Titlebook: ;

粗魯性質(zhì)

https://doi.org/10.1007/978-3-642-51334-3r zones were responsible for the migration, drainage and tapping of magmas from the source region. The inclined attitude of the shear zones would have acted as a roof-guide for the up-rising magmas. Finally, the transcurrent movement most likely enhanced the upward migration of magmas.