综述与评述

苏门答腊弧后盆地特征及其油气勘探进展

  • 周增园 ,
  • 朱伟林 ,
  • 彭文绪 ,
  • 孙和风 ,
  • 付晓伟 ,
  • 赵世杰 ,
  • 冯凯龙
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  • 1.同济大学海洋地质国家重点实验室,上海 200092
    2.同济大学海洋资源研究中心,上海 200092
    3.中国海洋石油国际有限公司,北京 100027
周增园,博士研究生,主要从事东南亚地区石油地质研究. E-mail:zhou_zengyuan@tongji.edu.cn
朱伟林,教授,主要从事海域构造地质及石油地质研究. E-mail:zhuwl@tongji.edu.cn

收稿日期: 2023-11-27

  修回日期: 2024-02-14

  网络出版日期: 2024-04-01

基金资助

国家自然科学基金(92055203);国家留学基金委(CSC)项目(202306260234)

Progress of Hydrocarbon Exploration and Characteristics of the Petroliferous Basin in the Sumatra Back-arc Area

  • Zengyuan ZHOU ,
  • Weilin ZHU ,
  • Wenxu PENG ,
  • Hefeng SUN ,
  • Xiaowei FU ,
  • Shijie ZHAO ,
  • Kailong FENG
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  • 1.State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China
    2.Research Center for Marine Resources, Tongji University, Shanghai 200092, China
    3.CNOOC International Limited, Beijing 100027, China
ZHOU Zengyuan, Ph. D student, research areas include petroleum geology in Southeast Asia. E-mail: zhou_zengyuan@tongji.edu.cn
ZHU Weilin, Professor, research areas include marine structural geology and petroleum geology. E-mail: zhuwl@tongji.edu.cn

Received date: 2023-11-27

  Revised date: 2024-02-14

  Online published: 2024-04-01

Supported by

the National Natural Science Foundation of China(92055203);The China Scholarship Fund(202306260234)

摘要

苏门答腊盆地群是东南亚典型的弧后盆地,也是印度尼西亚第一大油气富集区,近5年发现新增油气储量呈上升趋势,待发现资源量大,具有较大的勘探潜力。通过系统梳理苏门答腊盆地群油气勘探历史、主要油气资源分布和盆地构造演化特征,分析了苏门答腊弧后盆地油气分布差异性及其主控因素。油气的不均一分布格局,主要受控于断陷期烃源岩的差异性分布,断陷期的“三阶段”构造演化过程控制不同类型的沉积环境及沉积相分布,进而影响主力烃源岩的分布;其次,地壳拉张变薄以及岩浆作用促使弧后地区浅层形成较高热流值,加速烃源岩的热解生烃。结合苏门答腊弧后盆地群油气勘探历史及其待发现油气资源量,认为苏门答腊盆地北部Andaman Ⅲ PSC区块等深水区、南苏门答腊盆地源下基底潜山新层系以及中苏门答腊盆地的陆上低程度勘探地区是下一步研究的新领域。

本文引用格式

周增园 , 朱伟林 , 彭文绪 , 孙和风 , 付晓伟 , 赵世杰 , 冯凯龙 . 苏门答腊弧后盆地特征及其油气勘探进展[J]. 地球科学进展, 2024 , 39(3) : 232 -246 . DOI: 10.11867/j.issn.1001-8166.2024.020

Abstract

The Sumatera Basin Group is a typical back-arc basin in Southeast Asia and is the largest oil and gas enrichment area in Indonesia. In the past five years, it has been found that the new oil and gas reserves are on the rise, and the amount of resources to be discovered is large, which has great exploration potential. This study systematically sorts out the hydrocarbon exploration history, main oil and gas resource distribution, and basin tectonic evolution characteristics of the Sumatra Basin group and analyzes the differences in oil and gas distribution and its main controlling factors in the back-arc basin of Sumatra. The uneven distribution patterns of oil and gas were mainly controlled by the differential distribution of source rocks during the fault depression period. The three-stage tectonic evolution during the fault depression period controlled the distribution of sedimentary facies in different types of sedimentary environments, which in turn affected the distribution of the main source rocks. Secondly, crustal tension thinning and magmatism promoted the formation of high heat flow values in the shallow layer of the back-arc area, which accelerated the pyrolysis of the hydrocarbon source rocks. Combined with the oil and gas exploration history of the back-arc basin group in Sumatra and the amount of oil and gas resources to be discovered, it is considered that deep-water areas, such as the Andaman III PSC block in the northern part of the Sumatra Basin, the new strata of the basement buried hill under the source of the South Sumatra Basin, and the low exploration degree areas on land in the Central Sumatra Basin are new areas for the next mature basin exploration.

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