不同古地貌单元水下分流河道沉积特征及其意义&mdash;&mdash;以准噶尔盆地夏盐地区三工河组二段为例

厚刚福; 孙靖; 王力宝; 李亚哲; 李啸; 沈金龙; 窦洋; 陈扬; 韩守华

doi:10.14027/j.issn.1000-0550.2018.175

ISSN 1000-0550 CN 62-1038/P

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不同古地貌单元水下分流河道沉积特征及其意义——以准噶尔盆地夏盐地区三工河组二段为例

厚刚福, 孙靖, 王力宝, 李亚哲, 李啸, 沈金龙, 窦洋, 陈扬, 韩守华

文章导航 > 沉积学报 > 2019 > 37(4): 825-833

厚刚福, 孙靖, 王力宝, 李亚哲, 李啸, 沈金龙, 窦洋, 陈扬, 韩守华. 不同古地貌单元水下分流河道沉积特征及其意义——以准噶尔盆地夏盐地区三工河组二段为例[J]. 沉积学报, 2019, 37(4): 825-833. doi: 10.14027/j.issn.1000-0550.2018.175

引用本文:

HOU GangFu, SUN Jing, WANG LiBao, LI YaZhe, LI Xiao, SHEN JinLong, DOU Yang, CHEN Yang, HAN ShouHua. Sedimentary Characteristics and Significance of Underwater Distri butary Channel in Different Paleogeomorphic Units: A case study of the second member of the Sangonghe Formation in Xiayan district, Junggar Basin[J]. Acta Sedimentologica Sinica, 2019, 37(4): 825-833. doi: 10.14027/j.issn.1000-0550.2018.175

Citation:

HOU GangFu, SUN Jing, WANG LiBao, LI YaZhe, LI Xiao, SHEN JinLong, DOU Yang, CHEN Yang, HAN ShouHua. Sedimentary Characteristics and Significance of Underwater Distri butary Channel in Different Paleogeomorphic Units: A case study of the second member of the Sangonghe Formation in Xiayan district, Junggar Basin[J]. Acta Sedimentologica Sinica, 2019, 37(4): 825-833. doi: 10.14027/j.issn.1000-0550.2018.175

引用本文:

Citation:

HOU GangFu, SUN Jing, WANG LiBao, LI YaZhe, LI Xiao, SHEN JinLong, DOU Yang, CHEN Yang, HAN ShouHua. Sedimentary Characteristics and Significance of Underwater Distri butary Channel in Different Paleogeomorphic Units: A case study of the second member of the Sangonghe Formation in Xiayan district, Junggar Basin[J]. Acta Sedimentologica Sinica, 2019, 37(4): 825-833. doi: 10.14027/j.issn.1000-0550.2018.175

不同古地貌单元水下分流河道沉积特征及其意义——以准噶尔盆地夏盐地区三工河组二段为例

doi: 10.14027/j.issn.1000-0550.2018.175

1.
中国石油杭州地质研究院, 杭州 310023;
2.
中国石油新疆油田分公司勘探开发研究院, 新疆克拉玛依 834000

基金项目: 国家科技重大专项（2017ZX05001-002，2017ZX05001-004）；中国石油科技重大专项（2017E-0401，2019B-0303）

详细信息

作者简介:
厚刚福,男,1982年出生,高级工程师,沉积储层,E-mail:hougf_hz@petrochina.com.cn

中图分类号: P631;P618.13

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文章访问数: 419
HTML全文浏览量: 19
PDF下载量: 201
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Sedimentary Characteristics and Significance of Underwater Distri butary Channel in Different Paleogeomorphic Units: A case study of the second member of the Sangonghe Formation in Xiayan district, Junggar Basin

1.
Hangzhou Research Institute of Geology, PetroChina, Hangzhou 310023, China;
2.
Research Institute of Exploration and Development, Xinjiang Oilfield Company, PetroChina, Karamay, Xinjiang 834000, China

Funds: National Science and Technology Major Project, No. 2017ZX05001-002, 2017ZX05001-004; Science and Technology Major Project, CNPC, No. 2017E-0401,2019B-0303

