Génesis de Nódulos de Cuarzo en el Paleozoico de la Ibérica (Rama Aragonesa)
DOI:
https://doi.org/10.3989/egeol.87433-4586Keywords:
Iberian Mountains, Paleozoic Nodules, Diagenesis, SilicaAbstract
A particular feature in the paleozoic materials from Iberian Mountains (Spain) is the presence of diagenetic silica-nodules. The nodules, from microscopic to mesoscopic size and almost always constituted by a mosaic association of neoformed quartz-crystals, appear to have been originated in relation with tectonic processes. Three steps are differenciated, from early one, defined by a microcrystalline structure, to the nowadays one, formed ocasionally by quartz monocrystals.
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Published
1987-08-30
How to Cite
Navas, A., & Tena, J. (1987). Génesis de Nódulos de Cuarzo en el Paleozoico de la Ibérica (Rama Aragonesa). Estudios Geológicos, 43(3-4), 179–184. https://doi.org/10.3989/egeol.87433-4586
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