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

可憐

書(shū)目名稱Hypogene Karst Regions and Caves of the World影響因子(影響力)




書(shū)目名稱Hypogene Karst Regions and Caves of the World影響因子(影響力)學(xué)科排名




書(shū)目名稱Hypogene Karst Regions and Caves of the World網(wǎng)絡(luò)公開(kāi)度




書(shū)目名稱Hypogene Karst Regions and Caves of the World網(wǎng)絡(luò)公開(kāi)度學(xué)科排名




書(shū)目名稱Hypogene Karst Regions and Caves of the World被引頻次




書(shū)目名稱Hypogene Karst Regions and Caves of the World被引頻次學(xué)科排名




書(shū)目名稱Hypogene Karst Regions and Caves of the World年度引用




書(shū)目名稱Hypogene Karst Regions and Caves of the World年度引用學(xué)科排名




書(shū)目名稱Hypogene Karst Regions and Caves of the World讀者反饋




書(shū)目名稱Hypogene Karst Regions and Caves of the World讀者反饋學(xué)科排名

Interregnum

invulnerable

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

SEMI

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

潛伏期

Mendacious

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

pantomime

CHARM

啤酒

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

字形刻痕

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