性和规模性，古隆起围斜部位的中缓坡丘滩体是储层发育的有利相带。
- 塔里木盆地 /
- 苏盖特布拉克剖面 /
- 肖尔布拉克组 /
- 白云岩 /
- 储层建模
Abstract: Studying the quality and distribution law of the Xiaoerblak Formation (Fm.) is significant for guiding the exploration of Cambrian sub-salt area. The quality and scale of the reservoir are the main factors causing the restriction of further exploration in the Xiaoerblak Fm. of the Lower Cambrian, Tarim Basin. This study takes the Sugaiteblak Section in the Keping area as an example. Based on the detailed description, physical properties analysis, and three-dimensional (3D) reservoir geological modeling in the Xiaoerblak Fm., we found that microbial dolomite (including laminate, thrombolite, stromatolite, and microbial framework dolomite), dolarenite, and muddy to micritic dolomite are the main rock types indicating the sedimentary characteristics of the ramp. Vugs, intergranular dissolved pores (or intercrystalline pores), and framework pores are the main reservoir spaces, which have an obvious correlation with lithofacies. Among them, dolarenite and microbial framework dolomite are the most favorable reservoir rocks. Generally speaking, the reservoir has characteristics of middle-high porosity and middle-low permeability. The scale development of the reservoir was controlled by a high frequency sequence and sedimentary microfacies, and microbial mounds and shoals in the middle ramp around the ancient uplift are the favorable facies zones.
- Tarim Basin /
- Sugaiteblak Section /
- Xiaoerblak Formation /
- dolomite /
- reservoir modeling

HTML全文

参考文献(0)

[1]	王振宇, 宁科科, 屈海洲, 胡安平, 张云峰, 陈薇, 罗新生, 张兴宇. 阿克苏地区寒武系肖尔布拉克组不同白云岩的孔隙特征、成因及演化 . 沉积学报, 2023, 41(1): 256-269. doi: 10.14027/j.issn.1000-0550.2021.157
[2]	魏天媛, 蔡春芳, 扈永杰, 刘大卫, 蒋子文. 塔里木盆地下寒武统肖尔布拉克组储层成因 . 沉积学报, 2023, 41(2): 527-544. doi: 10.14027/j.issn.1000-0550.2021.116
[3]	宋亚芳, 陈代钊, 郭川, 周锡强. 塔里木盆地肖尔布拉克剖面肖尔布拉克组下段微生物碳酸盐岩沉积特征 . 沉积学报, 2020, 38(1): 55-63. doi: 10.14027/j.issn.1000-0550.2019.024
[4]	朱永进, 倪新锋, 刘玲利, 乔占峰, 陈永权, 郑剑锋. 裂后沉降期碳酸盐岩缓坡沉积响应及成储特征——以塔里木盆地下寒武统肖尔布拉克组为例 . 沉积学报, 2019, 37(5): 1044-1057. doi: 10.14027/j.issn.1000-0550.2019.006
[5]	李百强, 王起琮, 张小莉, 魏巍. 白云岩成岩相与地球化学特征——以鄂尔多斯盆地中东部马家沟组马五₅-马五₁亚段为例 . 沉积学报, 2018, 36(3): 608-616. doi: 10.14027/j.issn.1000-0550.2018.038
[6]	尤东华, 韩俊, 胡文瑄, 陈强路, 曹自成, 席斌斌, 鲁子野. 塔里木盆地顺南501井鹰山组白云岩储层特征与成因 . 沉积学报, 2018, 36(6): 1206-1217. doi: 10.14027/j.issn.1000-0550.2018.092
[7]	邓世彪, 关平, 庞磊, 刘沛显, 金亦秋, 张艳秋. 塔里木盆地柯坪地区肖尔布拉克组优质微生物碳酸盐岩储层成因 . 沉积学报, 2018, 36(6): 1218-1232. doi: 10.14027/j.issn.1000-0550.2018.084
[8]	杨程宇, 李美俊, 倪智勇, 杨福林, 陈昊卫. 塔里木盆地西北缘玉尔吐斯组硅质岩成因及石油地质意义 . 沉积学报, 2016, 34(4): 653-661. doi: 10.14027/j.cnki.cjxb.2016.04.005
[9]	高达, 林畅松, 胡明毅, 黄理力. 利用自然伽马能谱测井识别碳酸盐岩高频层序——以塔里木盆地塔中地区T1井良里塔格组为例 . 沉积学报, 2016, 34(4): 707-715. doi: 10.14027/j.cnki.cjxb.2016.04.011
[10]	熊益学, 陈永权, 关宝珠, 邓力萍, 倪新锋, 熊冉. 塔里木盆地下寒武统肖尔布拉克组北部台缘带展布及其油气勘探意义 . 沉积学报, 2015, 33(2): 408-415. doi: 10.14027/j.cnki.cjxb.2015.02.020
[11]	. 塔里木盆地中央隆起区寒武—奥陶系白云岩结构特征及成因探讨 . 沉积学报, 2014, 32(3): 538-549.
[12]	倪新锋. 塔里木盆地英买力—哈拉哈塘地区奥陶系碳酸盐岩岩溶型储层特征及成因 . 沉积学报, 2011, 29(3): 465-474.
[13]	张荣虎. 塔里木盆地白垩系巴什基奇克组陆相砂岩中碳酸盐岩碎屑特征及其地质意义 . 沉积学报, 2009, 27(3): 410-418.
[14]	刘建清. 羌塘盆地中央隆起带南侧隆额尼—昂达尔错布曲组古油藏白云岩稀土元素特征及成因意义 . 沉积学报, 2008, 26(1): 28-38.
[15]	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.
[16]	于炳松, 陈建强, 李兴武, 林畅松. 塔里木盆地肖尔布拉克剖面下寒武统底部硅质岩微量元素和稀土元素地球化学及其沉积背景 . 沉积学报, 2004, 22(1): 59-66.
[17]	陈强路, 王恕一, 钱一雄, 马红强. 塔里木盆地阿克库勒地区下奥陶统古岩溶及油气分布 . 沉积学报, 2002, 20(4): 633-637.
[18]	张晓宝. 准噶尔盆地南缘东部中二叠流芦草沟组黑色页岩中白云岩夹层的成因探讨 . 沉积学报, 1993, 11(2): 133-140.
[19]	史基安. 塔里木盆地西北缘震旦系和古生代白云岩成因及其储集性 . 沉积学报, 1993, 11(2): 43-50.
[20]	曾允孚, 黄思静, H.Kulke, M.Sch nfeld. 四川甘溪泥盆系观雾山组白云岩特征与其形成条件的关系(英文) . 沉积学报, 1988, 6(4): 12-21.

