The polyphase evolution of the Seridó Belt (NE-Brazil) includes D1 crust formation at 2.3-2.1 Ga, D2 thrust tectonics at 1.9 Ga and crustal reworking by D3 strike-slip shear zones at 600 Ma. Microstructural investigations within mylonites associated with D2 and D3 events were used to constrain the tectono-thermal evolution of the belt. D2 shear zones commenced at deeper crustal levels and high amphibolite facies conditions (600-650 °C) through grain boundary migration, subgrain rotation and operation of quartz 〈c〉-prism slip. Continued shearing and exhumation of the terrain forced the re-equilibration of high-T fabrics and the switching of slip systems from 〈c〉-prism to positive and negative 〈a〉-rhombs. During D3, enhancement of ductility b...
Field relationships, geochemistry and U-Pb zircon and Sm-Nd whole-rock geochronology are used to con...
The different tectonic stages that occurred at the end of the Proterozoic and during the Phanerozoic...
The Marília Formation, which crops out in southeastern Brazil, is interpreted as a Late Cretaceous e...
Chemical analyses suggest that the metavolcanic rocks of the Almas Greenstone Belt (AGB), Tocantins ...
Recent structural investigations and geochronological studies of rocks from the Médio Coreaú domain ...
The São Francisco shield is one of the major cratonic units forming the backbone of the South Americ...
Mafic rocks are often the key to magmatic and metamorphic processes that take place deep within the ...
Subvertical quartzites and pelitic schists crop out in structural conformity with gneisses and migma...
The Vazante Group hosts the Vazante nonsulfide zinc deposit, which comprises high-grade zinc silicat...
Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)The São Francisco Craton (SFC) is an Ar...
Fifteen multi-dimensional diagrams for basic and ultrabasic rocks, based on log-ratio transformation...
Prior to the tectonic events related to the opening of the Central Atlantic, the Mosquito Formation ...
The Sergipano belt is the outcome of collision between the Pernambuco-Alagoas Domain (Massif) and th...
Geochemical and oxygen isotopic data on the Neoproterozoic granulite facies rocks (enderbites, charn...
The trace element composition of high-grade metamorphic rocks in the Guaxupé Massif is investigated....
Field relationships, geochemistry and U-Pb zircon and Sm-Nd whole-rock geochronology are used to con...
The different tectonic stages that occurred at the end of the Proterozoic and during the Phanerozoic...
The Marília Formation, which crops out in southeastern Brazil, is interpreted as a Late Cretaceous e...
Chemical analyses suggest that the metavolcanic rocks of the Almas Greenstone Belt (AGB), Tocantins ...
Recent structural investigations and geochronological studies of rocks from the Médio Coreaú domain ...
The São Francisco shield is one of the major cratonic units forming the backbone of the South Americ...
Mafic rocks are often the key to magmatic and metamorphic processes that take place deep within the ...
Subvertical quartzites and pelitic schists crop out in structural conformity with gneisses and migma...
The Vazante Group hosts the Vazante nonsulfide zinc deposit, which comprises high-grade zinc silicat...
Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)The São Francisco Craton (SFC) is an Ar...
Fifteen multi-dimensional diagrams for basic and ultrabasic rocks, based on log-ratio transformation...
Prior to the tectonic events related to the opening of the Central Atlantic, the Mosquito Formation ...
The Sergipano belt is the outcome of collision between the Pernambuco-Alagoas Domain (Massif) and th...
Geochemical and oxygen isotopic data on the Neoproterozoic granulite facies rocks (enderbites, charn...
The trace element composition of high-grade metamorphic rocks in the Guaxupé Massif is investigated....
Field relationships, geochemistry and U-Pb zircon and Sm-Nd whole-rock geochronology are used to con...
The different tectonic stages that occurred at the end of the Proterozoic and during the Phanerozoic...
The Marília Formation, which crops out in southeastern Brazil, is interpreted as a Late Cretaceous e...