水-岩系统的最佳协合作用(英文)

现已证明 ,水岩系统能满足最佳协合作用的主要要求 ,而该作用乃是关于有机成因和无机成因在内的自组织系统科学。自组织的主要前提是其非平衡态平衡态的性质 ,从地质学上说此性质是在确定着漫长的而严格地定向性发展过程中的 ,并伴有越来越多的新矿物相的、以及新地球化学类型的水的形成。这种水结构方面的新变化可以加以利用来评价和传递有关的信息。自组织的这些特性 ,使得水岩系统就成为了在地壳内部的许多地质作用与现象发展过程中的一个基本系统。

THE WATER-ROCK SYSTEM SYNERGY

It is shown that a water-rock system satisfies principal demandsof synergy, the science of self-organization of systems in organic and inorganic nature. The main premise of self-organization is its nonequilibrium-equilibrium character, determining geologically long and strictly directional development with formation of increasingly new mineral phases and geochemical types of water. The new changes of water structures can be used to evaluate and pass information. Properties of self-organization make the water-rock system a basic one in the development of many geological processes and phenomena within the Earth’s crust.