准噶尔盆地红山嘴地区三叠系克上组两类粗粒三角洲的沉积记录差异及其成因<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2018.06.071

古地理学报 ›› 2018, Vol. 20 ›› Issue (6): 973-988. doi: 10.7605/gdlxb.2018.06.071

• “碎屑岩油气储层表征” 专辑 • 上一篇下一篇

准噶尔盆地红山嘴地区三叠系克上组两类粗粒三角洲的沉积记录差异及其成因^*

高阳^1,2, 于兴河², 曾大乾¹, 姚宗全², 刘文峰³, 杨新涛³

1 中国石化石油勘探开发研究院,北京 100083;
2 中国地质大学(北京)能源学院,北京 100083;
3 中国石油新疆油田分公司采油一厂,新疆克拉玛依 834000

收稿日期:2018-04-13 修回日期:2018-09-25 出版日期:2018-12-01 发布日期:2018-11-27
通讯作者: 于兴河,男,1958年生,中国地质大学(北京)教授,博士生导师,主要研究方向为沉积学、储集层表征建模及油气地质。E-mail: billyu@cugb.edu.cn。
作者简介:高阳,男,1988年生,中国石化石油勘探开发研究院博士后,主要从事沉积学、储层表征与建模方面的研究工作。E-mail: gaoyangdzdx@126.com。
基金资助:
*国家自然科学基金项目(编号: 41472091)和国家科技重大专项(编号:2017ZX05001-002-003)联合资助

Differences in sedimentary records of different coarse-grained deltas and their genesis in the Triassic Upper Karamay Formation,Hongshanzui area,Junggar Basin

Gao Yang^{1, 2}, Yu Xing-He², Zeng Da-Qian¹, Yao Zong-Quan², Liu Wen-Feng³, Yang Xin-Tao³

1 Petroleum Exploration and Production Research Institute,SINOPEC,Beijing 100083;
2 School of Energy Resources,China University of Geosciences(Beijing),Beijing 100083;
3 No.1 Oil Production Plant,Xinjiang Oilfield Company,PetroChina,Karamay 834000,Xinjiang;

Received:2018-04-13 Revised:2018-09-25 Online:2018-12-01 Published:2018-11-27
Contact: Yu Xing-He,born in 1958,is a professor and doctoral supervisor in China University of Geosciences(Beijing).He is mainly engaged in sedimentology,reservoir characterization and modeling and petroleum geology.E-mail: billyu@cugb.edu.cn.
About author:Gao Yang,born in 1988,is a postdoctor in Petroleum Exploration and Production Research Institute,Sinopec.He is mainly engaged in sedimentology,reservoir characterization and modeling.E-mail: gaoyangdzdx@126.com.
Supported by:
Co-funded by the National Natural Science Foundation of China(No.41472091) and the National Science and Technology Major Project(No.2017ZX05001-002-003)

摘要/Abstract

摘要： 准噶尔盆地红山嘴地区三叠系克上组存在扇三角洲与辫状河三角洲这两类粗粒三角洲,其界定在油气沉积学领域一直备受关注,而基于岩相类型及其垂向组合特征的沉积作用研究,辅以砂体宏观展布规律将有助于这两类三角洲的判别。红山嘴地区克上组扇三角洲以发育各种交错层理砾岩相(Gi、Gt、Gp)与块状砾岩相(Gmm、Gcm、Gcs)为特点,而辫状河三角洲则发育各种砂岩相(St、Sp、Sm和Sh等);扇三角洲6种岩相组合显示其碎屑流与密度流沉积相对发育,韵律特征不明显,而辫状河三角洲的7种岩相组合均显示其牵引流沉积作用更为显著,且正韵律居多;坡度陡、物源足造就了扇三角洲“砂体发育而分布局限、切割叠置频繁”的沉积响应特点,辫状河三角洲则因坡度中等且物源供给弱而具有“砂体薄而广布、多为孤立式接触”的响应特点。

关键词: 扇三角洲, 辫状河三角洲, 沉积记录, 克上组, 三叠系, 红山嘴地区, 准噶尔盆地

Abstract: The recognization of fan delta and braided-river delta of the Upper Karamay Formation in Hongshanzui area in Junggar Basin has always been concerning the geologists in the field of hydrocarbon sedimentology. Depositional analysis based on lithofacies supplemented by the macroscopic distribution mode of sandbody is helpful for distinguishing the two kinds of deltas. Cross-bedded conglomerate lithofacies(Gi,Gt,Gp)and massive gravel lithofacies(Gmm,Gcm,Gcs)were developed in fan delta,with sandy lithofacies(St,Sp,Sm and Sh, etc.)developed in braided-river delta in Hongshanzui area. Debris flows and density flows were indicated by six lithofacies associations in fan delta system,with unobvious rhythm feature. Seven lithofacies associations in braided-river delta show that the traction currents and positive rhythm feature are more significant. Steep slope and abundant sediments contributed to a thick stacked sandbody with limited distribution in the fan delta system. Gentle slope,insufficient sediments supply caused a thin sandbody with board distribution in the braided-river delta,mainly showing isolated contacts between the sandbodies.

Key words: fan delta, braided-river delta, sedimentary records, Upper Karamay Formation, Triassic, Hongshanzui area, Junggar Basin

中图分类号:

P588.21

高阳, 于兴河, 曾大乾, 姚宗全, 刘文峰, 杨新涛. 准噶尔盆地红山嘴地区三叠系克上组两类粗粒三角洲的沉积记录差异及其成因^*[J]. 古地理学报, 2018, 20(6): 973-988.

Gao Yang, Yu Xing-He, Zeng Da-Qian, Yao Zong-Quan, Liu Wen-Feng, Yang Xin-Tao. Differences in sedimentary records of different coarse-grained deltas and their genesis in the Triassic Upper Karamay Formation,Hongshanzui area,Junggar Basin[J]. JOPC, 2018, 20(6): 973-988.

http://www.gdlxb.cn/CN/Y2018/V20/I6/973

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准噶尔盆地红山嘴地区三叠系克上组两类粗粒三角洲的沉积记录差异及其成因^*

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准噶尔盆地红山嘴地区三叠系克上组两类粗粒三角洲的沉积记录差异及其成因*

Differences in sedimentary records of different coarse-grained deltas and their genesis in the Triassic Upper Karamay Formation,Hongshanzui area,Junggar Basin

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准噶尔盆地红山嘴地区三叠系克上组两类粗粒三角洲的沉积记录差异及其成因^*