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Titlebook: Hypogene Karst Regions and Caves of the World; Alexander Klimchouk,Arthur N. Palmer,Philippe Audr Book 2017 Springer International Publish

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發(fā)表于 2025-3-21 18:11:58 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Hypogene Karst Regions and Caves of the World
編輯Alexander Klimchouk,Arthur N. Palmer,Philippe Audr
視頻videohttp://file.papertrans.cn/431/430775/430775.mp4
概述Presents the most representative coverage of hypogene karst of the world.Helps the reader with numerous regional and cave-specific case studies to acknowledge the diversity of hypogene speleogenetic p
叢書名稱Cave and Karst Systems of the World
圖書封面Titlebook: Hypogene Karst Regions and Caves of the World;  Alexander Klimchouk,Arthur N. Palmer,Philippe Audr Book 2017 Springer International Publish
描述This book illustrates the diversity of hypogene speleogenetic processes and void-conduit patterns depending on variations of the geological environments by presenting regional and cave-specific case studies. The cases include both well-known and newly recognized hypogene karst regions and caves of the world. They all focus on geological, hydrogeological, geodynamical and evolutionary contexts of hypogene speleogenesis..The last decade has witnessed the boost in recognition of the possibility, global occurrence, and practical importance of hypogene karstification (speleogenesis), i.e. the development of solutional porosity and permeability by upwelling flow, independent of recharge from the overlying or immediately adjacent surface. Hypogene karst has been identified and documented in many regions where it was previously overlooked or misinterpreted. The book enriches the basis for generalization and categorization of hypogene karst and thus improves ourability to adequately model hypogene karstification and predict related porosity and permeability. It is a book which benefits every researcher, student, and practitioner dealing with karst..
出版日期Book 2017
關(guān)鍵詞Hypogene Karst; Deep-seated Karst; Hypogene Speleogenesis; Solutional Porosity and Permeability; Karst R
版次1
doihttps://doi.org/10.1007/978-3-319-53348-3
isbn_softcover978-3-319-85131-0
isbn_ebook978-3-319-53348-3Series ISSN 2364-4591 Series E-ISSN 2364-4605
issn_series 2364-4591
copyrightSpringer International Publishing AG, part of Springer Nature 2017
The information of publication is updating

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沙發(fā)
發(fā)表于 2025-3-21 21:20:35 | 只看該作者
板凳
發(fā)表于 2025-3-22 00:59:54 | 只看該作者
Marketing und Innovationsmanagementudes deep-seated acidic sources (CO./H.S), “hydrothermal” cooling, mixing corrosion, and Sulfuric Acid Speleogenesis (SAS) at and above the water table. HS localizes in basin at sites of upward flows and convergences, in deformed strata at structural highs and major faults. In disrupted basins, geot
地板
發(fā)表于 2025-3-22 05:52:58 | 只看該作者
https://doi.org/10.1007/978-3-658-21968-0 mechanisms rarely observed in hypogene cavities elsewhere in the world. Here, we investigate the hypogenic morphologies and speleothems of four caves in this region, namely Sima de la Higuera, Sima Destapada, Cueva del Agua and Cueva del Puerto. Also, other ten caves showing evidence for hypogenic
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發(fā)表于 2025-3-22 16:54:37 | 只看該作者
https://doi.org/10.1007/978-3-658-10301-9 hundred caves of hypogene origin are known, whose features and modes of origin are reviewed in this article. Most currently known hypogene caves cluster along the rim of the southern Vienna Basin. Some of these caves, including Eisensteinh?hle, are characterized by a slight thermal anomaly associat
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https://doi.org/10.1007/978-3-658-04401-5lfidic thermal waters that mix with both recent fresh infiltration waters and coastal salt water has formed four active sulfuric acid speleogenesis (SAS) caves. These caves are characterized by the typical set of sulfuric acid meso- and micromorphologies, and also by the presence of both gypsum and
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發(fā)表于 2025-3-23 08:08:39 | 只看該作者
https://doi.org/10.1007/978-3-658-17855-0he anticline where the river valley reaches the top of a Meso-Cenozoic limestone succession, capped by less permeable rocks. An important terraced travertine deposit was produced by the thermal water throughout the Pleistocene. The most interesting caves are in the valley of the Rio Garrafo, a tribu
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