准噶尔盆地红山嘴北部三叠系克拉玛依组沉积特征

doi:10.16108/j.issn1006-7493.2022024

高校地质学报 ›› 2023, Vol. 29 ›› Issue (5): 776-787.DOI: 10.16108/j.issn1006-7493.2022024

准噶尔盆地红山嘴北部三叠系克拉玛依组沉积特征

王进¹，于兴河^2*，卢凤豪¹，牛小军¹，野兆瑞¹，杨新涛³

1. 河北省煤田地质局新能源地质队，邢台 054000；
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第一采油厂，克拉玛依 834000

出版日期:2023-10-11 发布日期:2023-10-10

Sedimentary Characteristics of the Triassic Karamay Formation in the North Hongshanzui Area, Junggar Basin

WANG Jin¹，YU Xinghe^2*，LU Fenghao¹，NIU Xiaojun¹，YE Zhaorui¹，YANG xintao³

1. New Energy Geological Team, Hebei Provincial Provincal Bureau of Coal Geology, Xingtai 054000, China;
2. School of Energy Resources, China University of Geosciences, Beijing 100083, China;
3. No. 1 Oil Production Plant, Xinjiang Oilfield Company, PetroChina, Karamay 834000, China

Online:2023-10-11 Published:2023-10-10

摘要/Abstract

摘要： 红山嘴北部的克上组与克下组地层存在明显的沉积差异。为明确克拉玛依组沉积特征及成因，利用地震、钻测井、岩心及分析化验等资料，对克拉玛依组的岩矿特征、岩相类型、沉积相类型与展布进行研究。结果表明：克下组为以牵引流为主的辫状河沉积，发育辫状河道（Gi→St→Sp→(Sh)→Md）、心滩（St→Sp↔Sm）及冲积平原（Mr↔Md→Fr），河道砂体呈条带展布，多呈孤立状分布于厚层泥岩中；克上组为碎屑流、洪流与牵引流共同作用下扇三角洲沉积，平原发育辫状河道（Gmm→Gcm→Gi→Sh）、辫状分支河道（Gcm→Gi↔Gt）与辫流坝微相（Gp↔Gi→Gcm），前缘发育水下分流河道（Gi→Gt→Gp→St）、河口坝（Md→Sp↔Sw）及水下分流间湾微相（Md↔Sc），所沉积的厚层砂砾岩体相互切割叠置，连片分布，连通性好。受控于物源体系前移与供给强度的增加、古气候由干旱—半干旱向半湿润—湿润转变及湖平面上升，研究区克拉玛依组经历了由辫状河向扇三角洲转变的沉积演化。

关键词: 辫状河, 扇三角洲, 垂向序列, 沉积演化, 克拉玛依组, 红山嘴北部

Abstract: The obvious sedimentary differences can be found between the upper and lower parts of the Karamay Formation in the north of Hongshanzui. To determine the sedimentary characteristics of the Karamay Formation, the seismic, core logging, and analytical data were used to analyze the rock and mineral characteristics, typical lithofacies, and sedimentary facies of the Karamay Formation. The results show that the lower Karamay Formation is characterized by the braided river deposits with obvious traction-current deposition, which is mainly composed of braided channel (Gi → St → Sp → (Sh) → Md), braided bar (St→Sp↔Sm), and alluvial plain (Mr↔Md → Fr). The channel sand-bodies are banded and mostly isolated from thick mudstone. The upper Karamay Formation is dominated by fan-delta with debris flow, density flow and tractioncurrent deposits. The braided channel (Gmm→Gcm→Gi→Sh), braided distributary channel (Gcm→Gi↔Gt) and braided bar (Gp↔Gi→Gcm) are developed in the fan-delta plain. The underwater distributary channel (Gi→Gt→Gp→St), mouth bar (Md→Sp↔Sw) and interdistributary bay (Md↔Sc) are developed in the fan-delta front. The thick stacked sandy conglomerate bodies are scours and overlap with each other and also characterized by good connectivity and broad distribution. The transformation from the braided river to fan-delta in the Karamay Formation is mainly controlled by the forwarded provenance system and increased supply capacity, the transition of the paleoclimate from arid and semi-arid to sub-humid and humid, and the lake level rise.

