Hydrothermal massive dolomitization in the Cantabrian Zone (NW Spain): a Permian to Triassic event promoted by extensional tectonics?
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Translated title of the contribution | Hydrothermal massive dolomitization in the Cantabrian Zone (NW Spain): a Permian to Triassic event promoted by extensional tectonics? |
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Original language | English |
Title of host publication | Deformation history, fluid flow reconstruction and reservoir appraisal in foreland fold and thrust |
Pages | 1-5 |
Publication status | Published - 2002 |