北吕宋岛菲律宾活动带蛇绿岩及其上覆浊积岩的放射虫研究新进展(英文)

摘要

The basement of the Philippine Mobile Belt (PMB) is mainly composed of ophiolites that are mostly overlain by Paleogene to Miocene turbidites in central Luzon.To clarify the geological development of the PMB with respect to the initial stage of the arc volcanism(eg.Yumul et al.,2003,2008;