摘要
克百断槽始于克拉玛依市北的克北断裂,NE向延伸并被大侏罗沟断裂、盆缘断裂、克-百断裂围限。火山岩储层是该断槽内的主要储层,其层位时代无据、层序不清、归属不明。笔者通过对克百断槽古66井242.14~800.18 m井段详细的岩心编录、测井曲线岩电识别及关键层位火山岩锆石U-Pb年代学研究,结果表明:古66井242.14~800.18 m井段是被两层陆源粗碎屑岩(标志层)分隔的3套火山岩建造,于玄武安山岩中获得(304±3)Ma和(303±2)Ma的LA-ICP-MS锆石U-Pb年龄,其岩石组合、时代、层序、地层厚度均与井北缘哈山一带哈拉阿拉特组建组剖面C_(2)h^(1)~C_(2)h^(3)岩段总体可对比。古66井所处的克百断槽是一个四周被断层围限的相对独立火山岩型储层断槽油气藏,这一油气藏新类型丰富了西准噶尔盆内油气藏类型。同时,该断槽具有向南西延伸的构造条件、储层类型和圈闭样式,因而是后续扩大油气勘探的新靶区。
The Kebai fault-trough originates from the Kebei fault at the southwest end and extends northeastward,intersected by the Dazhuluogou fault,which begins in the northern region of Karamay City.It is bounded by the basin-edge fault on its northwest edge and the Kebai fault on its southeast edge.The primary reservoirs within this fault-trough are composed of volcanic rock.However,the stratigraphic allocation,age,and sequence of these volcanic rocks remain uncertain.This study employs a comprehensive approach involving detailed core logging,lithodensity identification using well logging curves,and zircon U-Pb dating of key volcanic rock layers within the interval of 242.14~800.18 m in the well Gu 66,located within the Kebai fault-trough.The results of our investigation reveal the following insights:The interval from 242.14~800.18 m in the well Gu 66 encompasses three distinct sets of volcanic rock formations,interspersed by two layers of terrestrial clastic rocks functioning as marker beds.Through zircon LA-ICP-MS U-Pb dating,we determined ages of 304±3 Ma and 303±2 Ma for the andesite in the well Gu 66.The rock composition,ages,stratigraphy,and thickness of these formations show notable similarity to the C_(2)h^(1)~C_(2)h^(3) sections of the Hala’alate Formation profile situated in the northern edge of the Hashan region.The Kebai fault-trough,hosting the well Gu 66,represents a distinctive faulttrough characterized by volcanic rock reservoirs,enclosed by surrounding fault structures.This novel type of hydrocarbon reservoir expands the repertoire of oil and gas reservoir types found in the western Junggar.Furthermore,the fault-trough exhibits structural attributes,reservoir characteristics,and trap styles that extend southwestward,rendering it a promising new target area for forthcoming oil and gas exploration.
作者
王玉伟
李永军
王盼龙
王韬
黄家瑄
张新远
郑孟林
张越迁
WANG Yuwei;LI Yongjun;WANG Panlong;WANG Tao;HUANG Jiaxuan;ZHANG Xinyuan;ZHENG Menglin;ZHANG Yueqian(Xinjiang Oilfield Exploration Division,Xinjiang Oilfield Company,PetroChina,Karamay 834000,Xinjiang,China;Research Institute of Exploration and Development,Xinjiang Oilfield Company,PetroChina,Karamay 834000,Xinjiang,China;School of Earth Science and Resources,Chang’an University,Xi’an 710054,Shaanxi,China)
出处
《西北地质》
CAS
CSCD
北大核心
2024年第5期209-223,共15页
Northwestern Geology
基金
国家科技重大专项“新疆北部深层区域构造格架、沉积演化与有利区带评价”(2017ZX05008-006-003-001)
国家重点研发计划“深地资源勘查开采重点专项”(2018YFC060400)
中国石油天然气股份有限公司科学研究与技术开发项目“北疆海相泥盆-石炭系油气地质研究”(2022DJ0507)
中石油前瞻性基础研究项目“地层不整合油气藏成藏主控因素与关键要素定量评价技术研究”(2021DJ0405)联合资助。
关键词
克百断槽
古66井
火山岩储层
地质时代
盆-山地层对比
Kebai fault-trough
well Gu 66
volcanic reservoir
geological age
basin-mountain sequence comparison
