准噶尔盆地滴北凸起早石炭世沉积充填特征及油气地质意义<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2019.04.042

古地理学报 ›› 2019, Vol. 21 ›› Issue (4): 637-646. doi: 10.7605/gdlxb.2019.04.042

• 岩相古地理学及沉积学 • 上一篇下一篇

准噶尔盆地滴北凸起早石炭世沉积充填特征及油气地质意义^*

黄芸¹, 梁舒艺², 夏雨¹, 李艳平¹, 谷新萍¹, 伏小鹏¹

1 新疆油田公司勘探开发研究院,新疆乌鲁木齐 830013;
2 中国石油大学(华东)地球科学学院,山东青岛 266580

收稿日期:2018-10-15 修回日期:2018-11-23 出版日期:2019-08-01 发布日期:2019-07-23
作者简介:黄芸,女,1969年生,高级工程师,1989年毕业于西北大学地质学系,现主要从事油气勘探工作。E-mail: huangyun@petroChina.com.cn。
基金资助:
*国家重点基础研究发展规划“973”项目(编号: 2009CB219304)资助

Sedimentary filling characteristics and petroleum geologic significance of the Early Carboniferous in Dibei uplift,Junggar Basin

Huang Yun¹, Liang Shu-Yi², Xia Yu¹, Li Yan-Ping¹, Gu Xin-Ping¹, Fu Xiao-Peng¹

1 Research Institute of Exploration and Development,Xinjiang Oilfield Company,Ürümqi 830013,China;
2 School of Geosciences,China University of Petroleum(East China),Qingdao 266580,China

Received:2018-10-15 Revised:2018-11-23 Online:2019-08-01 Published:2019-07-23
About author:About the first author Huang Yun,born in 1969,senior engineer, graduated from Northwest University in 1989. She is mainly engaged in petroleum exploration. E-mail: huangyun@petroChina.com.cn.
Supported by:
Financially supported by the National Basic Research Development Plan “973” Project(No. 2009CB219304)

摘要/Abstract

摘要： 利用钻井、测井、地震、古生物及地化分析资料,研究了准噶尔盆地滴北凸起早石炭世构造环境、沉积充填特征及其油气地质意义。结果表明,滴北凸起早石炭世发育半地堑式伸展断陷,发育海相复理石建造并发育海底火山喷发岩,具备烃源岩的发育环境。泉5井最新的地化分析表明,该区烃源岩发育且成熟度高,为好—较好烃源岩;这个结果改写了滴北凸起石炭系烃源岩成熟度低、无勘探潜力的认识。依据克拉美丽气田“近源隆控”的成熟勘探模式,提出滴北凸起发育“源储一体”和“近源隆控”2种模式,明确了有利勘探区带。

关键词: 准噶尔盆地, 滴北凸起, 早石炭世, 复理石相, 油气地质意义

Abstract: This paper studies the tectonic setting,sedimentary filling characteristics and the petroleum geologic significance of the Early Carboniferous deposits in Dibei uplift,Junggar Basin,based on the datasets consisted of drilling,logging,seismic,paleontology,and geochemical data. It is suggested that during the Early Carboniferous Dibei uplift developed half-garben stretching rift and was characterized by the marine flysch and volcanic facies,which make it suitable for the occurrence of the hydrocarbon source rock. Based on the latest geochemical study of Well Quan 5,Dibei uplift has the source rock with high maturity,i.e. good source rocks. Such geological understanding breaks the original one that the Carboniferous source rocks of Dibei uplift is low-maturity and has no exploration potential. According to the mature exploration model of “near source and uplift controls”in Kalameili gas-field,this paper proposes two hydrocarbon accumulation patterns in Dibei uplift: “source and reservoir integration”and “near source and uplift controls”,which clears the favorable exploration zone.

Key words: Junggar Basin, Dibei uplift, Early Carboniferous, flysch facies, petroleum geologic significance

中图分类号:

TE121.3+1

黄芸, 梁舒艺, 夏雨, 李艳平, 谷新萍, 伏小鹏. 准噶尔盆地滴北凸起早石炭世沉积充填特征及油气地质意义^*[J]. 古地理学报, 2019, 21(4): 637-646.

