Recent mineralogical investigations carried out in Scarisoara Glacier Cave pointed out the presence of speleothems made up of monohydrocalcite and hydromagnesite. Although both minerals were documented earlier from other Romanian caves this is for the first time when a speleothem is described as being entirely composed of monohydrocalcite. Crocoite, a rare mineral was also identified; however, this is not a real cave mineral being transported into the cave by the percolating waters. U-Th dating of some speleothems from Scarisoara Glacier Cave enabled us to draw some considerations concerning the palaeoclimate changes and the age of the cave
The Bǎiţa metallogenic district, in Bihor County, Romania, is genetically connected to a deep-seated...
This paper presents the mineralization of five medium-size limestone-caves and eleven skarn-hosted c...
Cryogenic cave carbonates have been described from several formerly or presently glaciated karst cav...
Recent mineralogical investigations carried out in Scarisoara Glacier Cave pointed out the presence ...
Speleothems are secondary minerals that precipitate in caves, most commonly as stalagmites, stalacti...
The cave of Poiana Vârtop in the NW Bihor Mountains hosts the fourth largest underground perennial g...
In order to test the potential for Uranium-series disequilibrium dating of speleothems in Romania, n...
From a mineralogical point of view, Pestera din Valea Rea presents a great interest. Gypsum is uniqu...
The Purcăreţ - Boiu Mare Plateau and the southern edge of the Baia Mare Depression, in Sălaj and Mar...
Within the Cerna Valley in southwestern Romania, over a 100 caves were formed in the Jurassic and Cr...
Eighteen minerals belonging to eight chemical groups were identified from three caves within Şălitra...
The caves from Cerna Valley, southwest Romania, are ideal for mineralogical studies because the reac...
With the discovery of the József-hegy Cave, a cave of hydrothermal origin with an abundance of miner...
With the discovery of the József-hegy Cave, a cave of hydrothermal origin with an abundance of miner...
Caves commonly provide suitable sites for the accumulation of chemical, detrital and organic deposit...
The Bǎiţa metallogenic district, in Bihor County, Romania, is genetically connected to a deep-seated...
This paper presents the mineralization of five medium-size limestone-caves and eleven skarn-hosted c...
Cryogenic cave carbonates have been described from several formerly or presently glaciated karst cav...
Recent mineralogical investigations carried out in Scarisoara Glacier Cave pointed out the presence ...
Speleothems are secondary minerals that precipitate in caves, most commonly as stalagmites, stalacti...
The cave of Poiana Vârtop in the NW Bihor Mountains hosts the fourth largest underground perennial g...
In order to test the potential for Uranium-series disequilibrium dating of speleothems in Romania, n...
From a mineralogical point of view, Pestera din Valea Rea presents a great interest. Gypsum is uniqu...
The Purcăreţ - Boiu Mare Plateau and the southern edge of the Baia Mare Depression, in Sălaj and Mar...
Within the Cerna Valley in southwestern Romania, over a 100 caves were formed in the Jurassic and Cr...
Eighteen minerals belonging to eight chemical groups were identified from three caves within Şălitra...
The caves from Cerna Valley, southwest Romania, are ideal for mineralogical studies because the reac...
With the discovery of the József-hegy Cave, a cave of hydrothermal origin with an abundance of miner...
With the discovery of the József-hegy Cave, a cave of hydrothermal origin with an abundance of miner...
Caves commonly provide suitable sites for the accumulation of chemical, detrital and organic deposit...
The Bǎiţa metallogenic district, in Bihor County, Romania, is genetically connected to a deep-seated...
This paper presents the mineralization of five medium-size limestone-caves and eleven skarn-hosted c...
Cryogenic cave carbonates have been described from several formerly or presently glaciated karst cav...