Analysis of Hydrothermal Activity in the Oceanic Ridges

它是对山脊下热区水热过程动力学的理论研究。设计了一个自然系统的理论模拟，以便于分析过程之间的相互作用，这些过程通过上覆岩石中的渗流网络重新分配来自洋壳底部附近的深成岩浆体的能量和质量。这项研究的目的是预测由输送过程中的局部反馈引起的活动温泉下地下场强参数的长期和短期变化的大小和周期。这项研究将主要集中在与流体临界区近场重合的状态下的热液活动行为。

Theis is a theoretical study of the dynamics of hydrothermal processes beneath ridge.crest thermal areas. A theoretical analog of the natural system has been designed to facilitate analyses of the interaction among processes that redistribute energy and mass from the pluton sized magma bodies near the bottom of the ocean crust through percolation networks in the overlying rocks. The objective of the study is to predict the magnitude and periodicity of long and short term variations of field parameters in the subsurface beneath active hot springs that are caused by local feedbacks amongst the transport processes. The study will focus primarily on the behavior of hydrothermal activity at state conditions that coincide with the near field of the critical region of the fluid.