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A multi-method approach for speleogenetic research on alpine karst caves. Torca La Texa shaft, Picos de Europa (Spain)

机译:高山岩溶洞穴成因研究的一种多方法方法。 Torca La Texa竖井,Picos de Europa(西班牙)

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Speleogenetic research on alpine caves has advanced significantly during the last decades. These investigations require techniques from different geoscience disciplines that must be adapted to the methodological constraints of working in deep caves. The Picos de Europa mountains are one of the most important alpine karsts, including 14% of the World's Deepest Caves (caves with more than 1 km depth). A speleogenetic research is currently being developed in selected caves in these mountains; one of them, named Torca La Texa shaft, is the main goal of this article. For this purpose, we have proposed both an optimized multi-method approach for speleogenetic research in alpine caves, and a speleogenetic model of the Torca La Texa shaft. The methodology includes: cave surveying, dye-tracing, cave geometry analyses, cave geomorphological mapping, Uranium series dating (U-234/Th-230) and geomorphological, structural and stratigraphical studies of the cave surroundings. The SpeleoDisc method was employed to establish the structural control of the cavity. Torca La Texa (2653 m length, 215 m depth) is an alpine cave formed by two cave levels, vadose canyons and shafts, soutirage conduits, and gravity-modified passages. The cave was formed prior to the Middle Pleistocene and its development was controlled by the drop of the base level, producing the development of the two cave levels. Coevally to the cave levels formation, soutirage conduits originated connecting phreatic and epiphreatic conduits and vadose canyons and shafts were formed. Most of the shafts were created before the local glacial maximum (43-45 ka) and only two cave passages are related to dolines developed in recent times. The cave development is strongly related to the structure, locating the cave in the core of a gentle fold with the conduits' geometry and orientation controlled by the bedding and five families of joints. (C) 2015 Elsevier B.V. All rights reserved.
机译:在过去的几十年中,对高山洞穴的造山作用研究取得了重大进展。这些调查需要来自不同地球科学学科的技术,这些技术必须适应于深洞工作的方法学约束。欧罗巴山(Picos de Europa)山脉是最重要的高山喀斯特地貌之一,占世界上最深洞穴(深度超过1公里的洞穴)的14%。目前正在这些山区的特定洞穴中进行成因研究。其中一个名为Torca La Texa的竖井是本文的主要目标。为此,我们提出了一种用于高山洞穴造山研究的优化多方法方法,以及Torca La Texa竖井的造山模型。该方法包括:洞穴勘测,染料示踪,洞穴几何分析,洞穴地貌制图,铀系列定年(U-234 / Th-230)以及洞穴周围环境的地貌,结构和地层研究。 SpeleoDisc方法用于建立空腔的结构控制。 Torca La Texa(长2653 m,深215 m)是一个高山洞穴,由两个洞穴水平,渗流峡谷和竖井,污水管道和重力修正通道组成。该洞穴是在中更新世之前形成的,其发育受基础水平的下降控制,从而产生了两个洞穴水平的发育。到洞穴水平的形成很明显,形成了连接潜水和上水管道的泥浆管道,并形成了渗流峡谷和竖井。大多数竖井都是在当地冰川最大值(43-45 ka)之前创建的,只有两个洞穴通道与最近形成的do龙有关。洞穴的发育与结构密切相关,将洞穴定位在平缓褶皱的核心,其导管的几何形状和方向由垫层和五个节理控制。 (C)2015 Elsevier B.V.保留所有权利。

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