@article{10272/13340,
year = {1996},
url = {http://hdl.handle.net/10272/13340},
abstract = {The sulphides of Latedo-Sejas are mainly constituted of pyrite-pyrrhotite and, on the basis of their textural and structural characteristics, two mineralógicaI stages have been differentiated: syn-diagenetic and/or metamorphic (before or syn-phase 1) and syn-phase 3. The mineralization is associated to two processes of alteration: carbonatization and chloritization. Owe to S34S values, a biogenic origin can be attributed to these sulphides with greater hydrothermal contamination in Latedo. The changes in 8 34S values are due to the transit from a deep anoxic to another shallow and coastal environment in the sedimentary basin},
publisher = {Sociedad Geológica de España},
keywords = {8 34S},
keywords = {Sedimentary sulphides},
keywords = {Silurian},
keywords = {Zamora},
title = {834S de los sulfuros silúricos tipo "sedex" de Latedo-Sejas de Aliste (Zamora, España)},
title = {8 34S of the "sedex" type Silurian sulphides of Latedo-Sejas de Aliste (Zamora, Spain)},
author = {Timón, S. M. and Moro Benito, M. C. and Fernández Fernández, A.},
}