摘要

摘要: 为详细解剖水下分流河道沉积特征，探讨其岩性圈闭意义，采用多参数分析方法，对水下分流河道微相沉积特征进行了分析，提出了发育于不同古地貌单元的水下分流河道微相砂体由于物性存在差异而对岩性圈闭的形成具有重要意义。研究结果表明：研究区三工河组二段发育古低凸和古沟槽2种古地貌单元，古沟槽发育反旋回叠置型水下分流河道，低凸翼部发育正旋回叠置型水下分流河道。正旋回叠置型水下分流河道砂体物性自下而上逐渐变差，在侧向对反旋回叠置型水下分流河道储集体构成侧向遮挡，有利于形成岩性圈闭。在此基础上建立了岩性圈闭模式，将该模式应用到油田预探井井位部署中，取得了很好的效果。
- 准噶尔盆地 /
- 三工河组 /
- 水下分流河道 /
- 正旋回 /
- 反旋回 /
- 岩性圈闭
Abstract: In order to dissect the characteristics of underwater distributary channel and discuss its significance for the formation of lithological traps,the sedimentary microfacies characteristics of an underwater distributary channel were analyzed by multi-parameter analysis. It is proposed that underwater distributary channel microfacies sandbodies which develop in different paleogeomorphological units are of great significance to the formation of lithological traps because of their different physical properties. The results show that two paleogeomorphological units are present in an ancient low rise and an ancient trench in the second section of the Sangonghe Formation in the study area:a non-rotat-ing distributary channel was developed in the ancient trench,and a rotating distributary channel developed on the sides of the low rise. The physical properties of the normal cyclic underwater distributary channel sandbody gradually deteriorated from bottom to top,and lateral blockages formed at the sides of the reverse cyclic distributary channel reservoir,which was beneficial to the formation of lithological traps. On this basis,a lithological trap model was es-tablished and applied for the positioning of a pre-exploration well in the oilfield, and achieved good results.
- Junggar Basin /
- Sangonghe Formation /
- underwater distributary channel /
- positive cycle /
- reverse cycle /
- lithological trap

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[1]	单祥, 郭华军, 陈希光, 郭旭光, 佘敏, 李亚哲. 准噶尔盆地玛西斜坡区百口泉组砂砾岩埋藏溶蚀作用实验模拟研究 . 沉积学报, 2022, 40(5): 1406-1418. doi: 10.14027/j.issn.1000-0550.2021.050
[2]	张新智, 吕沛宗, 方琳浩, 杨涵, 邓胜徽, 卢远征, 房亚男, 张小宇, 黄汝婷, 梁佳宝, 师生宝. 三叠纪—侏罗纪之交准噶尔盆地南缘野火记录及全球对比 . 沉积学报, 2022, 40(2): 473-483. doi: 10.14027/j.issn.1000-0550.2020.103
[3]	梁爽, 杜社宽. 准噶尔盆地中拐凸起侏罗系三工河组储层特征及控制因素 . 沉积学报, 2019, 37(6): 1269-1279. doi: 10.14027/j.issn.1000-0550.2019.010
[4]	张坦, 张昌民, 瞿建华, 朱锐, 袁瑞, 潘进, 陶金雨. 准噶尔盆地玛湖凹陷百口泉组相对湖平面升降规律研究 . 沉积学报, 2018, 36(4): 684-694. doi: 10.14027/j.issn.1000-0550.2018.057
[5]	郭沫贞, 徐洋, 寿建峰, 刘占国, 韩守华. 准噶尔盆地西北缘二叠系碎屑岩次生孔隙发育控制因素 . 沉积学报, 2017, 35(2): 330-342. doi: 10.14027/j.cnki.cjxb.2017.02.011
[6]	高崇龙, 纪友亮, 高志勇, 王剑, 任影, 刘大卫, 段小兵, 桓芝俊, 程同冉. 准噶尔盆地腹部深层储层物性保存过程多因素耦合分析 . 沉积学报, 2017, 35(3): 577-591. doi: 10.14027/j.cnki.cjxb.2017.03.015
[7]	单祥, 邹志文, 孟祥超, 唐勇, 郭华军, 陈能贵, 徐洋. 准噶尔盆地环玛湖地区三叠系百口泉组物源分析 . 沉积学报, 2016, 34(5): 930-939. doi: 10.14027/j.cnki.cjxb.2016.05.012
[8]	任双坡, 姚光庆, 毛文静. 三角洲前缘水下分流河道薄层单砂体成因类型及其叠置模式——以古城油田泌浅10区核三段Ⅳ-Ⅵ油组为例 . 沉积学报, 2016, 34(3): 582-593. doi: 10.14027/j.cnki.cjxb.2016.03.016
[9]	孙雨, 赵丹, 于利民, 王继平, 闫百泉, 马世忠. 浅水湖盆河控三角洲前缘砂体分布特征与沉积模式探讨——以松辽盆地北部永乐地区葡萄花油层为例 . 沉积学报, 2015, 33(3): 439-447. doi: 10.14027/j.cnki.cjxb.2015.03.002
[10]	. 松辽盆地新立—新北地区嫩江组三段浅水三角洲水下分流河道砂体半定量解剖 . 沉积学报, 2012, 30(3): 511-521.
[11]	唐勇. 准噶尔盆地腹部缓坡型岩性地层油气藏成藏控制因素分析 . 沉积学报, 2009, 27(3): 567-573.
[12]	赵霞. 准噶尔盆地石南地区清水河组一段层序地层特征 . 沉积学报, 2007, 25(5): 716-721.
[13]	李双文, 刘洛夫, 张有平, 姚卫江, 靳军, 赵建章, 孙东. 准噶尔盆地莫北凸起侏罗系三工河组沉积演化及微相构成 . 沉积学报, 2006, (6): 819-828.
[14]	李双文刘洛夫张有平姚卫江靳军赵建章孙东. 准噶尔盆地莫北凸起侏罗系三工河组沉积演化及微相构成 . 沉积学报, 2006, 24(06): 819-828.
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[16]	何志平, 邵龙义, 康永尚, 刘永福, 罗文林, 齐雪峰. 准噶尔盆地侏罗系八道湾组聚煤作用控制因素分析 . 沉积学报, 2004, 22(3): 449-454.
[17]	李凤杰, 王多云, 郑希民, 刘自亮, 王峰, 李树同, 王志坤. 陕甘宁盆地华池地区延长组缓坡带三角洲前缘的微相构成 . 沉积学报, 2002, 20(4): 582-587.
[18]	刘洛夫, 康永尚, 齐雪峰, 唐勇, 熊正祥. 准噶尔盆地侏罗系层序地层格架中的烃源岩评价 . 沉积学报, 2002, 20(4): 687-694.
[19]	李文厚, 林晋炎, 袁明生, 王武和. 吐鲁番－哈密盆地的两种粗碎屑三角洲 . 沉积学报, 1996, 14(3): 113-121.
[20]	顾家裕, 何斌. 塔里木盆地轮南地区三叠系扇三角洲沉积与储集层研究 . 沉积学报, 1994, 12(2): 54-62.

