The East African Orogen involves a collage of Proterozoic microcontinents and arc terranes that became wedged between older cratonic blocks during the assembly of Gondwana. The Ediacaran–Cambrian Ambalavao and Maevarano Suites in Madagascar were emplaced during the waning orogenic stages and consist of weakly deformed to undeformed plutonic rocks and dykes of mainly porphyritic granite but also gabbro, diorite and charnockite. U-Pb geochronological data date emplacement of the Ambalavao Suite to between ca. 580 Ma and 540 Ma and the Maevarano Suite to between ca. 537 Ma and 522 Ma. Major and trace element concentrations are consistent with emplacement in a syn- to post-collisional tectonic setting as A-type (anorogenic) suites. Oxygen (δ¹⁸O...
New detrital zircon U-Pb age data obtained from various quartzite units of three spatially separate...
International audienceMadagascar is a key area for unraveling the geodynamic evolution of the transi...
International audienceThe widespread ∼800 Ma Imorona–Itsindro magmatic suite of Central Madagascar c...
Madagascar occupies an important location in many Proterozoic plate reconstructions. It lies within ...
Madagascar occupies an important location within the East African Orogen (EAO). The EAO comprises an...
Madagascar is a key area for unraveling the geodynamic evolution of the transition between the Rodin...
Madagascar occupies an important location within the East African Orogen (EAO), which involves a col...
Our recent geological survey of the basement of central and northern Madagascar allowed us to re-ev...
International audienceThe stratoid granites of Madagascar are sheet-like granite sills emplaced conf...
New detrital zircon U-Pb age data obtained from various quartzite units of three spatially separate...
International audienceMadagascar is a key area for unraveling the geodynamic evolution of the transi...
International audienceThe widespread ∼800 Ma Imorona–Itsindro magmatic suite of Central Madagascar c...
Madagascar occupies an important location in many Proterozoic plate reconstructions. It lies within ...
Madagascar occupies an important location within the East African Orogen (EAO). The EAO comprises an...
Madagascar is a key area for unraveling the geodynamic evolution of the transition between the Rodin...
Madagascar occupies an important location within the East African Orogen (EAO), which involves a col...
Our recent geological survey of the basement of central and northern Madagascar allowed us to re-ev...
International audienceThe stratoid granites of Madagascar are sheet-like granite sills emplaced conf...
New detrital zircon U-Pb age data obtained from various quartzite units of three spatially separate...
International audienceMadagascar is a key area for unraveling the geodynamic evolution of the transi...
International audienceThe widespread ∼800 Ma Imorona–Itsindro magmatic suite of Central Madagascar c...