Practical analysis of strike-slip faults using multi attributes 3D seismic data: A case study in Eastern Colombia

2014 ◽  
Author(s):  
Antonio Pico* ◽  
Jesús Aboud ◽  
Felipe Parraga ◽  
Jose Antonio Martinez ◽  
Gonzalo Lopez
2010 ◽  
Vol 61 (6) ◽  
pp. 483-493 ◽  
Author(s):  
Márton Palotai ◽  
László Csontos

Strike-slip reactivation of a Paleogene to Miocene fold and thrust belt along the central part of the Mid-Hungarian Shear ZoneRecently shot 3D seismic data allowed for a detailed interpretation, aimed at the tectonic evolution of the central part of the Mid-Hungarian Shear Zone (MHZ). The MHZ acted as a NW vergent fold and thrust belt in the Late Oligocene. The intensity of shortening increased westwards, causing clockwise rotation of the western regions, relatively to the mildly deformed eastern areas. Blind thrusting and related folding in the MHZ continued in the Early Miocene. Thrusting and gentle folding in the MHZ partly continued in the earliest Pannonian, and was followed by sinistral movements in the whole MHZ, with maximal displacement along the Tóalmás zone. Late Pannonian inversion activated thrusts and generated transpressional movements along the Tóalmás zone.


First Break ◽  
2018 ◽  
Vol 36 (12) ◽  
pp. 99-103
Author(s):  
Paolo Esestime ◽  
Milos Cvetkovic ◽  
Jonathan Rogers ◽  
Howard Nicholls ◽  
Karyna Rodriguez

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