大葉大學圖書館 |

Evolution of karst in the lower part of Crna Reka River Basin[electronic resource] /

紀錄類型:	書目-語言資料,印刷品 : Monograph/item
杜威分類號:	551.447094976
書名/作者:	Evolution of karst in the lower part of Crna Reka River Basin/ by Marjan Temovski.
作者:	Temovski, Marjan.
出版者:	Cham : : Springer International Publishing :, 2016.
面頁冊數:	xiii, 265 p. : : ill., map, digital ;; 24 cm.
Contained By:	Springer eBooks
標題:	Karst - Macedonia.
標題:	Earth Sciences.
標題:	Earth Sciences, general.
ISBN:	9783319245478
ISBN:	9783319245454
內容註:	Introduction -- General overview of the research area -- Methodology -- Hypogenic cave development -- Epigenic cave development -- Characteristics of karst surface -- General conclusions -- Appendix A -- Appendix B.
摘要、提要註:	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.
電子資源:	http://dx.doi.org/10.1007/978-3-319-24547-8

Evolution of karst in the lower part of Crna Reka River Basin[electronic resource] /
Temovski, Marjan.

Evolution of karst in the lower part of Crna Reka River Basin[electronic resource] /by Marjan Temovski. - Cham :Springer International Publishing :2016. - xiii, 265 p. :ill., map, digital ;24 cm. - Springer theses,2190-5053. - Springer theses..

Introduction -- General overview of the research area -- Methodology -- Hypogenic cave development -- Epigenic cave development -- Characteristics of karst surface -- General conclusions -- Appendix A -- Appendix B.

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.

ISBN: 9783319245478

Standard No.: 10.1007/978-3-319-24547-8doiSubjects--Topical Terms:

652433
Karst
--Macedonia.

LC Class. No.: GB600.4.M33

Dewey Class. No.: 551.447094976

Evolution of karst in the lower part of Crna Reka River Basin[electronic resource] /
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