The origination of the magma is related with the dehydration of the subducting plate of the Paleozoic Tethys Sea.
岩浆的起源与古生代特提斯海俯冲板块的脱水有关。
Then the next instance of subduction occurs years later, and the lip of the subducting plate pushes further, but what happens to the rumpling that occurred the first time?
下一个例子是几年后发生俯冲，该俯冲板块的顶端进一步推动，但第一次起皱时会发生什么情况？
The origination of the magma is related with the dehydration of the subducting plate of the Palezoic Tethy Sea and the early tension of the form of the Lancangjiang belt red layer basin.
火山岩岩浆的形成既与古特提斯洋的俯冲洋壳在深部脱水有关，又与南澜沧江带红层盆地形成初期的拉张作用有关，为山—盆转化阶段特殊岩浆类型。
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