【摘要】 碳酸盐岩洞穴化与洞石堆积是同一个系统相反的两种表象。其机理很简单，即系统序参量活度积。但过程复杂，受制于造洞环境的多样性与多变性。形态的同步异相集、世代叠加集，具分形特征。动力的多样性与涨落对全球变化响应而具混沌有序。洞石堆积的非线性特征，为认识和研究洞穴开拓了一个新的方向。更多还原

【Abstract】 Karst cavitation and speleothem deposit are two contrary phenomena in a cave system. The mechanism is very simple, that is,activity product of order parameters of a system. And the process is complicated, and is controlled by the variousness and changability of cave development environment. The synchronogenic heteropic set of morphometric features, and the generation superposition set have fracture characteristics. There is chaos order between the variousness and fluctuation of dynamics and their response to global changes. The non linear characteristics of speleothem deposit open up a path for understanding and studying caves.更多还原