The Mount S. Giovanni caves developed mostly during Paleozoic and Mesozoic in Cambrian limestones (Gonnesa formation) locally mineralized. Their infilling, of economic interest, took place during or nearly after the volcanic Cenozoic phase. The material derives from the removal of important pedogenetic cover, with episodes of clays masses redeposition and phases of wall collapses and of concretioning. -from Authors
Paleokarstic fills in Iglesiente (Sardinia Italy) sedimentary processes and age / A. Bini, M. Cremaschi, P. Forti, J. Perna. - In: ANNALES DE LA SOCIÉTÉ GÉOLOGIQUE DE BELGIQUE. - ISSN 0037-9395. - 10:1(1988), pp. 123-177. ((Intervento presentato al convegno Colloque international de sédimentologie karstique tenutosi a Liege nel 1988.
Paleokarstic fills in Iglesiente (Sardinia Italy) sedimentary processes and age
A. BiniPrimo
;M. CremaschiSecondo
;
1988
Abstract
The Mount S. Giovanni caves developed mostly during Paleozoic and Mesozoic in Cambrian limestones (Gonnesa formation) locally mineralized. Their infilling, of economic interest, took place during or nearly after the volcanic Cenozoic phase. The material derives from the removal of important pedogenetic cover, with episodes of clays masses redeposition and phases of wall collapses and of concretioning. -from Authors
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