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: 493
HTML全文浏览量: 29
PDF下载量: 321
被引次数: 0

苏盖特布拉克剖面肖尔布拉克组储层建模研究及其勘探意义

doi: 10.14027/j.issn.1000-0550.2018.142

1. 中国石油集团碳酸盐岩储层重点实验室, 杭州 310023;

2. 中国石油杭州地质研究院, 杭州 310023;

3. 中国石油塔里木油田分公司, 新疆库尔勒 841000

基金项目: 国家重大科技专项（2016ZX05004002）；中国石油天然气股份有限公司科技项目（2016B-0402）

作者简介:
郑剑锋,男,1977年出生,硕士,高级工程师,碳酸盐岩沉积储层,E-mail:zhengjf_hz@petrochina.com.cn

收稿日期: 2018-04-02
修回日期: 2018-05-25
刊出日期: 2019-06-10

中图分类号: P618.13;P628⁺.3TE319

关键词:

白云岩 /

摘要: 明确塔里木盆地肖尔布拉克组储层的品质、规模及分布规律对指导寒武系盐下领域的勘探具有重要意义。通过对柯坪地区苏盖特布拉克剖面的解剖，阐明了肖尔布拉克组主要发育与藻（蓝细菌）有关的微生物白云岩（层纹石白云岩、凝块石白云岩、叠层石白云岩和藻格架白云岩）、黏结藻屑白云岩、藻砂屑白云岩、泥-粉晶白云岩和含砂屑泥-粉晶白云岩，自下而上的岩相组合指示缓坡型台地沉积特征；孔隙类型主要为溶蚀孔洞，粒（晶）间溶孔和藻格架溶孔，总体具有中高孔-中低渗的特征，孔隙的发育与岩相具有明显的相关性，其中藻砂屑白云岩和具有格架结构的微生物白云岩储层物性最好；通过二维地质建模及基于数字露头的三维地质建模，揭示了肖尔布拉克组储层具有较好的层位性、相控性和规模性，古隆起围斜部位的中缓坡丘滩体是储层发育的有利相带。

English Abstract

Reservoir Modeling of the Lower Cambrian Xiaoerblak Formation in the Sugaitblak Section and Its Significance for Exploring Regions in the Tarim Basin, NW China

1. Key Laboratory of Carbonate Reservoir, CNPC, Hangzhou 310023, China;

2. PetroChina Hangzhou Research Institute of Geology, Hangzhou 310023, China;

3. Tarim Oil field Company, PetroChina, Korla, Xinjiang 841000, China

Funds: National Science and Technology Major Project, No. 2016ZX05004002; Petro China Science and Technology Project, No. 2016B-0402

Received Date: 2018-04-02
Rev Recd Date: 2018-05-25
Publish Date: 2019-06-10

Keywords:

Abstract: Studying the quality and distribution law of the Xiaoerblak Formation (Fm.) is significant for guiding the exploration of Cambrian sub-salt area. The quality and scale of the reservoir are the main factors causing the restriction of further exploration in the Xiaoerblak Fm. of the Lower Cambrian, Tarim Basin. This study takes the Sugaiteblak Section in the Keping area as an example. Based on the detailed description, physical properties analysis, and three-dimensional (3D) reservoir geological modeling in the Xiaoerblak Fm., we found that microbial dolomite (including laminate, thrombolite, stromatolite, and microbial framework dolomite), dolarenite, and muddy to micritic dolomite are the main rock types indicating the sedimentary characteristics of the ramp. Vugs, intergranular dissolved pores (or intercrystalline pores), and framework pores are the main reservoir spaces, which have an obvious correlation with lithofacies. Among them, dolarenite and microbial framework dolomite are the most favorable reservoir rocks. Generally speaking, the reservoir has characteristics of middle-high porosity and middle-low permeability. The scale development of the reservoir was controlled by a high frequency sequence and sedimentary microfacies, and microbial mounds and shoals in the middle ramp around the ancient uplift are the favorable facies zones.

