Te-Rich argyrodite occurrence in Roşia Montană ore deposit, Apuseni Mountains, Romania
| Autor: | Adrian Minuţ, Călin Gabriel Tămaş, Laurent Bailly |
|---|---|
| Přispěvatelé: | Bureau de Recherches Géologiques et Minières (BRGM) (BRGM), Travaux et recherches archéologiques sur les cultures, les espaces et les sociétés (TRACES), École des hautes études en sciences sociales (EHESS)-Université Toulouse - Jean Jaurès (UT2J)-Ministère de la Culture et de la Communication (MCC)-Centre National de la Recherche Scientifique (CNRS) |
| Jazyk: | angličtina |
| Rok vydání: | 2005 |
| Předmět: |
Global and Planetary Change
010504 meteorology & atmospheric sciences Hessite Argyrodite Geochemistry Mineralogy engineering.material Canfieldite 010502 geochemistry & geophysics 01 natural sciences Alabandite Sphalerite Altaite Galena engineering General Earth and Planetary Sciences Marcasite Geology ComputingMilieux_MISCELLANEOUS 0105 earth and related environmental sciences [SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy |
| Zdroj: | Comptes Rendus Géoscience Comptes Rendus Géoscience, Elsevier, 2005, 337 (8), pp.755-762 |
| Popis: | A new argyrodite occurrence has been discovered in the Rosia Montana ore deposit located in the South Apuseni Mountains, Romania. Argyrodite is associated with common base metal sulfides and sulfosalts (galena, sphalerite, chalcopyrite, tetrahedrite ± alabandite, pyrite, and marcasite), tellurides (hessite, altaite, sylvanite) and rare electrum grains in the Ag-rich Cârnicel vein hosted by an extracraterial phreatomagmatic breccia within the Cârnic massif. SEM and EPMA analyses revealed that this argyrodite is Te-rich and a mean Ag 8.04 Ge 0.9 Te 2.07 S 3.77 formula was calculated. This phase could be the germaniferous equivalent of the previously-described Te-rich canfieldite. To cite this article: L. Bailly et al., C. R. Geoscience 337 (2005). |
| Databáze: | OpenAIRE |
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