Inicio > Ciencias de la tierra, geografía, medioambiente, planificación > Ciencias de la tierra/geociencias > Geología y la litosfera > Evolução tectónico-diapirica da região de Fej Lahdoum-Dougga
Evolução tectónico-diapirica da região de Fej Lahdoum-Dougga

Evolução tectónico-diapirica da região de Fej Lahdoum-Dougga

Ahmed Kaabouri

72,33 €
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Editorial:
KS OmniScriptum Publishing
Año de edición:
2026
Materia
Geología y la litosfera
ISBN:
9786630079395
72,33 €
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Na região de Fej Lahdoum Norte-Dougga (zona dos diapiros, norte da Tunísia), surgem estruturas cuja evolução geodinâmica é caracterizada por uma halocinese. Estas estruturas, iniciadas por uma tectónica em blocos, continuam a desenvolver-se durante o Cretáceo e o início do Terciário. Durante as fases tectónicas do Mioceno e do Quaternário, estas estruturas assumem a sua morfologia atual. O estudo geológico desta região permitiu-nos evidenciar o papel da tectónica na evolução geodinâmica e estrutural, tendo simultaneamente em conta a evolução dos corpos triássicos ao longo do intervalo do Cretáceo até ao presente.

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