引用本文:

Citation:

ZHENG JianFeng, CHEN YongQuan, HUANG LiLi, YAN Wei, NI XinFeng, LI BaoHua, Guo XiaoYan. Reservoir Modeling of the Lower Cambrian Xiaoerblak Formation in the Sugaitblak Section and Its Significance for Exploring Regions in the Tarim Basin, NW China[J]. Acta Sedimentologica Sinica, 2019, 37(3): 601-609. doi: 10.14027/j.issn.1000-0550.2018.142

全文HTML

下载: 全尺寸图片幻灯片

返回文章

用微信扫码二维码

分享至好友和朋友圈

x 关闭永久关闭

2023年地质事件沉积研究新进展国际学术研讨会（第一号通知）

留言板

苏盖特布拉克剖面肖尔布拉克组储层建模研究及其勘探意义

doi: 10.14027/j.issn.1000-0550.2018.142

作者简介:
郑剑锋,男,1977年出生,硕士,高级工程师,碳酸盐岩沉积储层,E-mail:zhengjf_hz@petrochina.com.cn

计量

Reservoir Modeling of the Lower Cambrian Xiaoerblak Formation in the Sugaitblak Section and Its Significance for Exploring Regions in the Tarim Basin, NW China

计量

目录

苏盖特布拉克剖面肖尔布拉克组储层建模研究及其勘探意义

doi: 10.14027/j.issn.1000-0550.2018.142

1. 中国石油集团碳酸盐岩储层重点实验室, 杭州 310023;

2. 中国石油杭州地质研究院, 杭州 310023;

3. 中国石油塔里木油田分公司, 新疆库尔勒 841000

作者简介:
郑剑锋,男,1977年出生,硕士,高级工程师,碳酸盐岩沉积储层,E-mail:zhengjf_hz@petrochina.com.cn

English Abstract

Reservoir Modeling of the Lower Cambrian Xiaoerblak Formation in the Sugaitblak Section and Its Significance for Exploring Regions in the Tarim Basin, NW China

1. Key Laboratory of Carbonate Reservoir, CNPC, Hangzhou 310023, China;

2. PetroChina Hangzhou Research Institute of Geology, Hangzhou 310023, China;

3. Tarim Oil field Company, PetroChina, Korla, Xinjiang 841000, China

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

苏盖特布拉克剖面肖尔布拉克组储层建模研究及其勘探意义

doi: 10.14027/j.issn.1000-0550.2018.142

作者简介: 郑剑锋,男,1977年出生,硕士,高级工程师,碳酸盐岩沉积储层,E-mail:zhengjf_hz@petrochina.com.cn

计量

出版历程

Reservoir Modeling of the Lower Cambrian Xiaoerblak Formation in the Sugaitblak Section and Its Significance for Exploring Regions in the Tarim Basin, NW China

计量

出版历程

目录

苏盖特布拉克剖面肖尔布拉克组储层建模研究及其勘探意义

doi: 10.14027/j.issn.1000-0550.2018.142

1. 中国石油集团碳酸盐岩储层重点实验室, 杭州 310023; 2. 中国石油杭州地质研究院, 杭州 310023; 3. 中国石油塔里木油田分公司, 新疆库尔勒 841000

作者简介: 郑剑锋,男,1977年出生,硕士,高级工程师,碳酸盐岩沉积储层,E-mail:zhengjf_hz@petrochina.com.cn

English Abstract

Reservoir Modeling of the Lower Cambrian Xiaoerblak Formation in the Sugaitblak Section and Its Significance for Exploring Regions in the Tarim Basin, NW China

1. Key Laboratory of Carbonate Reservoir, CNPC, Hangzhou 310023, China; 2. PetroChina Hangzhou Research Institute of Geology, Hangzhou 310023, China; 3. Tarim Oil field Company, PetroChina, Korla, Xinjiang 841000, China

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
郑剑锋,男,1977年出生,硕士,高级工程师,碳酸盐岩沉积储层,E-mail:zhengjf_hz@petrochina.com.cn

1. 中国石油集团碳酸盐岩储层重点实验室, 杭州 310023;

2. 中国石油杭州地质研究院, 杭州 310023;

3. 中国石油塔里木油田分公司, 新疆库尔勒 841000

作者简介:
郑剑锋,男,1977年出生,硕士,高级工程师,碳酸盐岩沉积储层,E-mail:zhengjf_hz@petrochina.com.cn

1. Key Laboratory of Carbonate Reservoir, CNPC, Hangzhou 310023, China;

2. PetroChina Hangzhou Research Institute of Geology, Hangzhou 310023, China;

3. Tarim Oil field Company, PetroChina, Korla, Xinjiang 841000, China