1. Seismic Clatter•Discovery Procedure:•Observe each seismic map for patterns of geologicfeatures.•Shade in and describe the general patterns shown byeach map. Follow…
1. 3D facies modelling strategies in large fan-delta reservoirs and their implications in predictions. Data from Montserrat and Sant Llorenç del Munt outcropping analogues…
CHAPTER . . Strike-Slip Faults Strike-slip faults are generally vertical faults that ac- commodate horizontal shear within the crust. Their traces on the Earth's surface…
157 STRIKE-SLIP AND OBLIQUE-SLIP TECTONICS Strike–slip faulting is a common mode of deformation in both continental and oceanic crust and occurs at a wide range of scales.…
Experimental clay modeling is used to study the geometry andevolution of deformation zones formed above basement faults.The nature of deformation is compared for reverse…
157 STRIKE-SLIP AND OBLIQUE-SLIP TECTONICS Strike–slip faulting is a common mode of deformation in both continental and oceanic crust and occurs at a wide range of scales.…