In the Sierra de San Luis, Central Argentina, a belt of small and discontinuous lenses of mafic-ultramafic rocks intrude a polydeformed basement and are thought to be the cause of a local increase of the metamorphic grade from amphibolite to granulite facies conditions. This assumption was especially based on forward modelling of a huge gravity anomaly centered over the Sierra de San Luis, which lead some workers to think that a vast volume of mafic-ultramafic rocks lay in shallow levels. Here, we propose an alternative model to explain this anomaly, in which the mafic-ultramafic intrusion is not the ultimate source. Therefore, there is no need to propose a bigger size than that observed in outcrops for the mafic-ultramafic bodies. The ther...
New petrologic, thermobarometric and U-Pb monazite geochronologic information allowed to resolve the...
Magmatic structures related to the mechanical interaction between mafic magmas and granitoids have b...
The Sierra Valle Fértil Complex of west-central Argentina represents a section of the Ordovician (~4...
The Sierras de San Luis, which are part of the Sierras Pampeanas, are located in Central Argentina. ...
At La Melada, Sierra de San Luis, Argentina, two lenses of mafic-ultramafic rocks, which underwent F...
Argentina. The crystalline basement of the Sierras de San Luis is built up of three main blocks (wes...
The Virorco layered mafic-ultramafic intrusion is part of a belt that extends over 100 km from NE to...
This paper presents the results of a geophysical study of the southern portion of the Sierra Grande ...
El área de estudio comprende el sector central de las Las Sierras Grandes de San Luis, situadas en e...
This thesis investigated the evolution of a high temperature, low pressure crustal block of the Late...
This thesis investigated the evolution of a high temperature, low pressure crustal block of the Late...
The ranges of the Sierras Valle Fértil-La Huerta expose natural cross sections through a paleo-arc c...
In central-western Argentina, a mafic-ultramafic belt occurs throughout the western margin of the Pr...
At La Melada, Sierra de San Luis, Argentina, two lenses of mafic-ultramafic rocks, mainly consisting...
At La Melada, Sierra de San Luis, Argentina, two lenses of mafic-ultramafic rocks, mainly consisting...
New petrologic, thermobarometric and U-Pb monazite geochronologic information allowed to resolve the...
Magmatic structures related to the mechanical interaction between mafic magmas and granitoids have b...
The Sierra Valle Fértil Complex of west-central Argentina represents a section of the Ordovician (~4...
The Sierras de San Luis, which are part of the Sierras Pampeanas, are located in Central Argentina. ...
At La Melada, Sierra de San Luis, Argentina, two lenses of mafic-ultramafic rocks, which underwent F...
Argentina. The crystalline basement of the Sierras de San Luis is built up of three main blocks (wes...
The Virorco layered mafic-ultramafic intrusion is part of a belt that extends over 100 km from NE to...
This paper presents the results of a geophysical study of the southern portion of the Sierra Grande ...
El área de estudio comprende el sector central de las Las Sierras Grandes de San Luis, situadas en e...
This thesis investigated the evolution of a high temperature, low pressure crustal block of the Late...
This thesis investigated the evolution of a high temperature, low pressure crustal block of the Late...
The ranges of the Sierras Valle Fértil-La Huerta expose natural cross sections through a paleo-arc c...
In central-western Argentina, a mafic-ultramafic belt occurs throughout the western margin of the Pr...
At La Melada, Sierra de San Luis, Argentina, two lenses of mafic-ultramafic rocks, mainly consisting...
At La Melada, Sierra de San Luis, Argentina, two lenses of mafic-ultramafic rocks, mainly consisting...
New petrologic, thermobarometric and U-Pb monazite geochronologic information allowed to resolve the...
Magmatic structures related to the mechanical interaction between mafic magmas and granitoids have b...
The Sierra Valle Fértil Complex of west-central Argentina represents a section of the Ordovician (~4...