The present-day knowledge of the outcropping rocks indicates that they deformed under conditions of diagenesis, with a peak reaching very low grade metamorphism. This raises the question of how rocks can flow at temperatures below 150-200 ºC, and stimulates the discussion of very low temperature deformation assisted by fluids. Therefore the field trip aims at discussing modelling of structures as diverse as folds (multi and single layer), cleavage, faults, boudins and veining under very low temperature and assisted by fluids. Ultimately we will discuss how far modelling is from reality.
An article published this year in Tectonics will serve as field guide. Download here
For further information, please e-mail F.O. Marques at fomarques@fc.ul.pt |