Add to ORKGSilica speleothems take differenr forms such as cylindrical stems growing from either the floor or the ceiling in granitic caves. Mineralogically they are opal-A and accumulate in successive layers with a whiskery druse tip formed by gypsum crystals. Initially they are porous but progressively become infilled by opal precipitation. This results in formation of solid speleothems. their size is only a few millimetres long. Bacterial activity accelerate quartz dissolutio
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 caves of Naica (Chihuahua, Mexico) are perhaps the most famous mine caves of the world due to th...
Meteoric waters infiltrate along fractures and fissures in granitic massifs. Bacteria in the waters ...
The amorphous silica (opal-A) speleothems associated to the open structural system of granitic rocks...
Granite massifs often contain caves, with dimensions ranging from a few meters up to 1,000 m, also r...
The present communication characterizes and discusses the genesis of cave speleothems developed in F...
Water trickling through the discontinuities of granitic massifs causes a slow chemical and physical ...
Siliceous, opal-A speleothems of the Chimalacatepec lava tube system in central Mexico are character...
peer reviewedBol. Soc. Venezolana Espel. v.39 Caracas dic. 2005 ®download el artículo en el forma...
11 páginas.-- 8 figuras.-- 1 tabla.-- 33 referenciasCoralloid-type speleothems were recorded on the ...
A cave in granitic rocks was studied in Mezesse, South Cameroon. Coralloid speleothems, draperies an...
[Abstract] Granite massifs often contain caves, with dimensions ranging from a few meters up to 1,00...
The largest and longest silicate caves in the world created in arenites of the Roraima Group in Vene...
In March 2009 the Guacamaya Cave was discovered on the Auyan Tepui. It represents one of the longest...
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 caves of Naica (Chihuahua, Mexico) are perhaps the most famous mine caves of the world due to th...
Meteoric waters infiltrate along fractures and fissures in granitic massifs. Bacteria in the waters ...
The amorphous silica (opal-A) speleothems associated to the open structural system of granitic rocks...
Granite massifs often contain caves, with dimensions ranging from a few meters up to 1,000 m, also r...
The present communication characterizes and discusses the genesis of cave speleothems developed in F...
Water trickling through the discontinuities of granitic massifs causes a slow chemical and physical ...
Siliceous, opal-A speleothems of the Chimalacatepec lava tube system in central Mexico are character...
peer reviewedBol. Soc. Venezolana Espel. v.39 Caracas dic. 2005 ®download el artículo en el forma...
11 páginas.-- 8 figuras.-- 1 tabla.-- 33 referenciasCoralloid-type speleothems were recorded on the ...
A cave in granitic rocks was studied in Mezesse, South Cameroon. Coralloid speleothems, draperies an...
[Abstract] Granite massifs often contain caves, with dimensions ranging from a few meters up to 1,00...
The largest and longest silicate caves in the world created in arenites of the Roraima Group in Vene...
In March 2009 the Guacamaya Cave was discovered on the Auyan Tepui. It represents one of the longest...
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 caves of Naica (Chihuahua, Mexico) are perhaps the most famous mine caves of the world due to th...