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High resolution geochemical mapping in the Mociços mine (Ossa-Morena Zone, Portugal). [PDF]

open access: possible, 2022
The Mociços mine is a Cu-rich quartz-carbonate vein-type deposit hosted in the Palaeozoic detrital metasediments of the Ossa-Morena Zone (SW Portugal), exploited during the beginning of the XX century. A soil geochemistry campaign was carried out, with a portable X-Ray Fluorescence, in order to estimate metal distribution throughout the Mociços mine ...
Nogueira, Pedro   +5 more
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Early Paleozoic rifting and bimodal volcanism in the Ossa-Morena Zone of south-west Spain

Geologische Rundschau, 1994
Lower Paleozoic volcanic members have been investigated by geological, petrographical and geochemical means in a traverse across the Ossa-Morena Zone (OMZ) in south-west Spain.
Uwe Giese, Bernhard B�hn
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Geochemistry and paleotectonic setting of Ediacaran metabasites from the Ossa-Morena Zone (SW Iberia)

International Journal of Earth Sciences, 2013
New results on the geochemistry of Neoproterozoic (late Ediacaran) metabasites of the Ossa-Morena Zone (OMZ, Iberian Massif) are presented. The metabasite suite exhibits N- and E-MORB signatures, as well as volcanic arc signatures. The three amphibolite groups are discerned on the basis of major and trace element contents, and the Nd isotope relations ...
M. E. Sánchez Lorda   +5 more
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Fluid constraints in the Miguel Vacas Cu deposit (Ossa-Morena Zone, Portugal)

2019
The ancient Miguel Vacas copper mine belongs to a cluster of ancient Cu mines and occurrences in the Ossa-Morena Zone, specifically in the Sousel-Barrancos metallogenic belt (SBMB), such as Mociços, Ferrarias and Bugalho. This deposit is characterised by an anastomosing vein structure mainly composed of quartz + carbonate + sulphides that extends over ...
MAIA, Miguel   +4 more
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Magnetotelluric survey of the electrical conductivity of the crust across the Ossa Morena Zone and South Portuguese Zone suture

Tectonophysics, 1999
Abstract The transition between the South Portuguese Zone (SPZ) and the Ossa Morena Zone (OMZ) is made up of a major geosuture, which is indicated by the Beja-Acebuches ophiolite. Several geological data suggest that this suture is the result of an oblique collision, with a northward propagation, between the SPZ and OMZ.
Fernando A. Monteiro Santos   +6 more
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Application of unsupervised machine learning techniques for lithological and soil mapping in Ossa-Morena Zone

2022
<p>Unsupervised methods are a good entry point for satellite image classification, requiring little to no input, and outputting an analysis, in the form of a thematic map, that may act as a guide for more user input intensive methods. For this work, we use K-means methods to classify satellite and drone imagery that cover the Ossa-Morena ...
Marcelo Silva   +3 more
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Cambrian ensialic rift-related magmatism in the Ossa-Morena Zone

2011
The Late Ediacaran (c. 560–550 Ma) Série Negra sediments of the Évora–Aracena metamorphic belt, Ossa-Morena Zone, SW Iberian Massif, preserve a record of the erosion of an Avalonian–Cadomian magmatic arc and subsequent related turbiditic sedimentation. Detrital zircon from the Série Negra is characterized by predominantly Ediacaran and Cryogenian ages,
Chichorro, Martim   +6 more
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Fluid constraints in the Mociços Cu deposit (Ossa-Morena Zone, Portugal)

2020
The Mociços copper deposit is located in the Ossa-Morena Zone, at the Sousel-Barrancos metallogenic belt (SBMB) and belongs to a cluster of ancient Cu mines and occurrences, such as Miguel Vacas, Ferrarias and Bugalho. This deposit is characterised by a main sulphide assemblage of chalcopyrite + pyrite in a quartz + carbonate decametric lode, with an ...
MAIA, Miguel   +5 more
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The structure of a major suture zone in the SW Iberian Massif: the Ossa-Morena/Central Iberian contact

Tectonophysics, 2001
Abstract We have investigated the stratigraphy, structure and metamorphism of the boundary between the Ossa Morena Zone (OMZ) and the Central Iberian Zone (CIZ), two significant continental portions of the Variscan Iberian Massif. The OMZ/CIZ contact is marked by a strongly deformed and metamorphosed NW–SE trending narrow band, namely, the Central ...
J.F. Simancas   +4 more
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Relicts of Rheic Ocean in Southwest Iberia (Ossa-Morena Zone - Portugal)

2010
The geodynamic evolution of Iberian Peninsula during the Variscan Orogeny is directly related with the Wilson Cycle of Rheic Ocean (Vera, 2004; Dias et al., 2006; Ribeiro et al., 2007). This relationship is underlined by major sutures zones and by several occurrences of high pressure metamorphic rocks (i. e.
Pedro, Jorge   +4 more
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