Research on morphological caracteristics of endokarst in Rarau Massif. Premises for local palaeoclimatic records
<p>The occurrence of karst in Romania is associated to a variety of carbonate rocks; however, limestone and dolomite are the most relevant in terms of spatial distribution and morphological diversity, as shown by the karst landforms present in Apuseni Mts, Banat Mts, Cerna Mts, the southern ar...
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„Ștefan cel Mare” University Press
2014-11-01
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Online Access: | http://georeview.ro/ojs/index.php/revista/article/view/233 |
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doaj-99f7b054765c48cf9bab25995b627b6b2021-06-02T11:16:08Zeng„Ștefan cel Mare” University PressGEOREVIEW: Scientific Annals of Stefan cel Mare University of Suceava. Geography Series1583-14692014-11-01242122127273Research on morphological caracteristics of endokarst in Rarau Massif. Premises for local palaeoclimatic recordsDinu OPREAGeorgiana BUTA<p>The occurrence of karst in Romania is associated to a variety of carbonate rocks; however, limestone and dolomite are the most relevant in terms of spatial distribution and morphological diversity, as shown by the karst landforms present in Apuseni Mts, Banat Mts, Cerna Mts, the southern area of Retezat Mts, Capatanii Mts, Valcan Mts, Mehedinti and Southern Dobrogea plateaus etc.<br />Our study area is located in Rarau Massif, in the northern sector of the crystalline axe of the Eastern Carpathians (fig. 1), which comprises, in terms of morphology, of a diversity of genetic categories of landforms among which petrographic landforms on limestone and dolomites stand out.</p>http://georeview.ro/ojs/index.php/revista/article/view/233endokarst |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Dinu OPREA Georgiana BUTA |
spellingShingle |
Dinu OPREA Georgiana BUTA Research on morphological caracteristics of endokarst in Rarau Massif. Premises for local palaeoclimatic records GEOREVIEW: Scientific Annals of Stefan cel Mare University of Suceava. Geography Series endokarst |
author_facet |
Dinu OPREA Georgiana BUTA |
author_sort |
Dinu OPREA |
title |
Research on morphological caracteristics of endokarst in Rarau Massif. Premises for local palaeoclimatic records |
title_short |
Research on morphological caracteristics of endokarst in Rarau Massif. Premises for local palaeoclimatic records |
title_full |
Research on morphological caracteristics of endokarst in Rarau Massif. Premises for local palaeoclimatic records |
title_fullStr |
Research on morphological caracteristics of endokarst in Rarau Massif. Premises for local palaeoclimatic records |
title_full_unstemmed |
Research on morphological caracteristics of endokarst in Rarau Massif. Premises for local palaeoclimatic records |
title_sort |
research on morphological caracteristics of endokarst in rarau massif. premises for local palaeoclimatic records |
publisher |
„Ștefan cel Mare” University Press |
series |
GEOREVIEW: Scientific Annals of Stefan cel Mare University of Suceava. Geography Series |
issn |
1583-1469 |
publishDate |
2014-11-01 |
description |
<p>The occurrence of karst in Romania is associated to a variety of carbonate rocks; however, limestone and dolomite are the most relevant in terms of spatial distribution and morphological diversity, as shown by the karst landforms present in Apuseni Mts, Banat Mts, Cerna Mts, the southern area of Retezat Mts, Capatanii Mts, Valcan Mts, Mehedinti and Southern Dobrogea plateaus etc.<br />Our study area is located in Rarau Massif, in the northern sector of the crystalline axe of the Eastern Carpathians (fig. 1), which comprises, in terms of morphology, of a diversity of genetic categories of landforms among which petrographic landforms on limestone and dolomites stand out.</p> |
topic |
endokarst |
url |
http://georeview.ro/ojs/index.php/revista/article/view/233 |
work_keys_str_mv |
AT dinuoprea researchonmorphologicalcaracteristicsofendokarstinraraumassifpremisesforlocalpalaeoclimaticrecords AT georgianabuta researchonmorphologicalcaracteristicsofendokarstinraraumassifpremisesforlocalpalaeoclimaticrecords |
_version_ |
1721404868305879040 |