Hydrothermal massive dolomitization in the Cantabrian Zone (NW Spain): a Permo-Triassic event promoted by extensional tectonic?

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Titel in ÜbersetzungHydrothermal massive dolomitization in the Cantabrian Zone (NW Spain): a Permo-Triassic event promoted by extensional tectonic?
OriginalspracheEnglisch
TitelDeformation history, fluid flow reconstruction and reservoir appraisal in foreland fold and thrust
Seiten18-23
StatusVeröffentlicht - 2002