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Titlebook: Evolution of Karst in the Lower Part of Crna Reka River Basin; Marjan Temovski Book 2016 Springer International Publishing Switzerland 201

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發(fā)表于 2025-3-21 17:12:54 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書(shū)目名稱(chēng)Evolution of Karst in the Lower Part of Crna Reka River Basin
編輯Marjan Temovski
視頻videohttp://file.papertrans.cn/318/317736/317736.mp4
概述Nominated as an outstanding Ph.D. thesis by the University of Nova Gorica, Slovenia.Presents the diversity and complexity of processes and mechanisms operating under various hypogenic speleogenetic en
叢書(shū)名稱(chēng)Springer Theses
圖書(shū)封面Titlebook: Evolution of Karst in the Lower Part of Crna Reka River Basin;  Marjan Temovski Book 2016 Springer International Publishing Switzerland 201
描述.This thesis addresses karst development in a terrain characterized by a highly complex geological and geomorphological evolution. It tackles the extent and complexity of both epigenic and hypogenic karst development, based on morphological analyses of caves, combined with analyses and datations of cave sediments and their correlation to regional geological and geomorphological evolution..?.Hypogenic karst registered is mainly the result of hydrothermal speleogenesis due to increased geothermal gradient in connection with nearby Pliocene-Pleistocene volcanic centers, with occurrence of sulfuric acid speleogenesis and ghost-rock weathering due to local geological or lithological control. Epigenic speleogenesis is strongly controlled by base level oscillations, with also examples of deep phreatic (now fossil) caves connected to regional base level rise, and per-ascensum speleogenesis..?.Another important finding is the constraining of the timing of Mariovo Lake draining in the Pleistocene, an important event in order to understand the geomorphological evolution in Macedonia, as it led to the onset of fluvial development and incision of valleys, shaping most of the present morphology.
出版日期Book 2016
關(guān)鍵詞Crna Reka; Epigenic speleogenesis; Ghost-rock weathering; Hypogenic speleogenesis; Karst evolution; Maced
版次1
doihttps://doi.org/10.1007/978-3-319-24547-8
isbn_softcover978-3-319-37409-3
isbn_ebook978-3-319-24547-8Series ISSN 2190-5053 Series E-ISSN 2190-5061
issn_series 2190-5053
copyrightSpringer International Publishing Switzerland 2016
The information of publication is updating

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發(fā)表于 2025-3-21 22:33:11 | 只看該作者
Book 2016nt and complexity of both epigenic and hypogenic karst development, based on morphological analyses of caves, combined with analyses and datations of cave sediments and their correlation to regional geological and geomorphological evolution..?.Hypogenic karst registered is mainly the result of hydro
板凳
發(fā)表于 2025-3-22 02:10:35 | 只看該作者
General Overview of the Research Area, of Macedonia. Karst areas within its basin are located in the upper part in Demir Hisar area, and in the lower part in Mariovo and Tikve? Basins, and also in the basin of its major tributary Raec River ( Fig.?.).
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Axiomata Erasmi Pro Cavsa Martini Lvtheri,sulfuric acid speleogenesis. In Ko?uf locality, hypogenic caves were not found, but several thermal springs emerging from carbonate rocks indicate that karstification is ongoing in deeper parts of the karst system.
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Evolution of Karst in the Lower Part of Crna Reka River Basin
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發(fā)表于 2025-3-23 09:30:32 | 只看該作者
2190-5053 Pleistocene, an important event in order to understand the geomorphological evolution in Macedonia, as it led to the onset of fluvial development and incision of valleys, shaping most of the present morphology.978-3-319-37409-3978-3-319-24547-8Series ISSN 2190-5053 Series E-ISSN 2190-5061
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