在中生代，苏鲁元古褶皱带受造山作用的影响活化，导致许多花岗岩体的侵入，使交代岩广泛发育。
In Mesozoic, the Proterozoic Sulu fold belt has undergone orogenic activization resulting in the intrusion of numerous granite bodies with broad development of metasomatic rocks.
并指出区域极低级变质作用是成岩-埋藏变质作用(造山前)和同造山变质作用的综合结果。
Regional very low grade metamorphism resulted from the combination of early diagenesis burial metamorphism (pre orogeny) and late syn orogeny metamorphism.
其余各岩体是本区造山后与大陆抬升作用以及大陆裂谷作用有关的花岗岩类。
The other intrusive bodies are post-orogenic granitoid in association with the continental uplifting and rifting.
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