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Abstract Growth strata and unconformities in the Cenozoic synorogenic sediments in the southern Cordillera Oriental of the northern Argentine Andes provide new evidence for the eastward migration of the Andean deformation from the Puna to the Santa Barbara system. The growth sequences and unconformities allow us to constrain the age of the structures
Núria Carrera, Josep Anton Muñoz
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Growth pattern of underlithified strata during thrust-related folding
Journal of Structural Geology, 2004Abstract Asymmetric anticlines with overturned or steeply dipping forelimbs and gently dipping backlimbs are generally interpreted as thrust-related folds. Fold asymmetry occurs as a consequence of forelimb rotation. If deformation takes place in environments dominated by submarine sedimentation, the limbs coincide with the slope (depositional ...
NIGRO, Fabrizio, RENDA P
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