Huang Yun, Liang Shu-Yi, Xia Yu, Li Yan-Ping, Gu Xin-Ping, Fu Xiao-Peng. Sedimentary filling characteristics and petroleum geologic significance of the Early Carboniferous in Dibei uplift,Junggar Basin[J]. JOPC, 2019, 21(4): 637-646.

http://www.gdlxb.cn/CN/Y2019/V21/I4/637

参考文献

[1] 陈世加,陈雪,路俊刚,陆林超,杨国平,王熠. 2011. 准噶尔盆地滴北凸起天然气来源及成藏特征. 天然气地球科学, 22(1): 97-101
[Chen S J,Chen X,Lu J G,Lu L C,Yang G P,Wang Y.2011. Characteristics of natural gas sources and accumulation in Dibei Uplift of Junggar Basin. Natural Gas Geoscience, 22(1): 97-101]
[2] 董雪梅,徐怀民,贺陆明,任军民,吴静. 2012. 克拉美丽石炭系火山岩气田的高效勘探开发. 新疆石油地质, 33(2): 214-217.
[Dong X M,Xu H M,He L M,Ren J M,Wu J.2012. Efficient exploration and development of Carboniferous volcanic gas field in Kelameili Area in Junggar Basin. XinJiang Petroleum Geology, 33(2): 214-217]
[3] 何国琦,李茂松,贾进斗. 2001. 论新疆东准噶尔蛇绿岩的时代及其意义. 北京大学学报(自然科学版), 37(6): 852-858.
[He G Q,Li M S,Jia J D.2001. A discussion on age and tectonic significance of Ophiolite in Eastern Junggar,Xinjiang. Acta Scientiarum Naturalium Universitatis Pekinensis, 37(6): 852-858]
[4] 晋慧娟,李育慈,李菊英. 1989. 新疆北天山中石炭统的复理石相. 沉积学报, 7(1): 51-56.
[Jin H J,Li Y C,Li J Y.1989. The Flysch facies of Middle Carboniferous in the Northern Tianshan,XinJiang. Acta Sedimentologica Sinica, 7(1): 51-56]
[5] 李涤,何登发,樊春,唐勇,阳孝法,常秋生,袁航. 2012a. 准噶尔盆地克拉美丽气田石炭系玄武岩的地球化学特征及构造意义. 岩石学报, 28(3): 981-992.
[Li D,He D F,Fan C,Tang Y,Yang X F,Chang Q S,Yuan H.2012a. Geochemical characteristics and tectonic significance of Carboniferous basalt in the Karameili gas field of Junggar Basin. Acta Petrologica Sinica, 28(3): 981-992]
[6] 李涤,何登发,唐勇,樊春,孔玉华. 2012b. 准噶尔盆地滴南凸起早石炭世火山岩的成因及其对克拉美丽洋闭合时限的约束. 岩石学报, 28(8): 2340-2354.
[Li D,He D F,Tang Y,Fan C,Kong Y H.2012b. Genesis of Early Carboniferous volcanic rocks of the Di’nan uplift in Junggar Basin: Constraints to the closure time of Kalamaili ocean.Acta Petrologica Sinica, 28(8): 2340-2354]
[7] 李锦轶,杨天南,李亚萍,朱志新. 2009. 东准噶尔卡拉麦里断裂带的地质特征及其对中亚地区晚古生代洋陆格局重建的约束. 地质通报, 28(12): 1817-1826.
[Li J Y,Yang T N,Li Y P,Zhu Z X.2009. Geological features of the Karamaili faulting belt,eastern Junggar region,Xinjiang,China and its constraints on the reconstruction of Late Paleozoic ocean-continental framework of the Central Asian region. Geological Bulletin of China, 28(12): 1817-1826]
[8] 李林,夏惠平,陈世加,陆俊刚,夏青. 2010. 准噶尔盆地滴北凸起天然气成因及成藏特征. 新疆石油地质, 31(4): 352-355.
