Citation: Ta. Little et al., Ductile fabrics in the zone of active oblique convergence near the Alpine Fault, New Zealand: identifying the neotectonic overprint, J STRUC GEO, 24(1), 2002, pp. 193-217
Citation: Ta. Little et al., Kinematics of oblique collision and ramping inferred from microstructures and strain in middle crustal rocks, central Southern Alps, New Zealand, J STRUC GEO, 24(1), 2002, pp. 219-239
Citation: Rj. Holcombe et Ta. Little, A sensitive vorticity gauge using rotated porphyroblasts, and its application to rocks adjacent to the Alpine Fault, New Zealand, J STRUC GEO, 23(6-7), 2001, pp. 979-989
Citation: Ta. Little et N. Mortimer, Rotation of ductile fabrics across the Alpine Fault and Cenozoic bending of the New Zealand orocline, J GEOL SOC, 158, 2001, pp. 745-756
Authors:
Benson, AM
Little, TA
Van Dissen, RJ
Hill, N
Townsend, DB
Citation: Am. Benson et al., Late Quaternary paleoseismic history and surface rupture characteristics of the eastern Awatere strike-slip fault, New Zealand, GEOL S AM B, 113(8), 2001, pp. 1079-1091
Citation: Ta. Little et al., An episodic Cretaceous cooling model for the Otago-Marlborough Schist, NewZealand, based on Ar-40/Ar-39 white mica ages, NZ J GEOL, 42(3), 1999, pp. 305-325
Citation: Db. Townsend et Ta. Little, Pliocene-Quaternary deformation and mechanisms of near-surface strain close to the eastern tip of the Clarence Fault, northeast Marlborough, New Zealand, NZ J GEOL, 41(4), 1998, pp. 401-417