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Karstic features in gypsum of Gachsaran Formation (case study; Chamshir Dam reservoir, Iran)

机译:Gachsaran组的石膏中的岩溶特征(案例研究;伊朗Chamshir大坝水库)

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摘要

Chamshir Dam site is located in southwest of Iran, on Zuhreh River, 20 km southeast of Gachsaran city. The study area mainly covered by evaporite formations of Fars Group especially Gachsaran Formation. Dam axis is located on limestone beds of Mishan Formation but nearly two-thirds of the dam reservoir is in contact with the Gachsaran Formation. The reservoir and dam site have been brecciated by several faults such as Dezh Soleyman thrust and Chamshir fault zone that lead to development of karst in this region. The region has a wide variety of developed karstic features such as karrens, dissolution dolines, karstic springs and cavities. These karst features can compromise on the ability of Chamshir Dam to hold water in the reservoir, and can even cause collapse of the dam. Gypsum karst in the Chamshir Dam reservoir may develop the solution channels and cavities which cause water to flow toward downstream of the dam reservoir. Therefore, to eliminate these problems, construction of cutoff wall or clay blanket is proposed.
机译:Chamshir大坝遗址位于伊朗西南部,祖赫雷河上,位于加沙兰市东南20公里处。研究区域主要覆盖了Fars组的蒸发岩层,特别是Gachsaran组。大坝轴线位于密山组的石灰岩层上,但将近三分之二的大坝水库与Gachsaran组相接触。水库和坝址已被Dezh Soleyman逆冲断层和Chamshir断层带等多个断层角砾化,导致该地区的岩溶发展。该地区具有各种发达的岩溶特征,例如岩溶,溶蚀圈线,岩溶泉和空洞。这些岩溶特征可能会损害Chamshir大坝将水保持在水库中的能力,甚至可能导致大坝倒塌。 Chamshir大坝水库中的石膏岩溶可能形成溶液通道和空腔,导致水流向大坝水库的下游。因此,为了消除这些问题,提出了建造防渗墙或粘土毯的方法。

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  • 来源
    《Carbonates and Evaporites》 |2012年第4期|p.291-297|共7页
  • 作者单位

    Department of Geology, Faculty of Sciences, Bu-Ali Sina University, Mahdieh Ave., 65175-38695, Hamedan, Iran;

    Department of Geology, Faculty of Sciences, Bu-Ali Sina University, Mahdieh Ave., 65175-38695, Hamedan, Iran;

    Department of Geology, Faculty of Sciences, Bu-Ali Sina University, Mahdieh Ave., 65175-38695, Hamedan, Iran;

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

    Dam; Karstic features; Gachsaran Formation;

    机译:大坝;岩溶特征;加沙兰组;

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