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菲律宾海板块(图1)是与俯冲过程有关的一些板块构造模式的资料来源。此板块的不同部份被用作为包括俯冲并始、洋内俯冲带发育、弧裂谷作用、弧后扩张和孤前拉张等构造过程的实例。已进行了两期大洋钻探。目的是了解其演化[深海钻井计划(DSDP)/大洋钻探计划)(ODP)的航次58、59、60、125、126。尽管这样,对板块的第三纪运动还了解甚少。推断运动史的主要障碍是菲律宾海板块自它被俯冲带包围后而独立于全球板块变化过程。由于这个原因,它的成因和运动史成为人们争论的根源,曾提出(Uyeda等, 1972)此板块是在太平洋板块于约45Ma时沿老太平洋洋底内的转换断层俯冲时形成的,并在西菲律宾盆地内圈捕了先前的扩张中心,这个观点在解释此板块史时继续在被引证。
The Philippine Sea Plate (Figure 1) is a source for some plate tectonics related to subduction processes. Different parts of this plate are used as examples of tectonic processes, including subduction and beginning, subduction zone development, arc rifting, backarc extension and solitary stretch. Two rounds of ocean drilling have been conducted. The purpose is to understand the voyage 58,59,60,125,126 of its evolution [Deep Ocean Drilling Program (DSDP) / Ocean Drilling Program] (ODP). Despite this, little is known about the Tertiary Movement in the plate. The main obstacle to infer the history of exercise is that the Philippine Sea plate is independent of the global plate change since it was subducted by the subduction zone. For this reason, its genesis and history have been the source of controversy. It has been proposed (Uyeda et al., 1972) that this plate was formed during the transitional subduction of the Pacific plate in the old Pacific Ocean at about 45 Ma, The inner circle of the West Philippine Basin caught the previous center of expansion, a view that continues to be cited in the interpretation of this plate history.