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在漫长的地质发展历史中,福建经过多次剧烈的构造变动,每一次构造变动,留下的构造形迹,常组成典型的构造型式或形成有成生联系的构造体系,已经被认识的主要有:纬向构造,经向构造,多字型构造,山字型构造,棋盘格式构造,帚状构造,环状构造,弧形或S型构造等。本文试图从福建境内主要构造型式的组合,结合地质历史中与时间和空间上有紧密联系的沉积槽地、岩浆的喷出和充填方式以及展布型式等特征,对本区地壳运动的方式和方向进行探讨。
In the long history of geologic development, after many dramatic structural changes in Fujian, each tectonic change and the tectonic trace left behind often constitute typical structural types or form a structural system with an established relationship with each other. The main known : Zonal structure, meridional structure, multi-font structure, mountain font structure, checkerboard format structure, broom structure, ring structure, arc or S-shaped structure. This paper tries to analyze the mode and direction of the crustal movement in this area from the combination of the main structural types in Fujian Province, combining with the sedimentary troughs, the eruption and filling modes of magma and the distribution patterns of magmatism closely related with time and space in geologic history To explore.