Solace 发表于 2025-3-26 21:00:46
978-3-030-26829-9Springer Nature Switzerland AG 2020虚假 发表于 2025-3-27 02:18:12
Karstology in the Classical Karst978-3-030-26827-5Series ISSN 2511-2066 Series E-ISSN 2511-2082小卒 发表于 2025-3-27 09:01:37
Martin Knez,Bojan Otoničar,Tadej SlabeExplains developments from a leading international karstological research and study center.Integrates interdisciplinary research on karst surface, caves, waters, and biological characteristics.DetailsSuggestions 发表于 2025-3-27 10:27:34
Advances in Karst Sciencehttp://image.papertrans.cn/k/image/542142.jpg商议 发表于 2025-3-27 15:49:36
http://reply.papertrans.cn/55/5422/542142/542142_35.pngCanvas 发表于 2025-3-27 18:04:43
http://reply.papertrans.cn/55/5422/542142/542142_36.pngAcumen 发表于 2025-3-27 23:53:51
Late Cretaceous and Paleogene Paleokarsts of the Northern Sector of the Adriatic Carbonate PlatformIn Western Slovenia, a paleokarstic surface with clayey bauxite deposits separates late? Cenomanian to late Turonian strata from middle/late Coniacian palustrine?, peritidal and shallow-marine carbonate deposits along the external-most preserved parts of the Adriatic Carbonate Platform (AdCP).cogitate 发表于 2025-3-28 06:11:17
Lithomorphogenesis of Karst Surface,The rock relief of karst phenomena is often a revealing and graphic trace of their formation and development. It is composed of rock forms.GULP 发表于 2025-3-28 08:06:05
Significant Findings from Karst Sediments Research,About 44% of Slovenia’s surface consists of carbonate rocks. Karst geomorphology and over 13,000 known caves represent a significant proportion of its landscape. Various sediments present on the karst surface in the form of clastic or precipitated deposits can cover or fill smaller or extended areas and they can also accumulate in the caves.Hemodialysis 发表于 2025-3-28 14:14:43
Measurements of Present-Day Limestone Dissolution and Calcite Precipitation Rates with Limestone TaQuantification of present-day fundamental chemical processes in caves (dissolution and calcite precipitation) can provide basic objective information on rates, make possible comparison with other speleogenetic processes, and provide insights into spatial and temporal variability as well as factors controlling both processes.