首页> 外文期刊>Journal of structural geology >Salt-influenced normal fault growth and forced folding: The Stavanger Fault System, North Sea
【24h】

Salt-influenced normal fault growth and forced folding: The Stavanger Fault System, North Sea

机译:盐影响的正常断层生长和强迫褶皱:北海斯塔万格断层系统

获取原文
获取原文并翻译 | 示例
           

摘要

Displacement ratio (D_r) is the ratio between salt thickness (T_v) and sub-salt normal fault displacement (D) (D_r = T_v/D), and it is typically used to predict the degree of geometric and kinematic linkage between sub- and supra-salt fault populations, and the overall structural style in salt-influenced extensional settings. However, we currently lack natural examples of how D_r and the underlying geological controls vary, and how these may control the three-dimensional geometry and evolution of salt-influenced normal fault systems. Furthermore, it is currently unknown if kinematic coherence in salt-influenced extensional settings can be maintained over relatively long length-scales (10~1-10~3 m) and for relatively long timeframes, and how this may impact the growth and geometry of large-throw (>500 m), salt-influenced normal fault systems. In this paper we use a 3600 km2, high-quality 3D seismic reflection dataset and borehole data from the Stavanger Fault System (SFS), Egersund Basin, eastern North Sea Basin to investigate; (i) how pre-rift salt thickness (T_v) and sub-salt fault throw (T) control the structural style and evolution of a basin-bounding, salt-influenced normal fault system; and (ii) the role salt plays in maintaining kinematic coherence in normal fault systems. We demonstrate that; (i) pre-rift salt distribution (T_v). specifically its presence in the proto-footwall (i.e., when T_v > 0), is the primary control on partitioning of faulting and (forced) folding along the fault system, and the style of linkage (i.e., hard- or soft-linkage) between sub- and supra-salt fault populations; and (ii) sub- and supra-salt fault populations represent brittle elements of a single, geometrically and kinematically coherent structure, the geometry and evolution of which is related to the ductile translation of strain on a scale (up to 8 km) and duration (c. 65 Myr) that believe is significantly greater and longer than previously documented.
机译:位移比(D_r)是盐厚度(T_v)与盐下法向断层位移(D)之间的比率(D_r = T_v / D),通常用于预测盐下层和盐层之间的几何和运动学联系程度超盐断层人口,以及盐影响的伸展构造的整体构造样式。但是,我们目前尚缺乏有关D_r和基础地质控制如何变化以及它们如何控制三维几何结构和盐影响的正常断层系统演化的自然示例。此外,目前尚不清楚是否可以在相对较长的长度范围(10〜1-10〜3 m)和相对较长的时间范围内维持盐影响的伸展环境中的运动学连贯性,以及这如何影响盐分的生长和几何形状。大范围(> 500 m)受盐影响的正常断层系统。在本文中,我们使用了一个3600 km2的高质量3D地震反射数据集和北海盆地东部埃格森德盆地斯塔万格断裂系统(SFS)的井眼数据进行调查; (i)裂谷前的盐厚度(T_v)和盐下断层投掷(T)如何控制盆地边界,受盐影响的正常断层系统的结构样式和演化; (ii)盐在正常断层系统中在维持运动学连贯性方面发挥着作用。我们证明了这一点; (i)裂谷前的盐分布(T_v)。特别是它存在于前脚下壁(即,当T_v> 0时)是对沿断裂系统划分断层和(强迫)折叠的分区以及链接方式(即硬链接或软链接)的主要控制权在超盐和超盐断裂种群之间; (ii)盐下和上盐断层群代表单一的,几何上和运动学上一致的结构的脆性元素,其几何结构和演化与应变的延性平移有关(最大8 km)和持续时间(c。65 Myr)认为比以前记录的要大得多,而且更长。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 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