Thrust Fault and Sub-Thrust Imaging in the Taranaki Basin With Least-Squares Tilted Orthorhombic Q-RTM
Thrust Fault and Sub-Thrust Imaging in the Taranaki Basin With Least-Squares Tilted Orthorhombic Q-RTM
The Taranaki Basin is one of New Zealand’s largest basins. Initially forming as a Cretaceous rift basin, it has over 400 exploration and production wells. Early basin history is characterized by extensional fault blocks, and as basin evolution continued, thrusting and inversion associated with ...