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不同古地貌单元水下分流河道沉积特征及其意义——以准噶尔盆地夏盐地区三工河组二段为例

doi: 10.14027/j.issn.1000-0550.2018.175

1. 中国石油杭州地质研究院, 杭州 310023;

2. 中国石油新疆油田分公司勘探开发研究院, 新疆克拉玛依 834000

基金项目: 国家科技重大专项（2017ZX05001-002，2017ZX05001-004）；中国石油科技重大专项（2017E-0401，2019B-0303）

作者简介:
厚刚福,男,1982年出生,高级工程师,沉积储层,E-mail:hougf_hz@petrochina.com.cn

收稿日期: 2018-07-09
修回日期: 2018-09-26
刊出日期: 2019-08-10

中图分类号: P631;P618.13

关键词:

准噶尔盆地 /

三工河组 /

水下分流河道 /

正旋回 /

反旋回 /

岩性圈闭

摘要: 为详细解剖水下分流河道沉积特征，探讨其岩性圈闭意义，采用多参数分析方法，对水下分流河道微相沉积特征进行了分析，提出了发育于不同古地貌单元的水下分流河道微相砂体由于物性存在差异而对岩性圈闭的形成具有重要意义。研究结果表明：研究区三工河组二段发育古低凸和古沟槽2种古地貌单元，古沟槽发育反旋回叠置型水下分流河道，低凸翼部发育正旋回叠置型水下分流河道。正旋回叠置型水下分流河道砂体物性自下而上逐渐变差，在侧向对反旋回叠置型水下分流河道储集体构成侧向遮挡，有利于形成岩性圈闭。在此基础上建立了岩性圈闭模式，将该模式应用到油田预探井井位部署中，取得了很好的效果。

English Abstract

Sedimentary Characteristics and Significance of Underwater Distri butary Channel in Different Paleogeomorphic Units: A case study of the second member of the Sangonghe Formation in Xiayan district, Junggar Basin

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

2. Research Institute of Exploration and Development, Xinjiang Oilfield Company, PetroChina, Karamay, Xinjiang 834000, China

Funds: National Science and Technology Major Project, No. 2017ZX05001-002, 2017ZX05001-004; Science and Technology Major Project, CNPC, No. 2017E-0401,2019B-0303

Received Date: 2018-07-09
Rev Recd Date: 2018-09-26
Publish Date: 2019-08-10

Keywords:

