首页> 外文期刊>Tectonics >Interactions between continental breakup dynamics and large-scale delta system evolution: Insights from the Cretaceous Ceduna delta system, Bight Basin, Southern Australian margin
【24h】

Interactions between continental breakup dynamics and large-scale delta system evolution: Insights from the Cretaceous Ceduna delta system, Bight Basin, Southern Australian margin

机译:大陆解体动力学与大规模三角洲系统演化之间的相互作用:来自南澳大利亚边缘比特盆地的白垩纪塞杜纳三角洲系统的见解

获取原文
获取原文并翻译 | 示例
           

摘要

The interpretation of two regional seismic reflection profiles and the construction of a balanced cross section through the southern Australian margin (Bight Basin) are designed to analyze the influence of the Australia-Antarctica continental breakup process on the kinematic evolution of the Cretaceous Ceduna delta system. The data show that the structural architecture of this delta system consists of two stacked delta systems. The lower White Pointer delta system (Late Albian-Santonian) is an unstable tectonic wedge, regionally detached seaward above Late Albian ductile shales. Sequential restoration suggests that the overall gravitational sliding behavior of the White Pointer delta wedge (~45 km of seaward extension, I.e., ~27%) is partially balanced by the tectonic denudation of the subcontinental mantle. We are able to estimate the horizontal stretching rate of the mantle exhumation between ~2 and 5 km Ma~(-1). The associated uplift of the distal part of the margin and associated flexural subsidence in the proximal part of the basin are partially responsible for the decrease of the gravitational sliding of the White Pointer delta system. Lithospheric failure occurs at ~84 Ma through the rapid exhumation of the mantle. The upper Hammerhead delta system (Late Santonian-Maastrichtian) forms a stable tectonic wedge developed during initial, slow seafloor spreading and sag basin evolution of the Australian side margin. Lateral variation of basin slope (related to the geometry of the underlying White Pointer delta wedge) is associated with distal raft tectonic structures sustained by high sedimentation rates. Finally, we propose a conceptual low-angle detachment fault model for the evolution of the Australian-Antarctic conjugate margins, in which the Antarctic margin corresponds to the upper plate and the Australian margin to the lower plate.
机译:解释了两个区域地震反射剖面并构造了贯穿澳大利亚南部边缘(Bight盆地)的平衡横截面,以分析澳大利亚-南极洲大陆破碎过程对白垩纪塞杜纳三角洲系统运动学演化的影响。数据表明,此增量系统的结构体系结构由两个堆叠的增量系统组成。较低的白尖三角洲系统(晚阿尔本-桑顿期)是一个不稳定的构造楔,晚阿尔本延性页岩上方的区域性分离海。序贯恢复表明,White Pointer三角楔的整体重力滑动行为(向海延伸约45 km,即约27%)被该次大陆幔的构造剥蚀部分平衡。我们可以估算出〜2至5 km Ma〜(-1)之间的地幔发掘的水平伸展率。边缘远侧部分的相关隆起和盆地近端部分中的相关挠性沉降是部分导致White Pointer三角洲系统重力滑动减小的原因。由于地幔的快速掘出,岩石圈破裂发生在〜84 Ma。上哈默黑德三角洲系统(晚期桑托尼亚-马斯特里赫蒂安)形成了一个稳定的构造楔,在初始,缓慢的海床扩张和澳大利亚侧缘的凹陷盆地演化过程中形成。盆地坡度的横向变化(与下伏的白点三角洲楔形的几何形状有关)与高沉积速率维持的远洋筏构造结构有关。最后,我们为澳大利亚-南极共轭边缘的演化提出了一个概念性的低角度脱离断层模型,其中南极边缘对应于上板块,澳大利亚边缘对应于下板块。

著录项

  • 来源
    《Tectonics》 |2009年第6期|TC6002.1-TC6002.26|共26页
  • 作者单位

    Institut Francais du Petrole, Rueil-Malmaison, France CEREGE, UMR 6635, Aix-Marseille Universite, Europole de l'Arbois, Aix-en-Provence, France;

    Institut Francais du Petrole, Rueil-Malmaison, France;

    Petroleum and Marine Division, Geoscience Australia, Canberra ACT, Australia;

    Petroleum and Marine Division, Geoscience Australia, Canberra ACT, Australia;

    Institut Francais du Petrole, Rueil-Malmaison, France;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

相似文献

  • 外文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号