• 主题
高级搜索  >
历史搜索 清空历史
首页> 外文会议>EAGE conference & exhibition;SPE EUROPEC 2005;Madrid 2005 >Regional tectonics and Hormuz Salt in Zagros,Iran. Geological observations and modeling
【24h】

Regional tectonics and Hormuz Salt in Zagros,Iran. Geological observations and modeling

机译：伊朗扎格罗斯的区域构造和Hormuz盐。地质观测与建模

获取原文
页面导航
  • 摘要
  • 著录项
  • 相似文献
  • 相关主题

摘要

The purpose of this paper is to discuss (1) the distribution of the Eocambrian Hormuz saltseries in the Zagros region; (2) the timing of salt diapirism; (3) the influence of pre-existingsalt structures on fold-and-trust location and propagation; (4) the mechanisms of rapid saltextrusion, and also (5) the location of the salt diapirs relative to thrusts and folds.The mechanisms of diapirism in the Hormuz series have been a subject of interest for manyyears in the Zagros fold-and-thrust belt. Most of the authors emphasis the role of salt on foldpropagation (basal decollement, fold propagation style),or the role of basement fault or pull-apartzone on the development of diapirs prior to the main shortening event.We based our interpretation on both geological observations, seismic and well data. Geologicdata are then compared to analogue sand box experiments. On these bases, we argue that thedriving mechanism of Hormuz halokinesis extrusion, during the Zagros folding and erosion,is the squeezing of pre-existing salt diapirs during shortening. These diapirs also influence thelocation of thrusts and strike slip relay faults (weak zones). Emergent diapirs occurred abovepre-existing domes along these faults, or at the plunging axes of the folds. Diapirs exposed inthe core of the anticlines are likely pre-existing salt pillow detached from the salt layer by thethrust propagation. Understanding the formation and development of the Hormuz diapirs is akey issue for reservoir understanding and hydrocarbon trapping in the Zagros province.
机译：本文的目的是讨论（1）扎格罗斯地区Eocambrian Hormuz盐系列的分布； （2）盐透性的时机； （3）既有的盐结构对折叠信任位置和传播的影响； （4）快速盐挤压的机制，以及（5）盐底物相对于推力和褶皱的位置。Hormuz系列中的透水作用机理多年来一直是Zagros褶皱-推力研究的主题。带。大多数作者都将盐的作用重点放在褶皱的传播（基底弯折，褶皱传播方式）上，或者将基层断层或拉脱带作用作用于主要起酥油事件之前的底辟发育上。我们基于这两个地质观测结果进行了解释。 ，地震和油井数据。然后将地质数据与模拟沙箱实验进行比较。在这些基础上，我们认为，在Zagros折叠和侵蚀过程中，霍尔木兹halokinesis挤压的驱动机制是缩短过程中先前存在的盐的挤压。这些底线也影响推力和走滑继电器故障（弱区）的位置。沿这些断层或褶皱的俯冲轴，在预先存在的穹顶上方出现了突发的底栖生物。暴露在背斜核心的底盘很可能是通过推力传播从盐层脱离的预先存在的盐枕。理解Hormuz底栖动物的形成和发育是了解扎格罗斯省储层和油气捕集的关键问题。

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