首页> 外文期刊>Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth >Integration of P- and SH-wave high-resolution seismic reflection and micro-gravity techniques to improve interpretation of shallow subsurface structure: New Madrid seismic zone
【24h】

Integration of P- and SH-wave high-resolution seismic reflection and micro-gravity techniques to improve interpretation of shallow subsurface structure: New Madrid seismic zone

机译:整合P和SH波高分辨率地震反射和微重力技术,以改善对浅层地下结构的解释:新马德里地震带

获取原文
获取原文并翻译 | 示例
           

摘要

Shallow high-resolution seismic reflection surveys have traditionally been restricted to either compressional (P) or horizontally polarized shear (SH) waves in order to produce 2-D images of subsurface structure. The northernmost Mississippi embayment and coincident New Madrid seismic zone (NMSZ) provide an ideal laboratory to study the experimental use of integrating P- and SH-wave seismic profiles, integrated, where practicable, with micro-gravity data. In this area, the relation between "deeper" deformation of Paleozoic bedrock associated with the formation of the Reelfoot rift and NMSZ seismicity and "shallower" deformation of overlying sediments has remained elusive, but could be revealed using integrated P- and SH-wave reflection. Surface expressions of deformation are almost non-existent in this region, which makes seismic reflection surveying the only means of detecting structures that are possibly pertinent to seismic hazard assessment. Since P- and SH-waves respond differently to the rock and fluid properties and travel at dissimilar speeds, the resulting seismic profiles provide complementary views of the subsurface based on different levels of resolution and imaging capability. P-wave profiles acquired in southwestern Illinois and western Kentucky (USA) detect faulting of deep, Paleozoic bedrock and Cretaceous reflectors while coincident SH-wave surveys show that this deformation propagates higher into overlying Tertiary and Quaternary strata. Forward modeling of micro-gravity data acquired along one of the seismic profiles further supports an interpretation of faulting of bedrock and Cretaceous strata. The integration of the two seismic and the micro-gravity methods therefore increases the scope for investigating the relation between the older and younger deformation in an area of critical seismic hazard. (c) 2006 Elsevier B.V All rights reserved.
机译:传统上,浅层高分辨率地震反射勘测仅限于压缩波(P)或水平极化剪切波(SH),以产生地下结构的二维图像。最北端的密西西比河退潮带和新马德里地震带(NMSZ)重合提供了一个理想的实验室,用于研究整合P波和SH波地震剖面的实验应用,并在可行的情况下将其与微重力数据进行整合。在该地区,与Reelfoot裂谷形成和NMSZ地震活动有关的古生代基岩的“更深”变形与上覆沉积物的“更浅”变形之间的关系仍然难以捉摸,但可以通过整合的P波和SH波反射来揭示。 。该区域几乎不存在形变的表面表达,这使得地震反射勘测成为检测可能与地震危险性评估有关的结构的唯一手段。由于P波和SH波对岩石和流体特性的响应不同,并且以不同的速度传播,因此,基于不同级别的分辨率和成像能力,所得的地震剖面可提供地下的互补视图。在伊利诺斯州西南部和肯塔基州西部(美国)获得的P波剖面可探测到深层的,古生代的基岩和白垩纪反射层的断裂,而同时的SH波勘测表明,这种变形会传播到上覆的第三纪和第四纪地层。沿其中一个地震剖面采集的微重力数据的正演模型进一步支持了对基岩和白垩纪地层断层的解释。因此,两种地震方法和微重力方法的集成增加了在严重地震危险区域研究老旧变形与年轻变形之间关系的范围。 (c)2006 Elsevier B.V保留所有权利。

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