[Li L,Xia H P,Chen S J,Lu J G,Xia Q.2010. Natural gas origin and its accumulation feature in Dibei Swell in Junggar Basin. Xinjiang Petroleum Geology, 31(4): 352-355]
[9] 李艳平,黄芸,袁波,冀冬生. 2016. 卡拉麦里山前石炭系火山岩序列层位归属及分布研究. 新疆地质, 34(4): 518-519.
[Li Y P,Huang Y,Yuan B,Ji D S.2016. Study on the ownership and distribution of volcano rock sequence of Carboniferous at Kelameili Piedmont. XinJiang Geology, 34(4): 518-519]
[10] 李增田. 1990. 细碧岩成因综述. 地质科技情报, 9(1): 19-24.
[Li Z T.1990. Review on geneses of spilite. Geological Science and Technology Information, 9(1): 19-24]
[11] 舒良树,王玉净. 2003. 新疆卡拉麦里蛇绿岩带中硅质岩的放射虫化石. 地质论评, 49(4): 408-412.
[Shu L S,Wang Y J.2003. Early carboniferous radiolarian fossils from siliceous rocks of the Kelameili Ophiolite,XinJiang. Geological Review, 49(4): 408-412]
[12] 汪帮耀,姜常义,李永军,吴宏恩,夏昭德,卢荣辉. 2009. 新疆东准噶尔卡拉麦里蛇绿岩的地球化学特征及大地构造意义. 矿物岩石, 29(3): 74-82.
[Wang B Y,Jiang C Y,Li Y J,Wu H E,Xia Z D,Lu R H.2009. Geochemistry and tectonic implication of Karamali ophiolite in east Junggar of Xinjiang. Journal of Mineralogy and Petrology, 29(3): 74-82]
[13] 王启宇,牟传龙,陈小炜,康建威. 2014. 准噶尔盆地及周缘地区石炭系岩相古地理特征及油气基本地质条件. 古地理学报,16(5),655-671.
[Wang Q Y,Mu C L,Chen X W,Kang J W.2014. Palaeogeographic characteristics and basic geological conditions of petroleum of the Carboniferous in Junggar Basin and its adjacent areas. Journal of Palaeogeography(Chinese Edition),16(5),655-671]
[14] 吴小奇,刘德良,魏国齐,李剑,李振生. 2009. 准噶尔盆地陆东—五彩湾地区石炭系火山岩地球化学特征及其构造背景. 岩石学报, 25(1): 55-66.
[Wu X Q,Liu D L,Wei G Q,Li J,Li Z S.2009. Geochemical characteristic and tectonic settings of Carboniferous volcanic rocks from Ludong-Wucaiwang area,Junggar Basin.Acta Petrologica Sinica, 25(1): 55-66]
[15] 余腾孝,曹自成,徐勤琪,潘泉涌,薛会,刘士林,解国军. 2010. 准噶尔盆地北部古生代构造演化与石炭系烃源岩. 石油与天然气地质, 31(1): 91-97.
[Yu T X,Cao Z C,Xu Q Q,Pan Q Y,Xue H,Liu S L,Xie G J.2010. The Paleozoic tectonic evolution and the Carboniferous source rocks in the northen Junggar Basin. Oil & Gas Geology, 31(1): 91-97]
[16] 赵恒乐,许凡,张冀,杨屹. 2012. 东准噶尔卡拉麦里蛇绿岩形成时代、地质特征及构造意义. 新疆地质, 30(2): 161-164.
[Zhao H L,Xu F,Zhang J,Yang Y.2012. The Kalamaili Ophiolites: Age,geological characteristics and tectonic significance. Xinjiang Geology, 30(2): 161-164]
[17] 赵霞,贾承造,张光亚,卫延召,赖绍聪,方向,张丽君. 2008. 准噶尔盆地陆东—五彩湾地区石炭系中、基性火山岩地球化学及其形成环境. 地学前缘, 15(2): 272-279.
[Zhao X,Jia C Z,Zhang G Y,Wei Y Z,Lai S C,Fang X,Zhang L Q.2008. Geochemistry and tectonic settings of Carboniferous intermediate-basic volcanic rocks in Ludong-Wucaiwan,Junggar Basin. Earth Science Frontiers, 15(2): 272-279]

