Granitoides paleozoicos de la Sierra de Narváez, Sistema de Famatina, Argentina: Hibridización de magmas en un margen continental activo

C. E. Cisterna

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DOI: 10.3989/egeol.92485-6389
Published: 12
Container: Estudios Geologicos
Publisher: Not recorded
Open access: yes

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Cite this work

BibTeX

@article{allodium:10.3989/egeol.92485-6389,
  title = {Granitoides paleozoicos de la Sierra de Narváez, Sistema de Famatina, Argentina: Hibridización de magmas en un margen continental activo},
  author = {C. E. Cisterna},
  year = {1992},
  journal = {Estudios Geologicos},
  doi = {10.3989/egeol.92485-6389},
  url = {https://doi.org/10.3989/egeol.92485-6389}
}

RIS

TY  - JOUR
TI  - Granitoides paleozoicos de la Sierra de Narváez, Sistema de Famatina, Argentina: Hibridización de magmas en un margen continental activo
AU  - C. E. Cisterna
PY  - 1992
JO  - Estudios Geologicos
DO  - 10.3989/egeol.92485-6389
UR  - https://doi.org/10.3989/egeol.92485-6389
ER  -

APA

Cisterna, C. E. (1992). Granitoides paleozoicos de la Sierra de Narváez, Sistema de Famatina, Argentina: Hibridización de magmas en un margen continental activo. Estudios Geologicos. https://doi.org/10.3989/egeol.92485-6389

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doaj · retrieved 2026-09-27T04:04:18.394Z