Abstract: In order to dissect the characteristics of underwater distributary channel and discuss its significance for the formation of lithological traps,the sedimentary microfacies characteristics of an underwater distributary channel were analyzed by multi-parameter analysis. It is proposed that underwater distributary channel microfacies sandbodies which develop in different paleogeomorphological units are of great significance to the formation of lithological traps because of their different physical properties. The results show that two paleogeomorphological units are present in an ancient low rise and an ancient trench in the second section of the Sangonghe Formation in the study area:a non-rotat-ing distributary channel was developed in the ancient trench,and a rotating distributary channel developed on the sides of the low rise. The physical properties of the normal cyclic underwater distributary channel sandbody gradually deteriorated from bottom to top,and lateral blockages formed at the sides of the reverse cyclic distributary channel reservoir,which was beneficial to the formation of lithological traps. On this basis,a lithological trap model was es-tablished and applied for the positioning of a pre-exploration well in the oilfield, and achieved good results.

引用本文:

Citation:

HOU GangFu, SUN Jing, WANG LiBao, LI YaZhe, LI Xiao, SHEN JinLong, DOU Yang, CHEN Yang, HAN ShouHua. Sedimentary Characteristics and Significance of Underwater Distri butary Channel in Different Paleogeomorphic Units: A case study of the second member of the Sangonghe Formation in Xiayan district, Junggar Basin[J]. Acta Sedimentologica Sinica, 2019, 37(4): 825-833. doi: 10.14027/j.issn.1000-0550.2018.175

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不同古地貌单元水下分流河道沉积特征及其意义——以准噶尔盆地夏盐地区三工河组二段为例

doi: 10.14027/j.issn.1000-0550.2018.175

作者简介:
厚刚福,男,1982年出生,高级工程师,沉积储层,E-mail:hougf_hz@petrochina.com.cn

计量

Sedimentary Characteristics and Significance of Underwater Distri butary Channel in Different Paleogeomorphic Units: A case study of the second member of the Sangonghe Formation in Xiayan district, Junggar Basin

计量

目录

不同古地貌单元水下分流河道沉积特征及其意义——以准噶尔盆地夏盐地区三工河组二段为例

doi: 10.14027/j.issn.1000-0550.2018.175

1. 中国石油杭州地质研究院, 杭州 310023;

2. 中国石油新疆油田分公司勘探开发研究院, 新疆克拉玛依 834000

作者简介:
厚刚福,男,1982年出生,高级工程师,沉积储层,E-mail:hougf_hz@petrochina.com.cn

English Abstract

Sedimentary Characteristics and Significance of Underwater Distri butary Channel in Different Paleogeomorphic Units: A case study of the second member of the Sangonghe Formation in Xiayan district, Junggar Basin

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

2. Research Institute of Exploration and Development, Xinjiang Oilfield Company, PetroChina, Karamay, Xinjiang 834000, China

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不同古地貌单元水下分流河道沉积特征及其意义——以准噶尔盆地夏盐地区三工河组二段为例

doi: 10.14027/j.issn.1000-0550.2018.175

作者简介: 厚刚福,男,1982年出生,高级工程师,沉积储层,E-mail:hougf_hz@petrochina.com.cn

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Sedimentary Characteristics and Significance of Underwater Distri butary Channel in Different Paleogeomorphic Units: A case study of the second member of the Sangonghe Formation in Xiayan district, Junggar Basin

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出版历程

目录

不同古地貌单元水下分流河道沉积特征及其意义——以准噶尔盆地夏盐地区三工河组二段为例

doi: 10.14027/j.issn.1000-0550.2018.175

1. 中国石油杭州地质研究院, 杭州 310023; 2. 中国石油新疆油田分公司勘探开发研究院, 新疆克拉玛依 834000

作者简介: 厚刚福,男,1982年出生,高级工程师,沉积储层,E-mail:hougf_hz@petrochina.com.cn

English Abstract

Sedimentary Characteristics and Significance of Underwater Distri butary Channel in Different Paleogeomorphic Units: A case study of the second member of the Sangonghe Formation in Xiayan district, Junggar Basin

1. Hangzhou Research Institute of Geology, PetroChina, Hangzhou 310023, China; 2. Research Institute of Exploration and Development, Xinjiang Oilfield Company, PetroChina, Karamay, Xinjiang 834000, China

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
厚刚福,男,1982年出生,高级工程师,沉积储层,E-mail:hougf_hz@petrochina.com.cn

1. 中国石油杭州地质研究院, 杭州 310023;

2. 中国石油新疆油田分公司勘探开发研究院, 新疆克拉玛依 834000

作者简介:
厚刚福,男,1982年出生,高级工程师,沉积储层,E-mail:hougf_hz@petrochina.com.cn

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

2. Research Institute of Exploration and Development, Xinjiang Oilfield Company, PetroChina, Karamay, Xinjiang 834000, China