Dating recurrent shear zone activity and the transition from ductile to brittle deformation: White mica geochronology applied to the Neoproterozoic Dom Feliciano Belt in South Brazil-Reference-Cited by-同舟云学术

Dating recurrent shear zone activity and the transition from ductile to brittle deformation: White mica geochronology applied to the Neoproterozoic Dom Feliciano Belt in South Brazil

Published:2020-12 Issue: Volume:141 Page:104199
ISSN:0191-8141
Container-title:Journal of Structural Geology
language:en
Short-container-title:Journal of Structural Geology

Author:

Hueck Mathias,Wemmer Klaus,Basei Miguel A.S.,Philipp Ruy P.,Oriolo Sebastián,Heidelbach Florian,Oyhantçabal Pedro,Siegesmund Siegfried

Funder

FAPESP

CNPq

Publisher

Elsevier BV

Subject

Geology

Reference158 articles.

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3. Tonian emplacement of ophiolites in the southern Brasiliano Orogen delimited by U-Pb-Hf isotopes of zircon from metasomatites;Arena;Gondwana Res.,2017

4. Sequências tectono-sedimentares mesopaleozóicas da Bacia do Paraná, Sul do Brasil;Assine;Rev. Bras. Geociencias,1994

5. U-Pb and Sm-Nd geochronology of the Neoproterozoic granitic-gneissic Dom Feliciano belt, southern Brazil;Babinski;J. S. Am. Earth Sci.,1997

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