Taihangshan orogen, called tectonomagmatic belt by most of geologists, is thought to be a part of Mesozoic circum Pacific magmaticarc.
太行山造山带被大多数学者称为构造岩浆带，被认为是中生代环太平洋岩浆弧的组成部分。
2
There is a typical example for arc-arc collision between the Yidun island arc andShalulishan magmaticarc, or even throughout eastern Tethys.
典型的义敦岛弧与沙鲁里山岩浆弧之间的弧-弧碰撞模式及其外延到整个东特提斯构造域内都是很普遍的。
3
The magma of melted detaching and sinking crystal completely mixes with that of the melted crust in the magmatic chamber of crust, which forms the Palaeogene syncollision and volcanic arc magma.