 | Mateo, Ester, Fanlo, Isabel, Subías, Ignacio, Recio, Clemente, Billström, Kjell (2010) Geological, mineralogical and geochemical constraints on the genesis of the Chinipí arsenopyrite-pyrite-invisible gold vein (Canfranc, Central Spanish Pyrenees) Neues Jahrbuch für Mineralogie - Abhandlungen, 187 (3) 313-327 doi:10.1127/0077-7757/2010/0182 | Journal (article/letter/editorial) | | on the genesis of the Chinipí arsenopyrite-pyrite-invisible gold vein (Canfranc, Central Spanish Pyrenees)...tables Abstract. The sulphidic ore deposit of Chinipí, hosted by early Carboniferous limestones, is related...Variscan basement. In the preferred model the Chinipí vein formation was favoured by a transtensional...metasediments located in the Eastern Pyrenees. The Chinipí deposit is unique among the above groups in that...Anayet Massif located a few kilometres north of the Chinipí deposit (Fig. 1b). These rocks developed under |  | | Journal (article/letter/editorial) | | Cerbuna, 12 (Edificio Geológicas), 50009 Zaragoza, Spain Department of Geological Sciences, Swedish Museum...Geological synthesis Outcrops of pre-Mesozoic rocks in Spain form various massifs that relate to both Variscan...as well as rare pyrite, sphalerite, galena and siderite. It should be mentioned that in addition to the...and geochemical evidences supporting that the Chinipí vein deposit, a 244 I. Subías et al. / Ore Geology...those deposits located in the Variscan portion of Spain (see Figs. 1A and 5A for localization of mineralizations) |
|
