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Romero, Rurik, Barra, Fernando, Leisen, Mathieu, Salazar, Eduardo, González-Jiménez, José María, Reich, Martin (2020) Sedimentary provenance of the Late Paleozoic metamorphic basement, south-central Chile: Implications for the evolution of the western margin of Gondwana. International Geology Review, 62 (5) 598-613 doi:10.1080/00206814.2019.1627589

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Reference TypeJournal (article/letter/editorial)
TitleSedimentary provenance of the Late Paleozoic metamorphic basement, south-central Chile: Implications for the evolution of the western margin of Gondwana
JournalInternational Geology Review
AuthorsRomero, RurikAuthor
Barra, FernandoAuthor
Leisen, MathieuAuthor
Salazar, EduardoAuthor
González-Jiménez, José MaríaAuthor
Reich, MartinAuthor
Year2020 (March 23)Volume62
Issue5
PublisherInforma UK Limited
DOIdoi:10.1080/00206814.2019.1627589Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID308950Long-form Identifiermindat:1:5:308950:1
GUID0
Full ReferenceRomero, Rurik, Barra, Fernando, Leisen, Mathieu, Salazar, Eduardo, González-Jiménez, José María, Reich, Martin (2020) Sedimentary provenance of the Late Paleozoic metamorphic basement, south-central Chile: Implications for the evolution of the western margin of Gondwana. International Geology Review, 62 (5) 598-613 doi:10.1080/00206814.2019.1627589
Plain TextRomero, Rurik, Barra, Fernando, Leisen, Mathieu, Salazar, Eduardo, González-Jiménez, José María, Reich, Martin (2020) Sedimentary provenance of the Late Paleozoic metamorphic basement, south-central Chile: Implications for the evolution of the western margin of Gondwana. International Geology Review, 62 (5) 598-613 doi:10.1080/00206814.2019.1627589
In(2020, March) International Geology Review Vol. 62 (5) Informa UK Limited

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González-Jiménez, José María, Barra, Fernando, Walker, Richard J., Reich, Martin, Gervilla, Fernando (2014) Geodynamic implications of ophiolitic chromitites in the La Cabaña ultramafic bodies, Central Chile. International Geology Review, 56 (12) 1466-1483 doi:10.1080/00206814.2014.947334
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