协同学作为自组织的一般理论包括了一大类自然现象,而并不局限于热力学的情态。热力学结构和热混沌仅仅是存在极性的一种形式。在发生结构自组织之初,形成了许多涨落。当系统远离平衡时,长程关联的振幅最初很小,后来增大。结果是,从众多的涨落中涌现出一个涵盖整个系统的涨落。协同学的这个论点从一种完全不同的视角来描述无机世界。包括地质学物体在内的各类无机物体应该被看成是变异选择的突变和产物,这种变异选择是按照达尔文的逻辑规划来实现的。大自然往往,然而并非总是以分形的形式展示出来,后者可以划分为“正确的”和“不正确的”两种分形形式。结晶格子是正确分形的实例,其单位晶胞具有不同尺度的重复性。我们的行星则是不正确分形这一类自然分形。如果我们将“隶属”视为分划结构的一种规律,那么人们必须将大、小构形的岩石圈看作是一种分形结构。从逻辑上讲,整个地质学的现实应该代表无机物质协同自组织的分形产物。地球和Benard对流结构一样,是一种多阶段的对流系统;在前者之中一个水平上的对流启动了另各一个上覆水平上的对流。这个形成结构的对流的原理表现在大、小尺度上,比如,它构成了矿床形成中的流体化理论的基础,后者也包括协同学的其他理论。按照这一理论,沉积岩的沉降伴随有扩张的流体饱和带的形成。流体以沉积断面上部中的水-碳氢化合物组分及其下部中的水-碳酸盐与矿石组分为代表。在随深度而增高的温度影响下,流体被加热,并且建造内的压力异常增大,因而加热了的流体穿透到断面的较高水平。上升的流体是强有力的热载体,它们使上覆沉积岩经过显著的增补加热而产生对流机制,并且大大地加速了它们的后生转变。 Synergy as a general theory of self-organization includes a wide range of natural phenomena, not just thermodynamics. Thermodynamic structure and thermal chaos are just a form of polarity. In the beginning of the structure of self-organization, formed a lot of fluctuations. When the system is far from equilibrium, the amplitude of long-range correlation is initially small and then increases. The result is a wave of fluctuations that covers the entire system. The argument of synergetics describes the inorganic world from a completely different perspective. All kinds of inorganic objects, including geologic objects, should be regarded as mutations and products of variation selection, which is made according to Darwin’s logical programming. Often, however, nature is not always shown in fractal form, which can be divided into two fractal forms, “right” and “incorrect.” The crystal lattice is an example of a correct fractal, with unit cells having different scales of repeatability. Our planet is not the correct fractal this type of natural fractal. If we consider “affiliation ” as a regular pattern of subdivision structures, one must consider large and small shaped lithosphere as a fractal structure. Logically speaking, the reality of the entire geology should represent the fractal product of the synergistic self-organization of inorganic matter. The Earth, like the Benard convection structure, is a multi-stage convective system; in the former one horizontal convection initiates convection over another overlying level. The principle of convection, which forms the structure, manifests itself at large and small scales. For example, it forms the basis of fluidization theory in the formation of deposits, and the latter includes other theories of synergies. According to this theory, the sedimentation of sedimentary rocks is accompanied by the formation of an expanding fluid saturation zone. The fluid is represented by the water-hydrocarbon component in the upper portion of the sedimentary section and the water-carbonate and ore components in the lower portion thereof. Under the influence of increasing temperature with depth, the fluid is heated and the pressure inside the construction abnormally increases so that the heated fluid penetrates to a higher level of the cross-section. The ascending fluids are powerful heat carriers that create convective mechanisms by overtaking the overlying sedimentary rocks with significant heating and greatly accelerate their epigenetic transformation.