Igneous rocks of alpine age associated with Keuper material in the Iberian Mountains, near Teruel (Spain)
DOI:
https://doi.org/10.3989/egeol.84401-2645Keywords:
Transformation processes, Alpine igneous rocks, syenites-monzogabbros.Abstract
In the present work, some rocks of igneous facies associated to Keuper materials, are studied. These rocks, previously referred to as ophites, consist in fact of plutonic rocks, compositionally ranging from syenites to monzogabbros. Field, petrographic and geochemical data appear to indicate that these igneous rocks facies were a consequence of metasomatic transformation processes that took place between allocthonous silica-alkaline elements and suitable wall-rocks, constituted, in this case, of evaporitic marls of Keuper facies.
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Published
1984-04-30
How to Cite
Sánchez Cela, V., & García Anquela, J. A. (1984). Igneous rocks of alpine age associated with Keuper material in the Iberian Mountains, near Teruel (Spain). Estudios Geológicos, 40(1-2), 23–32. https://doi.org/10.3989/egeol.84401-2645
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