Rosa María Martínez González, Marceliano Lago San José, José Ignacio Valenzuela Ríos, Ramon Vaquer Navarro, Ramón Salas Roig
Jurassic volcanic rocks are well exposed in the Sierra de Javalambre (Teruel). This multiepisodic volcanism is mainly volcaniclastic, showing a large variety of fragmentation and emplacement mechanisms, and it is intercalated between carbonatic rocks spanning from Pliensbachian through Bajocian. The mineral and chemical composition indicates a volcanism with alkaline affinity and little magmatic differentiation. From a geotectonic point of view, this volcanism corresponds to a late-volcanism within the postrift thermal subsidence (lower and middle jurassic) that took place during the mesozoic development of the Jberian Basin (lberian Chains).
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