Palaeomagnetism and KAr age of Mesozoic and Cenozoic igneous rocks from Antarctica

• Main Authors: Valencio, D.A., Mendía, JosE., Vilas, J.F.
• Format: Journal/Newspaper
• Language: unknown
• Subjects: Cape Spring; Deception Island; King George Island; oroclinal bending; polar movementigneous rocks; Antarc*; Antarctic; Antarctic Peninsula; Antarctica
• Online Access: https://hdl.handle.net/20.500.12110/paper_0012821X_v45_n1_p61_Valencio

A new analysis of palaeomagnetic data for igneous rocks from Deception Island, 25 de Mayo Island (King George Island) and Cape Spring, are given. K-Ar age determinations indicate that most of the igneous samples from 25 de Mayo Island included in the palaeomagnetic study are of Late Mesozoic/Early Tertiary age. The significance of these palaeomagnetic-radiometric data on the hypothesis of oroclinal bending of the Antarctic Peninsula and on the apparent polar movement of Antarctica is discussed. The positions of palaeomagnetic poles for the Andean igneous complex indicate that there has not been any apparent post-Late Cretaceous/Early Tertiary oroclinal bending in the Antarctic Peninsula from 74°S to 62°S. A comparison of the positions of palaeomagnetic poles for Antarctica and Australia suggests that the direction of apparent polar movement relative to Antarctica reversed after the Miocene. © 1979. Fil:Valencio, D.A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Mendía, JosE. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Vilas, J.F. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.