Thermal history along the Araçuaí Orogen and São Francisco Craton border, eastern Brazilian continental margin, based on low-temperature thermochronologic data - ScienceDirect
Por um escritor misterioso
Last updated 26 março 2025


Exhumation of the passive margin of the DR Congo during pre- and post- Gondwana breakup: Evidence from low-temperature thermochronology, geology and geomorphology - ScienceDirect

PDF) New insights from low-temperature thermochronology into the tectonic and geomorphologic evolution of the south-eastern Brazilian highlands and passive margin

An example of a Neoproterozoic hyperextended margin: An integrated perspective of the basic magmatism recorded in the Andrelândia Basin, central Ribeira Orogen, SE-Brazil - ScienceDirect

Asymmetric continental deformation during South Atlantic rifting along southern Brazil and Namibia - ScienceDirect

The southeast Brazilian rifted continental margin is not a single, continuous upwarp: Variations in morphology and denudation patterns along the continental drainage divide - ScienceDirect

PDF) Denudation history of the Bocaina Plateau, Serra do Mar, southeastern Brazil: Relationships to Gondwana breakup and passive margin development

Crustal architecture of Neoproterozoic terrains of western Gondwana revealed by integrated geophysical and structural data on the eastern Borborema Province, NE Brazil - ScienceDirect

Exhumation of the passive margin of the DR Congo during pre- and post- Gondwana breakup: Evidence from low-temperature thermochronology, geology and geomorphology - ScienceDirect

Decratonization by rifting enables orogenic reworking and transcurrent dispersal of old terranes in NE Brazil

Significance of age periodicity in the continental crust record: The São Francisco Craton and adjacent Neoproterozoic orogens as a case study - ScienceDirect

Control of inherited structural fabric on the development and exhumation of passive margins – Insights from the Araçuaí Orogen (Brazil) - ScienceDirect

PDF) Diachronic collision, slab break-off and long-term high thermal flux inthe Brasiliano–Pan-African orogeny: Implications for the geodynamicevolution of the Mantiqueira Province
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