“…There is some indication that the Oligocene magnetic lineations may extend northward beyond the eastern limit of the South of 3.5°N, the Caroline-Pacific Plate boundary, while still compressional, apparently changes from overthrusting of the Caroline Plate to underthrusting of the plate along the Mussau Trench, This trench is generally considered to be the site of incipient subduction (Bracey and Andrews, 1974;Bracey, 1975;Kogan, 1976;Weissel and Anderson, 1978). Bracey and Andrews (1974) felt that the former Pacific-Philippine plate boundary, marked by the Yap-Palau-Ayu Trough may now be extinct, or may be in the process of becoming inactive.…”