Inicio > Ciencias de la tierra, geografía, medioambiente, planificación > Ciencias de la tierra/geociencias > Geología y la litosfera > Evoluzione tettonico-diapirica della regione di Fej Lahdoum-Dougga
Evoluzione tettonico-diapirica della regione di Fej Lahdoum-Dougga

Evoluzione tettonico-diapirica della regione di Fej Lahdoum-Dougga

Ahmed Kaabouri

72,27 €
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Editorial:
KS OmniScriptum Publishing
Año de edición:
2026
Materia
Geología y la litosfera
ISBN:
9786630045512
72,27 €
IVA incluido
Disponible
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Nella regione di Fej Lahdoum Nord-Dougga (zona dei diapiri, Tunisia settentrionale) hanno origine strutture la cui evoluzione geodinamica è caratterizzata da un’alocinesi. Queste strutture, originate da una tettonica a blocchi, proseguono durante il Cretaceo e l’inizio del Terziario. Durante le fasi tettoniche del Miocene e del Quaternario, queste strutture assumono la loro morfologia attuale. Lo studio geologico di questa regione ci ha permesso di evidenziare il ruolo della tettonica nell’evoluzione geodinamica e strutturale, tenendo conto al contempo dell’evoluzione dei corpi triassici nel corso dell’intervallo dal Cretaceo ad oggi.

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