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塔里木盆地西南地区和田古隆起改造过程及其地质意义

刘士林 邓铭哲 蔡芃睿 曹日洲 周雨双 沙旭光

石油实验地质2025,Vol.47Issue(3):466-478,13.
石油实验地质2025,Vol.47Issue(3):466-478,13.DOI:10.11781/sysydz2025030466

塔里木盆地西南地区和田古隆起改造过程及其地质意义

Transformation processes of Hetian paleo-uplift in southwestern Tarim Basin and its geological significance

刘士林 1邓铭哲 2蔡芃睿 2曹日洲 2周雨双 2沙旭光3

作者信息

  • 1. 中国石化 油田勘探开发事业部,北京 100728
  • 2. 中国石化 石油勘探开发研究院 无锡石油地质研究所,江苏 无锡 214126
  • 3. 中国石化 西北油气分公司,乌鲁木齐 130062
  • 折叠

摘要

Abstract

The southwestern Tarim Basin experienced a complex construction and transformation process during the Paleozoic era.The unclear understanding of the superimposed transformation processes of the paleo-uplifts has restricted its oil and gas exploration.To address this issue,a series of studies,including seismic interpretation and structural analysis,were carried out based on the latest seismic and drilling data.The variation process of denudation was restored in different layers and periods,and the formation and transformation processes of the Hetian paleo-uplift were characterized.Based on the analysis of the ages and formation environments of basin-margin igneous rocks,the dynamic mechanism of the evolution and transformation of the paleo-uplift was discussed.Combined with the oil and gas exploration results,the controlling effects of the superimposed transformation of the paleo-uplifts were discussed.The results indicated that:(1)The denudation center in the southwestern Tarim Basin has undergone significant migration.During stageⅠof the middle Caledonian period,denudation was confined to the southwestern margin of the basin.By stage Ⅲ of the middle Caledonian period,the denudation area expanded northward.During the early Hercynian period,the denudation center migrated eastward.In the late Hercynian period,it was located in the northwestern part of the basin.During the Himalayan period,the denudation center was located in the area where the present Bachu Uplift is situated.(2)The Hetian paleo-uplift exhibited a two-stage evolutionary pattern.It was an uplift along continental margins during stageⅢof the middle Caledo-nian period and then transformed into an intracontinental uplift during the early Hercynian period.The Hetian paleo-uplift was mainly affected by the transformation of the western Maigaiti paleo-uplift in the northwestern margin of the Tarim Basin and the Bachu Uplift in the central basin,which adjusted the early paleogeomorphology of the Hetian paleo-uplift.(3)The migration and evolution of the paleo-uplift and the superimposed transformation between different paleo-uplifts controlled the distribution of different reservoir and caprock assemblages.The structural hinge zones between the Hetian,the western Maigaiti,and the Bachu paleo-uplifts were identified as favorable areas for oil and gas accumulation and should be the focus of future exploration efforts.

关键词

油气聚集/古隆起演化/不整合面/剥蚀量恢复/寒武纪/和田地区/塔里木盆地

Key words

oil and gas accumulation/paleo-uplift evolution/unconformity surface/denudation recovery/Cambrian/Hetian area/Tarim Basin

分类

石油、天然气工程

引用本文复制引用

刘士林,邓铭哲,蔡芃睿,曹日洲,周雨双,沙旭光..塔里木盆地西南地区和田古隆起改造过程及其地质意义[J].石油实验地质,2025,47(3):466-478,13.

基金项目

国家自然科学基金企业创新发展联合基金"三大盆地深层—超深层海相油气高效勘探开发基础研究"(U24B6001)资助. (U24B6001)

石油实验地质

OA北大核心

1001-6112

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