摘要
为明确位于新疆北部的布尔津盆地的资源状况,以实际采集数据为基础,采用建场测深法成果剖面研究了该盆地的地层地质结构,并对深层油气及浅部砂岩型铀矿进行评价。通过利用已知测井电阻率曲线模拟计算不同深度的电磁信号频率响应,论证了该方法探测从浅层第三系到深部石炭系的采集参数和工作方案;在数据处理成果的基础上,结合研究区已知地层物性特征,推断沿线的地质结构,揭示了布尔津凹陷的结构及下二叠统卡拉岗组、上石炭统哈尔加乌组、上石炭统恰其海组地层的分布,认为哈尔加乌组是本区有潜力的烃源岩。同时利用电阻率及双频相位属性对研究区浅部第三系砂岩型铀成矿条件进行分析,其结果与附近已知矿点情况吻合。本文提出的方法可为类似地区进行多种矿产资源勘探提供技术参考。
In order to determine the resource status of the Buerjin Basin in northern Xinjiang,this work studied the stratigraphic geological structures of this basin on the basis of actual collected data,and evaluated the deep oil and shallow sandstone-type uranium deposit.Known logging resistivity curves were utilized to simulate and calculate the electromagnetic signal frequency response at different depths,and the acquisition parameters and working scheme of this method for probing from shallow Tertiary to deep Carboniferous were demonstrated.On the basis of the data processing and the known stratigraphic physical characteristics of the study area,the geological structures along the line were inferred,which reveal the structures of the Buerjin Depression and the distribution of the Lower Permian Kalagang Formation,Upper Carboniferous Harjiawu Formation and Upper Carboniferous Chaiqihai Formation.The Harjiawu Formation is inferred to be a potential source rock in this area.The metallogenic conditions of Tertiary sandstone-type uranium in the shallow part of the study area were analyzed by resistivity and dual-frequency phase attributes.The results are in agreement with the known ore spots nearby.This proposed method provides technical reference for the exploration of various mineral resources in other areas.
作者
白诗筠
米晓利
杨俊
朱永山
张生
BAI Shiyun;MI Xiaoli;YANG Jun;ZHU Yongshan;ZHANG Sheng(BGP of CNPC,Zhuozhou,Hebei 072751)
出处
《地质与勘探》
CAS
CSCD
北大核心
2023年第5期1054-1064,共11页
Geology and Exploration
基金
中国石油天然气股份有限公司科学研究与技术开发项目(编号:2021DJ5303)资助。
关键词
建场测深法
油铀兼探
电阻率
双频相位
烃源岩
铀矿
布尔津盆地
新疆
field sounding method
oil-uranium joint exploration
resistivity
dual-frequency phase
source rocks
uranium deposit
Buerjin Basin
Xinjiang