利用航天测量资料研究地球内部结构的方法学基础

O. Azimov
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引用次数: 0

摘要

从现象学的角度,从概念上描述了利用远程航空航天技术研究地壳结构的方法的主要基础。关键(第一)原则关注的是相反方向的物理力同时相互作用(共生)的过程知识。这就是吸引力,与之相对的是斥力。第二个原则仅限于确定岩石圈结构出现和演化的两组地质驱动力(内部和外部)。遥感应用于地质目的的第三个原则是基于岩石塑性(准塑性)变形和脆性(准脆性)变形同时存在的概念。第四个原理声称,在地球的自然地球系统中,存在着永久中断的能量-质量交换的积极过程,这是物质存在及其运动形式的特殊方面的表现。第五个原理指出,特定的近期景观及其固有的异常,作为地质基底内部结构和与其相关的能量-质量交换过程的地质指标,可以通过不同波区的反射、吸收和发射电磁辐射的光谱特征来区分。因此,可以利用这些特征来区分它们,并可通过遥感数据对它们进行成像和识别。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
BASIC FOUNDATIONS OF THE METHODOLOGY OF STUDY OF THE INTERNAL STRUCTURE OF EARTH ACCORDING TO AEROSPACE SURVEY DATA
main foundations that are the basis of the methodology of investigation of the Earth crust structure using remote aerospace technologies are characterised conceptually from the phenomenological perspective. The keystone (first) principle con-cerns the knowledge of process for the simultaneous mutual interaction (paragenesis) of the physical forces oppositely direct-ed. These are the attractive power and the opposite of it the repulsive forces. The second principle is confined to determine of two groups for the geological driving forces (internal and external) for the appearance and evolution of the lithosphere structure. The third principle of remote sensing application for the geological purposes is based on the concept of existence both the plas-tic (quasiplastic) rock deformations and brittle (quasibrittle) ones. The fourth principle claims the existence of active processes for the permanent-interrupted energy-mass-exchange in the natural geosystems of the Planet as a manifestation of the special aspects for matter being and its forms of movements. The fifth principle states that the specific recent landscapes and the anomalies intrinsic to them as the geoindicators of interior structure of the geological substrate and energy-mass exchange processes connected with it are differentiated by the spectral features of reflected, absorbed, and emitted electromagnetic radi-ation in the different wave regions. As a result they are distinguished using these characteristics and may be imaged and iden-tified via remote sensing data.
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