2026-04-13T02:24:02Zhttps://recercat.cat/oai/requestoai:recercat.cat:2445/181752025-12-05T14:31:43Zcom_2072_1057col_2072_478917col_2072_478923
RECERCAT
author
Cardellach López, Esteve
author
Canals i Sabaté, Àngels
author
Tritlla i Cambra, Jordi
2011-05-25T10:48:51Z2011-05-25T10:48:51Z1990
Many of the veins enclosed within the Paleozoic basement of the Catalonian Coastal Ranges show severa1 common characteristics: low temperature of formation (between 75 and 200C), the presence of complex polisaline fluids and a certain relationship to the pretriassic paleosurface. Mineralogical composition and age are variable, ranging from Pb-Zn veins with carbonate gangue of late Hercynian age through metal poor fluorite rich veins to barite rich veins of Triasssic age. Mineralizing fluids are not related to late Hercynianmagmatism and deposition took place in active fractures developed either in extensional as in compressive regimes.
(c) Cardellach, et al., 1990 info:eu-repo/semantics/openAccess
Serralada Litoral Catalana
Mineralogia
Catalan Coastal Range (Catalonia)
Mineralogy
Late and post-Hercyniam low temperature veins in the Catalonian Coastal Ranges
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion