Devonian to Permian post-orogenic denudation of the Brasilia Belt of West Gondwana : insights from apatite fission track thermochronology

The Brasilia Belt in southern Brazil is a Neoproterozoic orogenic belt that represents the northern border of the Parana Basin, a long-lived early Paleozoic intracratonic basin. The belt is surrounded by cratonic domains and were modestly affected and reactivated by the opening of the South Atlantic...

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Bibliographic Details
Published in:Journal of Geodynamics
Main Authors: Fonseca, Ana Carolina, Piffer, Gabriella Vago, Nachtergaele, Simon, Van Ranst, Gerben, De Grave, Johan, Novo, Tiago Amancio
Format: Article in Journal/Newspaper
Language:English
Published: 2020
Subjects:
Earth and Environmental Sciences
Low-temperature thermochronology
Erosional denudation
West Gondwana basement
Pre-Andean orogenies
Parana Basin
ASIAN OROGENIC BELT
TECTONIC EVOLUTION
SOUTH-AMERICA
GEOCHRONOLOGICAL CONSTRAINTS
THERMOTECTONIC HISTORY
PRECAMBRIAN BASEMENT
LANDSCAPE EVOLUTION
ANNEALING KINETICS
CONTINENTAL-MARGIN
South Atlantic Ocean
Online Access:https://biblio.ugent.be/publication/8685631
http://hdl.handle.net/1854/LU-8685631
https://doi.org/10.1016/j.jog.2020.101733
https://biblio.ugent.be/publication/8685631/file/8685632
Description
Summary:The Brasilia Belt in southern Brazil is a Neoproterozoic orogenic belt that represents the northern border of the Parana Basin, a long-lived early Paleozoic intracratonic basin. The belt is surrounded by cratonic domains and were modestly affected and reactivated by the opening of the South Atlantic Ocean during the Cretaceous. Here we present new apatite fission track data from crystalline rocks of the Brasilia Belt. The apatite fission track central ages range from 386 to 243 Ma and the mean track lengths range between 13.4 and 14.5 mu m. Thermal history modeling reveals Devonian to Permian cooling, which we interpret as the main final exhumation of the Brasilia Belt, implying that indeed the influence of posterior Mesozoic and Cenozoic geodynamic history on the belt was limited. The Parana Basin and surrounding elevated terranes therefore provide a time window to study the tectonic history of Gondwana and the effect of far-field intraplate stresses on the interior of West Gondwana. Rapid basement exhumation of the Brasilia Belt is coeval with extension and tectonic subsidence in the Parana Basin as a result of continent-scale tectonic forces occurring over entire West Gondwana.

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