1引言响应于南中国海板块俯冲产生的台湾-吕宋弧，在弧的南端和北端与欧亚板块相碰。因此，火山作用在碰撞带附近停止或降低到低程度（图1）。沿弧喷出的岩浆地化的有规律时间和空间的变化被认为与俯冲的来自大陆的沉积物或靠近碰撞带的地壳碎片的卷入有关。然而，这些加入的成 1 Introduction In response to the Taiwan-Luzon arc resulting from the subduction of the South China Sea plate, it collides with the Eurasian plate at the southern and northern ends of the arc. As a result, volcanism ceases or decreases to a low level near the collision zone (Figure 1). Changes in regular time and space of magmatic geology along the arc are thought to be related to subduction of sediments from the continent or crustal debris near the collision zone. However, these added into