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Geophysical prediction and following development sinkholes in two Dead Sea areas, Israel and Jordan

机译:以色列和约旦两个死海地区的地球物理预测和后续开发陷井

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摘要

Geophysical methods-seismic refraction (SRFR), electrical resistivity tomography (ERT), and microgravity-were applied to the Dead Sea (DS) sinkhole problem in the Ein Gedi area at the earlier stage of the sinkhole development (1998-2002). They allowed determining the sinkhole formation mechanism and localizing the sinkhole hazardous zones. The SRFR method permitted to delineate the underground edge of a salt layer at the depth of 50 m. The salt edge was shaped like the sinkhole line on the surface. It was concluded that the sinkhole development is linked to the salt edge. Geoelectrical quasi-3D mapping based on the ERT technique detected large resistivity anomalies with 250-300 m~2 diameter and 25-35 m deep. The Ein Gedi area has been also mapped by the use of Microgravity method. The residual Bouguer gravity anomaly map shows negative anomalies arranged along the edge of the salt layer. Those gravity anomalies overall are very similar in plan to the resistivity distribution in this area. The results of forward modeling indicate that both high resistivity and residual gravity anomalies are associated with a subsurface decompaction of the soil mass and deep cavity at the sinkhole site. Following monitoring of the sinkhole development carried out by the Geological Survey of Israel confirmed our suggestions. The drilling of numerous boreholes verified the location of the salt edge. Geographical Information System (GIS) database testifies that during 2003-2009 new sinkholes are continuing to develop along the salt edge within a narrow 50-100 m wide strip oriented approximately in north-south direction (slightly parallel to the shoreline). No promotion in west-east direction (perpendicularly to the DS shoreline) was observed in Israel. Collapse of sinkholes and their clustering have been occurred within the area of high resistivity anomaly and negative residual gravity anomaly. Similar studies carried out at the Ghor Al-Haditha area (Jordan) have shown that sinkholes there are also arranged along the winding line conforming to the salt edge. In this area sinkholes are slowly moved to the Dead Sea direction. Results of geophysical studies in numerous DS sites indicate similar sinkhole development. It allowed generating of the sinkhole formation model based on ancient (10,000-11,000-year old) salt belt girding the Dead Sea along its shores.
机译:地球物理方法-地震折射(SRFR),电阻层析成像(ERT)和微重力-在沉降坑开发的早期阶段(1998-2002)被应用于Ein Gedi地区的死海(DS)沉降坑问题。他们允许确定下沉孔的形成机制并确定下沉孔的危险区域。 SRFR方法允许在50 m深度划定盐层的地下边缘。盐边缘的形状类似于表面上的下沉线。结论是,下沉孔的发育与盐边缘有关。基于ERT技术的地电准3D测绘发现了直径250-300 m〜2,深度25-35 m的大电阻率异常。 Ein Gedi地区也已通过使用微重力方法绘制了地图。剩余的布格重力异常图显示沿盐层边缘排列的负异常。总体上,这些重力异常在平面上与该区域的电阻率分布非常相似。正演模拟的结果表明,高电阻率和残余重力异常都与泥坑地下土体和深孔的地下破坏有关。以色列地质调查局对下沉坑的发展进行了监测,证实了我们的建议。大量钻孔的钻探证实了盐岩边缘的位置。地理信息系统(GIS)数据库证明,在2003-2009年期间,新的水坑在大约沿南北方向(略平行于海岸线)的50-100 m宽的窄带内沿盐边继续发展。以色列未观察到东西方向(垂直于DS海岸线)的上升。在高电阻率异常和负剩余重力异常区域内已经发生了塌陷塌陷及其聚集。在Ghor Al-Haditha地区(约旦)进行的类似研究表明,那里的水坑也沿着绕盐线的绕组线排列。在该区域,污水坑缓慢地向死海方向移动。在许多DS站点进行的地球物理研究结果表明类似的下沉发展。它允许根据沿海岸沿死海的古老(10,000-11,000年历史)盐带生成下沉形成模型。

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  • 来源
    《Environmental earth sciences》 |2013年第4期|1463-1478|共16页
  • 作者单位

    Geophysical Institute of Israel, 6 Baal Shem-Tov Street, 71100 Lod, Israel;

    Department of Geophysics and Planetary Sciences, Raymond and Beverly Sackler Faculty of Exact Sciences, Tel Aviv University, Ramat Aviv, 69978 Tel Aviv, Israel;

    Al-Balqa Applied University, Salt, Jordan;

    Geophysical Institute of Israel, 6 Baal Shem-Tov Street, 71100 Lod, Israel;

    Al-Balqa Applied University, Salt, Jordan;

    Al-Balqa Applied University, Salt, Jordan;

    Geophysical Institute of Israel, 6 Baal Shem-Tov Street, 71100 Lod, Israel,Schlumberger, Via dell'Unione Europea, 4 San Donato Milanese, Milan, Italy;

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

    Dead Sea; Sinkholes; Seismic refraction; ERT; Microgravity;

    机译:死海;污水池;地震折射ERT;微重力;

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