A Late Proterozoic-Early Paleozoic magmatic cycle in Sierra de la Ventana, Argentina.

DANIEL ALFREDO GREGORI; LOPEZ, VANINA; GRECCO, LAURA EDITH

Journal of South America Earth Sciences.

Elsevier

Lugar: Oxford , Inglaterra; Año: 2005 vol. 19 p. 155 - 171

Late Proterozoic–Early Paleozoic intrusive and volcanic rocks of Sierra de la Ventana can be grouped into two magmatic assemblages: the Meyer and Cochenleufu´ suites. The older (700–570 Ma) is composed of S-type quartz-monzodiorites, synogranites, and monzogranites associated with andesites and rhyolites and related to volcanic-arc and postcollisional settings. The younger (540–470 Ma) corresponds to highly fractionated homogeneous A-type monzogranites, linked to final plutonic events during postorogenic extension in collisional belts. Strong similarities between Sierra de la Ventana magmatic rocks and the S- and A-type granites of the Cape granite suite in South Africa allow positive correlation. In both areas, primitive volcanic arcs or collisional orogens are recognized. Continuous transpressional shearing between the Swartland and Tygerberg terranes in the Saldania belt may have triggered the generation and emplacement of both suites.