Add to ORKG“Reaction microtextures in blackwall zones, Río de Las Tunas mafic-ultramafic belt, Cor- dillera Frontal of Mendoza”. Reaction microtextures developed in the chlorite blackwall zones located in between bodies from Río de Las Tunas mafic- utramafic belt and schist country rock were stud- ied in this contribution. The outcrops belong to the Cordillera Frontal of Mendoza province. The studied microtextures are developed in porfiroblasts com- pletely replaced by chlorite. Around these porfirob- lasts is observed a rim with microvermiform spinel s.l. aggregates in reaction with chlorite and magnetite groundmass. Small amphibole porfirob- lasts with chemical zoning is superimposed to these reaction rims. The studied microtextures can be explained...
La zona de alteración Arroyo La Chilca-Zanjón del Buitre está ubicada en el bloque de San Rafael (35...
The ranges of the Sierras Valle Fértil-La Huerta expose natural cross sections through a paleo-arc c...
En el extremo sur de la Cordillera Principal entre los 35º-36ºLS, los depósitos sinorogénicos y los ...
Talc mineralization related to the ultramafic bodies of the Río de Las Tunas belt, Frontal Cordiller...
Absbvct- New petrographic and chemical data of volcanic rocks from the Metales Belt, Rio de las Tuna...
In the Río de Las Tunas belt, Central Andes of Argentina, spinel group minerals occur in metaperidot...
The Sierras de San Luis, which are part of the Sierras Pampeanas, are located in Central Argentina. ...
The Cuesta de Randolfo mylonite zone (CRMZ) in the southern Puna of Argentina comprises ≥6-km of mod...
Mineralogy of several samples from the Viñuela Formation,Lower Burdigalian (Vélez Málaga, Cordillera...
The Frontal Cordillera Composite Batholith (FCCB) is made up of a string of granitic plutons thought...
En la localidad de Salagasta, ubicada en el extremo austral de la Sierra de La Higuera, provincia de...
Mylonite with a big delta mantled porphyroclast of K-feldspar in a matrix of quartz, mica and feldsp...
In central-western Argentina, a mafic-ultramafic belt occurs throughout the western margin of the Pr...
A petrological and geochemical study was performed on rock samples collected from the retro-arc, Pay...
In the Río de Las Tunas belt, Central Andes of Argentina, spinel group minerals occur in metaperidot...
La zona de alteración Arroyo La Chilca-Zanjón del Buitre está ubicada en el bloque de San Rafael (35...
The ranges of the Sierras Valle Fértil-La Huerta expose natural cross sections through a paleo-arc c...
En el extremo sur de la Cordillera Principal entre los 35º-36ºLS, los depósitos sinorogénicos y los ...
Talc mineralization related to the ultramafic bodies of the Río de Las Tunas belt, Frontal Cordiller...
Absbvct- New petrographic and chemical data of volcanic rocks from the Metales Belt, Rio de las Tuna...
In the Río de Las Tunas belt, Central Andes of Argentina, spinel group minerals occur in metaperidot...
The Sierras de San Luis, which are part of the Sierras Pampeanas, are located in Central Argentina. ...
The Cuesta de Randolfo mylonite zone (CRMZ) in the southern Puna of Argentina comprises ≥6-km of mod...
Mineralogy of several samples from the Viñuela Formation,Lower Burdigalian (Vélez Málaga, Cordillera...
The Frontal Cordillera Composite Batholith (FCCB) is made up of a string of granitic plutons thought...
En la localidad de Salagasta, ubicada en el extremo austral de la Sierra de La Higuera, provincia de...
Mylonite with a big delta mantled porphyroclast of K-feldspar in a matrix of quartz, mica and feldsp...
In central-western Argentina, a mafic-ultramafic belt occurs throughout the western margin of the Pr...
A petrological and geochemical study was performed on rock samples collected from the retro-arc, Pay...
In the Río de Las Tunas belt, Central Andes of Argentina, spinel group minerals occur in metaperidot...
La zona de alteración Arroyo La Chilca-Zanjón del Buitre está ubicada en el bloque de San Rafael (35...
The ranges of the Sierras Valle Fértil-La Huerta expose natural cross sections through a paleo-arc c...
En el extremo sur de la Cordillera Principal entre los 35º-36ºLS, los depósitos sinorogénicos y los ...