选择文件类型/文献管理软件名称

选择包含的内容

准噶尔盆地滴北凸起早石炭世沉积充填特征及油气地质意义^*

Sedimentary filling characteristics and petroleum geologic significance of the Early Carboniferous in Dibei uplift,Junggar Basin

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	周勇, 梁涛, 赵祥宇, 纪友亮, 王剑, 卢轶伦, 陈俊, 严可欣. 火山岩不同喷发环境识别标志及喷发模式: 以准噶尔盆地东部石炭系为例^*[J]. 古地理学报, 2025, 27(2): 423-445.
[2]	刘惠民, 文华国, 张奎华, 郭佩, 张关龙, 于洪洲, 熊伟, 周健, 徐文礼, 宋梅远, 李长志. 准噶尔盆地西北缘哈山地区风城组碱湖页岩油地质特征与勘探展望^*[J]. 古地理学报, 2024, 26(5): 1017-1036.
[3]	郭文建, 郭瑞婧, 唐勇, 纪友亮, 马铮涛, 刘笑语, 梁涛, 马玉龙. 准噶尔盆地二叠系上乌尔禾组退覆式扇(辫状河)三角洲前缘-滩坝复合砂砾岩沉积特征及控制因素^*[J]. 古地理学报, 2024, 26(3): 584-599.
[4]	甄宇, 陈旋, 焦立新, 李新宁, 周志超, 刘文辉, 殷树铮, 李涤, 苟红光, 李成明, 何登发. 东疆地区石炭纪—二叠纪构造古地理与原型盆地演化^*[J]. 古地理学报, 2024, 26(1): 78-99.
[5]	殷树铮, 郭文建, 李新宁, 周志超, 刘文辉, 焦立新, 何登发. 准噶尔盆地西部坳陷带二叠系构造-地层层序与盆地演化^*[J]. 古地理学报, 2024, 26(1): 132-149.
[6]	焦国华, 张卫平, 谢利华, 王军, 周晋科, 汪云海. 准噶尔盆地南部下侏罗统三工河组沉积体系及其控制因素^*[J]. 古地理学报, 2023, 25(3): 628-647.
[7]	焦悦, 吴朝东, 王家林, 焦国华, 张卫平, 关旭同. 天山东段地区二叠系芦草沟组沉积特征与古环境对比^*[J]. 古地理学报, 2023, 25(2): 277-293.
[8]	吴晨骁, 姚宗全, 德勒恰提·加娜塔依, 邓高山, 李天明, 赫佳, 刘宇, 王小红, 曙格拉·马哈西. 准噶尔盆地沙湾凹陷西斜坡二叠系佳木河组物源区构造背景分析^*[J]. 古地理学报, 2022, 24(6): 1149-1161.
[9]	黄玉越, 王贵文, 宋连腾, 王松, 张益粼, 黄立良, 赖锦. 准噶尔盆地玛湖凹陷二叠系风城组页岩储集层裂缝测井识别与有效性分析^*[J]. 古地理学报, 2022, 24(3): 540-555.
[10]	高志勇, 石雨昕, 冯佳睿, 周川闽. 砾石在分析盆地物源区迁移与湖岸线演化中的作用^*[J]. 古地理学报, 2021, 23(3): 507-524.
[11]	史燕青, 王剑, 张国一, 刘明, 向鹏飞, 杨志波, 季汉成. 新疆博格达地区中二叠世—早三叠世构造-气候-沉积演化及耦合机制^*[J]. 古地理学报, 2021, 23(2): 389-404.
[12]	桑林翔, 刘军, 王贵文, 王苏天, 李全, 张云龙. 准噶尔盆地玛湖凹陷西斜坡三叠系百口泉组扇三角洲优质储集层预测[J]. 古地理学报, 2020, 22(6): 1053-1064.
[13]	程逸凡, 董艳蕾, 朱筱敏, 杨道庆, 伍炜, 杨棵, 苏彬, 赵瑞星, 乔陈凯. 准噶尔盆地春光探区白垩纪古地貌恢复及其控砂机制[J]. 古地理学报, 2020, 22(6): 1127-1142.
[14]	吴波, 邓克勇, 刘应忠, 徐安全. 贵州龙里地区早石炭世杜内期铝土矿微地貌及其对铝土矿的控制作用^*[J]. 古地理学报, 2020, 22(5): 977-988.
[15]	董艳蕾, 陈祥, 伍炜, 杨道庆, 杨棵, 苏彬, 程逸凡, 左一苇, 赵瑞星, 邹通, 朱筱敏. 准噶尔盆地西北部春光探区白垩系地震沉积学研究^*[J]. 古地理学报, 2020, 22(3): 412-427.

模态框（Modal）标题

选择文件类型/文献管理软件名称

选择包含的内容

准噶尔盆地滴北凸起早石炭世沉积充填特征及油气地质意义*

Sedimentary filling characteristics and petroleum geologic significance of the Early Carboniferous in Dibei uplift,Junggar Basin

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

准噶尔盆地滴北凸起早石炭世沉积充填特征及油气地质意义^*