
handle: 10261/199701
Las emanaciones hidrotermales, asociadas a las efusiones volcánicas, son frecuentemente una de las causas condicionantes de la existencia de sedimentación biosilícea marina, por lo que en el Mioceno Mediterráneo, con sus frecuentes interlaciones de rocas volcánicas, es fácil justificar esta sedimentación.
Proyecto subvencionado por CAICYT y CSIC.
Peer reviewed
Novelda, Alicante, Diatomitas, Diagénesis, Monforte del Cid
Novelda, Alicante, Diatomitas, Diagénesis, Monforte del Cid
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