--> Synthetic Transfer Zone Characterization Using Seismic Data, Taranaki Basin, New Zealand
[First Hit]

AAPG ACE 2018

Datapages, Inc.Print this page

Synthetic Transfer Zone Characterization Using Previous HitSeismicNext Hit Data, Taranaki Basin, New Zealand

Abstract

Synthetic transfer zones develop Previous HitbetweenNext Hit fault segments which dip in the same direction, with relay ramps connecting the fault blocks associated with the different fault segments. The characteristics of the transfer zones are controlled by the Previous HitlithologyNext Hit, deformation conditions, and strain magnitude. The Parihaka fault is a NE-SW trending set of three echelon faults connected by relay ramps in the Taranaki Basin, New Zealand. The structure in the basin is defined by extension during two episodes of deformation Previous HitbetweenNext Hit the late Cretaceous and Paleocene and Previous HitbetweenNext Hit the Late Miocene and Recent. To better understand the evolution of a synthetic transfer zone, we study the geometry and secondary faulting Previous HitbetweenNext Hit the individual fault segments in the Parihaka fault system using 3D Previous HitseismicNext Hit data, and Previous HitseismicNext Hit attributes.

A 3D Previous HitseismicNext Hit interpretation was conducted to interpret the major faults and surfaces. Unlike standard models of synthetic transfer zones, the Parihaka fault zone is characterized by extensional fault-propagation (drape) folding, which modifies the geometry of the transfer zone. Previous HitSeismicNext Hit attributes, including coherence and maximum and minimum curvature were used to understand the detailed geometry and variation in displacement on the individual faults, the nature of secondary faulting along the transfer zones, and the Previous HitrelationNext Hit Previous HitbetweenNext Hit the faults and the drape folds. Because the degree of faulting varies with the stage of development of the transfer zone, Previous HitseismicNext Hit characterization of the fault system was conducted for three separate horizons Previous HitbetweenTop the Miocene and Pliocene. Coherence and curvature analysis reveal the variation in geometry of the fault system for the different horizons, and the increasing maturity of the transfer zone with depth. Both attributes enhance the visualization of the major and associated secondary faults. The results are also compared to experimental models of transfer zones with associated drape folding.