Inicio > Ciencias de la tierra, geografía, medioambiente, planificación > Ciencias de la tierra/geociencias > Geología y la litosfera > Ewolucja tektoniczno-diapiryczna regionu Fej Lahdoum-Dougga
Ewolucja tektoniczno-diapiryczna regionu Fej Lahdoum-Dougga

Ewolucja tektoniczno-diapiryczna regionu Fej Lahdoum-Dougga

Ahmed Kaabouri

72,27 €
IVA incluido
Disponible
Editorial:
KS OmniScriptum Publishing
Año de edición:
2026
Materia
Geología y la litosfera
ISBN:
9786630238181
72,27 €
IVA incluido
Disponible
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W regionie Fej Lahdoum Północ-Dougga (obszar diapirów, północna Tunezja) powstają struktury, których ewolucja geodynamiczna charakteryzuje się halokinezą. Struktury te, zapoczątkowane przez tektonikę blokową, rozwijają się w okresie kredy i na początku trzeciorzędu. W fazach tektonicznych miocenu i czwartorzędu struktury te przybrały swój obecny kształt. Badania geologiczne tego regionu pozwoliły nam wykazać rolę tektoniki w ewolucji geodynamicznej i strukturalnej, z uwzględnieniem ewolucji ciał triasowych w okresie od kredy do współczesności.

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