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Titlebook: Karstology in the Classical Karst; Martin Knez,Bojan Otoni?ar,Tadej Slabe Book 2020 Springer Nature Switzerland AG 2020 Karstology.Classic

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31#
發(fā)表于 2025-3-26 21:00:46 | 只看該作者
978-3-030-26829-9Springer Nature Switzerland AG 2020
32#
發(fā)表于 2025-3-27 02:18:12 | 只看該作者
Karstology in the Classical Karst978-3-030-26827-5Series ISSN 2511-2066 Series E-ISSN 2511-2082
33#
發(fā)表于 2025-3-27 09:01:37 | 只看該作者
Martin Knez,Bojan Otoni?ar,Tadej SlabeExplains developments from a leading international karstological research and study center.Integrates interdisciplinary research on karst surface, caves, waters, and biological characteristics.Details
34#
發(fā)表于 2025-3-27 10:27:34 | 只看該作者
Advances in Karst Sciencehttp://image.papertrans.cn/k/image/542142.jpg
35#
發(fā)表于 2025-3-27 15:49:36 | 只看該作者
36#
發(fā)表于 2025-3-27 18:04:43 | 只看該作者
37#
發(fā)表于 2025-3-27 23:53:51 | 只看該作者
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).
38#
發(fā)表于 2025-3-28 06:11:17 | 只看該作者
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.
39#
發(fā)表于 2025-3-28 08:06:05 | 只看該作者
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.
40#
發(fā)表于 2025-3-28 14:14:43 | 只看該作者
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.
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