摘要
Early Cretaceous plutonic rocks at Creswick Peaks in NW Palmer Land, Antarctic Peninsula show evidence of synmagmatic crustal extension and deformation during emplacement and cooling at 141 ± 2 Ma. Deformation textures, ranging from sub-magmatic phenocryst alignment to ultramylonite, are preserved in granodiorite. Large volumes of gabbro were intruded late in the kinematic history. Crustal extension compensated by magma emplacement has occurred, and a close correspondence of ages between the shear zone, granodiorite and gabbro suggests a rapid phase of crustal growth. Extensional structures are partially overprinted by mid-Cretaceous thrusting and compression.