Key words: braided river, fan-delta, sedimentary sequences, depositional evolution, Karamay Formation, North Hongshanzui area

中图分类号:

P618

王进, 于兴河, 卢凤豪, 牛小军, 野兆瑞, 杨新涛. 准噶尔盆地红山嘴北部三叠系克拉玛依组沉积特征[J]. 高校地质学报, 2023, 29(5): 776-787.

WANG Jin, YU Xinghe, LU Fenghao, NIU Xiaojun, YE Zhaorui, YANG xintao. Sedimentary Characteristics of the Triassic Karamay Formation in the North Hongshanzui Area, Junggar Basin[J]. Geological Journal of China Universities, 2023, 29(5): 776-787.

[1]	张建民, 秦祎, 郭诚, 崔龙涛, 李卓, 金磊, 王晓雪. 莱州湾凹陷垦利油区沙三上亚段辫状河三角洲沉积特征表征[J]. 高校地质学报, 2021, 27(5): 515-525.
[2]	李峻颉, 侯国伟, 秦兰芝, 谢晶晶, 苗清. 构造转换带制约下的砂体富集效应：以平湖斜坡孔雀亭区平湖组为例[J]. 高校地质学报, 2021, 27(4): 459-468.
[3]	周清波，舒誉，朱筱敏，陈兆明，董小云，林秋金. 珠江口盆地HA地区古近系文昌组沉积特征[J]. 高校地质学报, 2019, 25(4): 558-.
[4]	郭建林，贾成业*，闫海军，季丽丹，李易隆，袁贺. 致密砂岩气藏储渗单元研究方法与应用：以鄂尔多斯盆地二叠系下石盒子组为例[J]. 高校地质学报, 2018, 24(3): 412-.
[5]	吴冬，朱筱敏*，刘常妮，李雨彤. “源-汇”体系主导下的断陷湖盆陡坡带扇三角洲发育模式探讨：以苏丹Muglad盆地Fula凹陷为例[J]. J4, 2015, 21(4): 653-.
[6]	葛家旺，朱筱敏，黄捍东，宋爽，周清波，董小云. 稀疏井区辫状河三角洲地层精细对比: 以惠州凹陷HZ-A油田文昌组为例[J]. J4, 2015, 21(3): 440-.
[7]	余宽宏*，金振奎，李桂仔，何苗，郭秀娟，杨婷. 天山北缘辫状河型洪积扇沉积特征及其对准噶尔盆地西北缘古代洪积扇油气勘探的指导意义[J]. J4, 2015, 21(2): 288-.
[8]	赵东娜，朱筱敏，梁兵，马英俊，薄永德，吴冬，刘芬，孙书洋. 江苏高邮凹陷深凹带古近系戴南组地震沉积学[J]. J4, 2015, 21(2): 336-.
[9]	杨巍 , 张廷山* ，魏国齐，杨威，刘满仓，刘治成. 城口-鄂西海槽西侧晚二叠世碳酸盐台地边缘发育新认识[J]. J4, 2015, 21(1): 79-.
[10]	丁巍伟，黎明碧，何敏，唐勇，方银霞. 南海中北部陆架-陆坡区新生代构造-沉积演化[J]. J4, 2009, 15(3): 339-350.
[11]	林春明，张志萍，李艳丽，岳信东,徐深谋，张霞，漆滨汶,. 二连盆地白音查干凹陷早白垩世腾格尔组沉积特征及物源探讨[J]. J4, 2009, 15(2): 226-239.
[12]	薛新克，岳大力，吴胜和，蒋婷婷，阿布力米提，黄治赳，陈诗波. 准噶尔盆地西北缘六七开发区侏罗系有利目标评价[J]. J4, 2008, 14(2): 276-282.
[13]	曹辉兰，华仁民，纪友亮，胡文瑄，张善文. 扇三角洲砾砾岩储层沉积特征及与储层物性的关系—以罗家油田沙四段砂砾岩体为例[J]. J4, 2001, 7(2): 222-229.

准噶尔盆地红山嘴北部三叠系克拉玛依组沉积特征

Sedimentary Characteristics of the Triassic Karamay Formation in the North Hongshanzui Area, Junggar Basin

PDF (PC)

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 13

编辑推荐

Metrics