Permo-Carboniferous hypabyssal magmatism in northern Portugal: the case of the Lamas de Olo microgranite and lamprophyre dykes
Author:
Funder
Fundação para a Ciência e a Tecnologia
Publisher
Springer Science and Business Media LLC
Subject
Stratigraphy,Geology
Link
https://link.springer.com/content/pdf/10.1007/s41513-021-00179-8.pdf
Reference100 articles.
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2. Allègre, C. J., & Minster, J. F. (1978). Quantitative models of trace element behavior in magmatic processes. Earth and Planetary Science Letters, 38(1), 1–25. https://doi.org/10.1016/0012-821X(78)90123-1
3. Almeida, A., Leterrier, J., Noronha, F., & Bertrand, J. M. (1998). U–Pb zircon and monazite geochronology of the Hercynian two-mica granite composite pluton of Cabeceiras de Basto (Northern Portugal). Comptes Rendus De L’academie Des Sciences, Serie II, Fascicule a, Earth and Planetary Sciences, 326(11), 779–785. https://doi.org/10.1016/s1251-8050(98)80243-7
4. Ballouard, C., Poujol, M., Boulvais, P., Branquet, Y., Tartese, R., & Vigneresse, J. L. (2016). Nb–Ta fractionation in peraluminous granites: A marker of the magmatic-hydrothermal transition. Geology, 44(3), 231–234. https://doi.org/10.1130/G37475.1
5. Batchelor, R. A., & Bowden, P. (1985). Petrogenetic interpretation of granitoid rock series using multicationic parameters. Chemical Geology, 48(1–4), 43–55. https://doi.org/10.1016/0009-2541(85)90034-8
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