一个岩浆系统似乎可以被想象成由断裂、脉及细脉构成的一个复杂网络,其大小大至补给脉小到粒间薄膜。就象血管系统一样,我想将一个岩浆通道系统的几何形状描述成破裂状而不是欧几里得形状或许要好得多。 Spera曾指出,岩浆上升存在着热的证据。除非岩浆上升的速度很快或者补给脉很大,否则,一旦上升的岩浆把热传递给冷的岩石圈,那么就会导致其自身发生“热死亡”并因此而凝固。当岩浆开始向地表运动时,最小的脉会快速凝固并同时释放出流体。如果这 A magmatic system seems to be conceived of as a complex network of faults, veins and veins that are as large in size as the donor veins to the intergranular membrane. Like the vasculature, I think it might be much better to describe the geometry of a magma channel system as a rupture rather than a Euclidean shape. Spera once pointed out that there is evidence of heat in the rise of magma. Unless the magma rises very fast or the recharge pulse is large, once the rising magma transfers heat to the cold lithosphere, it “cools itself” and solidifies as a result. As the magma begins to move to the surface, the smallest veins rapidly solidify and release fluid at the same time. If this