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本文提出了岩浆侵入作用的热动力模式,根据有时蒸气形成于岩浆房内部的事实讨论了火山喷发作用的机制。蒸气从正在上升的富含挥发份的岩浆束中解析出来,该岩浆束的上升引起体积增大、岩浆房的增压作用和可能的喷发作用,该模式推导出了一个控制岩浆增压作用动力学过程的微分方程展开式,发现通过这种机制可以产生非常高的内部压力,恰巧还没有其他任何确证的机制也能产生强烈的喷发作用。
This paper presents a thermodynamic model of magmatic intrusion that discusses the mechanism of volcanic eruption based on the fact that steam sometimes forms inside the magma chamber. Vapor is resolved from an ascending evaporite-rich magma bundle, which increases volume, magma chamber pressurization and possible eruptions. This model derives a kinetic that controls magma pressurization The evolution of the differential equations of the learning process reveals that very high internal pressures can be generated by this mechanism, and that no other confirmatory mechanism happens to produce a strong eruption as well.