Abstract: Interaction of Folding, Sedimentation, and Erosion in Three Dimensions: A Study of the Sant Llorenc de Morunys Fault Propagation Fold, Southeast Pyrenees Using gOcad: Initial Results

AAPG Bulletin ◽  
2000 ◽  
Vol 84 ◽  
Author(s):  
FORD, MARY, Ecole Nationale Superie
AAPG Bulletin ◽  
2012 ◽  
Vol 96 (1) ◽  
pp. 109-132 ◽  
Author(s):  
J. P. Brandenburg ◽  
Faruk Omer Alpak ◽  
John G. Solum ◽  
Steve J. Naruk

AAPG Bulletin ◽  
2016 ◽  
Vol 100 (10) ◽  
pp. 1523-1540 ◽  
Author(s):  
Luisa F. Zuluaga ◽  
Atle Rotevatn ◽  
Eirik Keilegavlen ◽  
Haakon Fossen

1997 ◽  
Vol 503 ◽  
Author(s):  
E. N. Nagy ◽  
E. N. Landis

ABSTRACTA high resolution three-dimensional scanning technique called x-ray microtomography was applied to measure internal damage and crack growth in small mortar cylinders loaded in compression. Tomographic scans were made at different load increments in the same specimen. Three-dimensional image analysis was used to measure internal crack growth during each load increment. Load-deformation curves were used to measure the work of the external load on the specimen. Non-recoverable work of load was related to measured crack growth to estimate work of fracture in three dimensions. Initial results indicate a roughly linear relationship between work of load and internal crack area.


2000 ◽  
Vol 171 (4) ◽  
pp. 441-449 ◽  
Author(s):  
Sylvain Grelaud ◽  
Diego Buil ◽  
Stuart Hardy ◽  
Dominique Frizon de Lamotte

Abstract The Oupia anticline is a fault-propagation fold located at the northeastern tip of the Pyrenees. We show that this structure is suitably modelled using the trishear kinematic model rather than the self-similar kink-band model. In particular, the trishear model accounts well for the change in forelimb dip along strike as well as for sequential overall thickening and then thinning of the forelimb deduced from microtectonic analysis.


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