Add to ORKGSpeleothems are secondary cave mineral deposits whose internal organization can be studied by mineralogical techniques. The ontogeny of minerals is a technique developed in Russia whereby individual crystals and their aggregates are studied as physical bodies rather than as mineral species. This paper gives a concise guide to the terminology of ontogeny, as applied to cave mineral deposits
Satisfactory explanation of the origin and development of caves (speleogenesis) is a core problem of...
A procedure using a scanning electron microscope (SEM) with mineral detection was developed to deter...
Within the Praileaitz cave there are evident signs of deterioration of different types and generatio...
Siga se izloča kot sekudarni jamski mineral, njeno notranjo zgradbo lahko preučujemo z mineraloškimi...
Cave Minerals of the World, second edition, is a book about cave minerals and speleothems. A speleo...
Mineral ontogeny is the study of the growth and development of mineral deposits in general and, in t...
The classification scheme of Hill and Forti, as used in the second edition of Cave Minerals of the W...
Caves are among Earth\u27s most important minerogenetic environments and they host over 350 minerals...
Secondary minerals forming speleothems are called “cave minerals” and are the results of complex int...
none1noCaves are amongst the Earth most important minerogenetic environments and actually over 300 m...
For many years gypsum karst was considered to contain little of interest from the point of view of c...
Water trickling through the discontinuities of granitic massifs causes a slow chemical and physical ...
A variety of speleothems are present in crevice and boulder caves developed in Cretaceous sandstones...
With the discovery of the József-hegy Cave, a cave of hydrothermal origin with an abundance of miner...
Satisfactory explanation of the origin and development of caves (speleogenesis) is a core problem of...
Satisfactory explanation of the origin and development of caves (speleogenesis) is a core problem of...
A procedure using a scanning electron microscope (SEM) with mineral detection was developed to deter...
Within the Praileaitz cave there are evident signs of deterioration of different types and generatio...
Siga se izloča kot sekudarni jamski mineral, njeno notranjo zgradbo lahko preučujemo z mineraloškimi...
Cave Minerals of the World, second edition, is a book about cave minerals and speleothems. A speleo...
Mineral ontogeny is the study of the growth and development of mineral deposits in general and, in t...
The classification scheme of Hill and Forti, as used in the second edition of Cave Minerals of the W...
Caves are among Earth\u27s most important minerogenetic environments and they host over 350 minerals...
Secondary minerals forming speleothems are called “cave minerals” and are the results of complex int...
none1noCaves are amongst the Earth most important minerogenetic environments and actually over 300 m...
For many years gypsum karst was considered to contain little of interest from the point of view of c...
Water trickling through the discontinuities of granitic massifs causes a slow chemical and physical ...
A variety of speleothems are present in crevice and boulder caves developed in Cretaceous sandstones...
With the discovery of the József-hegy Cave, a cave of hydrothermal origin with an abundance of miner...
Satisfactory explanation of the origin and development of caves (speleogenesis) is a core problem of...
Satisfactory explanation of the origin and development of caves (speleogenesis) is a core problem of...
A procedure using a scanning electron microscope (SEM) with mineral detection was developed to deter...
Within the Praileaitz cave there are evident signs of deterioration of different types and generatio...