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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 2025-3-26 23:00:52 | 只看該作者
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發(fā)表于 2025-3-27 04:35:50 | 只看該作者
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發(fā)表于 2025-3-27 05:56:48 | 只看該作者
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發(fā)表于 2025-3-27 10:36:32 | 只看該作者
Hypogene Caves of Romaniaconducted on ore deposits or thermal water resources used in spas. Genetically, they are grouped in three categories: (1) caves related to upwelling of H.S-rich thermal waters along Cerna Valley (SW Romania) and around the town of Mangalia (SE Romania), (2) voids created in skarns and limestones dur
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發(fā)表于 2025-3-27 13:59:41 | 只看該作者
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發(fā)表于 2025-3-27 20:35:59 | 只看該作者
Caves of the Buda Thermal Karstdapest, on the right side of the Danube, under 300–400?m high hills. Due to the mixing corrosion enhanced by CO. and perhaps sulfuric acid, the water circulation formed multi-storey cave systems with different morphologies and complicated layout along the tectonic fissures. The arrangement of caves
37#
發(fā)表于 2025-3-27 23:57:49 | 只看該作者
2364-4591 odel hypogene karstification and predict related porosity and permeability. It is a book which benefits every researcher, student, and practitioner dealing with karst..978-3-319-85131-0978-3-319-53348-3Series ISSN 2364-4591 Series E-ISSN 2364-4605
38#
發(fā)表于 2025-3-28 03:35:22 | 只看該作者
https://doi.org/10.1007/978-3-322-99887-3on of rocks around conduits. Genetic categorization and discrimination of characteristic settings of hypogene karst are based on consideration of driving forces and conditions for fluid circulation and ascending flow in the upper crust in the context of tectonic/geodynamic positions and history of r
39#
發(fā)表于 2025-3-28 06:26:26 | 只看該作者
40#
發(fā)表于 2025-3-28 13:50:15 | 只看該作者
Marketing und Innovationsmanagementdonite), with condensation–corrosion cupolas above the water Table.?2D maze caves develop below less permeable strata. Giant ascending shafts (Salins shaft), collapse shafts, and breccia pipes (called “organs” in the N.-French coal basin) correspond to “hyperkarst” phenomena. Caves with ore deposits
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