Geometry Of Strike-slip Faults Research Articles

Enhanced interpretation of strike-slip faults using hybrid attributes: Advanced insights into fault geometry and relationship with hydrocarbon accumulation in Jurassic formations of the Junggar Basin

Strike-slip faults can play an important role in hydrocarbon accumulation. Therefore advanced studies on the interpretation of intra-basinal strike-slip faults are crucial. Hybrid attributes computed from conditioned 3D seismic data via artificial neural networks may enhance subsurface fault images. Jurassic formations within the C36 3D Prospect located in the Central Depression of the Junggar Basin are important to hydrocarbon accumulation. However, the geometry of strike-slip faults and their relationship with hydrocarbon accumulation are inadequately understood. The present study highlights these strike-slip faults using 3D seismic data from the C36 3D Prospect. Several conditioning approaches have enabled enhanced imaging of the strike-slip faults using computed hybrid attributes. They are based on implementing a dip-steering cube extracted from the original seismic data, along with analyses of multiple seismic attributes and a supervised neural network. Analysis of the hybrid attributes reveals the development of isolated, soft-linked, hard-linked, and coalesced faults along an approximately NE-SW trend. Various types of interactions were observed between the upper and lower fault systems. The different types of vertical linkages between the strike-slip faults provide hydrocarbon migration paths and thus, contribute differently to hydrocarbon migration. • Improved strike-slip fault imaging features from 3D seismic data using hybrid attributes are presented. • The geometry of strike-slip faults is analyzed according to hybrid attributes in the Jurassic formations. • The isolated, soft-linked, hard-linked, and coalesced fault tracesare illustrated, and a simple model is established. • The fault linkage types control the position and number of layers favorable for hydrocarbon accumulation.

Strain Partitioning Controlled by Oblique Ramp in Intracratonic Chains in Tunisia: Example of Gafsa Basin

The aim of this contribution is the interpretation of intracratonic chains in African plates, but it is important to verify some parameters such us the oblique convergence between Africaand Europa plates. Particularly In southern central of atlassic Tunisian belts, the slickenside examination of directional preexisting faults of N120 direction shows the coexistence of thrusting and strike-slip faults striation. In the limits of these faults principally in some tectonics lens we distinguish abnormal contacts with Triassic facies. The kinematic evolution of Gafsa basin resumed in the geometry of strike-slip faults connected in the thrusting system, this movement resulted from the oblique convergence on Ben Younes, Bou Ramli and Attig chains during compressive phases. This deformation style requires a shortening axis oblique to the NW-SE accidents (N120). The strain partitioning model verify the geometry of faults and equivalent evolution of folds and confirms the Triassic decollement level but without integrated of basement structures in the deformation. It permeated a passive transport of deformation observed in cover structure.