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Quartz veins in metamorphic basement rocks document periods of hydrous fluid mobility. Here, we present a study of vein formation in the Agly Massif, eastern French Pyrenees, which was subjected to metamorphism during the Hercynian and Alpine orogeni
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::375aece639f68caca3214804ea8758cc
https://doi.org/10.5194/egusphere-egu23-5808
https://doi.org/10.5194/egusphere-egu23-5808
