2026-04-13T08:32:26Zhttps://recercat.cat/oai/request

oai:recercat.cat:2445/181752025-12-05T14:31:43Zcom_2072_1057col_2072_478917col_2072_478923

00925njm 22002777a 4500 dc Cardellach López, Esteve author Canals i Sabaté, Àngels author Tritlla i Cambra, Jordi author 2011-05-25T10:48:51Z 2011-05-25T10:48:51Z 1990 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. Serralada Litoral Catalana Mineralogia Catalan Coastal Range (Catalonia) Mineralogy Late and post-Hercyniam low temperature veins in the Catalonian Coastal Ranges