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    巴布亚湾两期前陆盆地叠置结构及其形成演化

    王德良 梅廉夫 胡孝林 杨松岭 吴路路 刘昭茜 杨焓 苏珈毅

    王德良, 梅廉夫, 胡孝林, 杨松岭, 吴路路, 刘昭茜, 杨焓, 苏珈毅, 2021. 巴布亚湾两期前陆盆地叠置结构及其形成演化. 地球科学, 46(2): 405-417. doi: 10.3799/dqkx.2020.022
    引用本文: 王德良, 梅廉夫, 胡孝林, 杨松岭, 吴路路, 刘昭茜, 杨焓, 苏珈毅, 2021. 巴布亚湾两期前陆盆地叠置结构及其形成演化. 地球科学, 46(2): 405-417. doi: 10.3799/dqkx.2020.022
    Wang Deliang, Mei Lianfu, Hu Xiaolin, Yang Songling, Wu Lulu, Liu Zhaoqian, Yang Han, Su Jiayi, 2021. Superimposed Structure and Evolution of Two-Stage Foreland Basin in Gulf of Papua. Earth Science, 46(2): 405-417. doi: 10.3799/dqkx.2020.022
    Citation: Wang Deliang, Mei Lianfu, Hu Xiaolin, Yang Songling, Wu Lulu, Liu Zhaoqian, Yang Han, Su Jiayi, 2021. Superimposed Structure and Evolution of Two-Stage Foreland Basin in Gulf of Papua. Earth Science, 46(2): 405-417. doi: 10.3799/dqkx.2020.022

    巴布亚湾两期前陆盆地叠置结构及其形成演化

    doi: 10.3799/dqkx.2020.022
    基金项目: 

    国家科技重大专项 2016ZX05026-003-001

    详细信息
      作者简介:

      王德良(1991-), 男, 博士, 主要从事含油气盆地构造分析.ORCID: 0000-0001-8486-2684.E-mail: wdlcug@163.com

      通讯作者:

      梅廉夫, ORCID: 0000-0002-1531-5748.E-mail: lfmei@cug.edu.cn

    • 中图分类号: P548

    Superimposed Structure and Evolution of Two-Stage Foreland Basin in Gulf of Papua

    • 摘要: 巴布亚湾受澳大利亚板块与太平洋板块高速斜向汇聚的控制,经历了复杂的中、新生代构造演化.前人对巴布亚湾盆地结构构造特征的研究多是局部的、分散的,关于盆地的形成时间和动力学机制仍存在争议.利用覆盖全盆的钻井约束的高精度2D、3D地震资料,精细地刻画了盆地的结构和构造特征,揭示了巴布亚湾发育潘多拉和奥雷两期叠置的前陆盆地.潘多拉前陆盆地是形成于渐新世不整合面之上的晚渐新世-中中新世微型前陆盆地,走向为NNE.奥雷前陆盆地是发育在复杂的裂谷边缘之上的早中新世-现今的周缘前陆盆地,沿着弧形的巴布亚半岛延伸480 km;盆地走向在148°E发生转变,由西部的NW向转为东部的近EW向.潘多拉微前陆盆地被奥雷前陆盆地向南逐渐超覆的沉积地层覆盖,两个前陆盆地走向相互垂直,垂向上形成叠置结构.阐明了巴布亚湾新生代经历三期挤压事件及两期叠置的前陆盆地的形成演化,解决了盆地结构及区域构造演化认识的不足,理清了复杂陆缘环境从伸展到挤压多期构造事件的时序及动力学机制,为澳大利亚板块北缘的板块构造重建提供了盆内证据.

       

    • 图  1  巴布亚东部区域构造背景

      Fig.  1.  Regional tectonic setting of eastern Papua

      图  2  巴布亚湾盆地地层综合柱状图

      岩性据Ott and Mann (2015)Bulois et al.(2018)

      Fig.  2.  Simplified stratigraphic column of the basin in the Gulf of Papua

      图  3  奥雷前陆盆地纵剖面(剖面位置见图 1

      Fig.  3.  Longitudinal sections of the Aure foreland basin(the location see Fig.1)

      图  4  潘多拉微前陆盆地横剖面(剖面位置见图 1

      Fig.  4.  Cross sections of the Pandora micro-foreland basin(the location see Fig.1)

      图  5  奥雷前陆盆地横剖面(剖面位置见图 1

      Fig.  5.  Cross sections of the Aure foreland basin(the location see Fig.1)

      图  6  褶皱化裂陷层序2D地震剖面(剖面位置见图 1

      Fig.  6.  2D seismic section of foldable rifting sequence/formation(the location see Fig.1)

      图  7  巴布亚湾走滑体系构造图(前陆盆地基底顶界面)

      Fig.  7.  Structural map of the strike-slip system in the Gulf of Papua (top-basement interface of foreland basin)

      图  8  巴布亚东部古新世-早中新世构造演化图

      Fig.  8.  Tectonic reconstruction of eastern Papua from the Paleocene to Early Miocene

      图  9  巴布亚湾两期前陆盆地叠置结构及其形成过程示意图

      Fig.  9.  Schematic map of the superimposed structure and formation process of two-stage foreland basin in the Gulf of Papua

      图  10  新几内亚晚渐新世碰撞示意图

      Pigram and Symonds(1993)修改

      Fig.  10.  Schematic map of New Guinea during the collision in the Late Oligocene

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    • 收稿日期:  2019-12-29
    • 刊出日期:  2021-02-15

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