Middle Triassic trachytic lava flows associated with coeval dyke swarm in the North Patagonian Massif: A postorogenic magmatism related to extensional collapse of the Gondwanide orogen-Reference-Cited by-同舟云学术

Middle Triassic trachytic lava flows associated with coeval dyke swarm in the North Patagonian Massif: A postorogenic magmatism related to extensional collapse of the Gondwanide orogen

Published:2017-04 Issue: Volume:75 Page:134-143
ISSN:0895-9811
Container-title:Journal of South American Earth Sciences
language:en
Short-container-title:Journal of South American Earth Sciences

Author:

González Santiago N.,Greco Gerson A.,Sato Ana M.,Llambías Eduardo J.,Basei Miguel A.S.^ORCID,González Pablo D.,Díaz Pablo E.^ORCID

Funder

Universidad Nacional de La Plata, UNLP

Consejo Nacional de Investigaciones Científicas y Técnicas

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

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3. Estudio sistemático de la tafoflora triásica de Los Menucos, provincia de Río Negro. Parte I. Sphenophyta, Filicophyta, Pteridospermophyta;Artabe;Ameghiniana,1985

4. Continental delamination and the Colorado plateau;Bird;J. Geophys. Res. Solid Earth,1979

5. Cratons, mobile belts, alkaline rocks and continental lithospheric mantle: the Pan-African testimony;Black;J. Geol. Soc.,1993

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