Еarth断层参考网格及其在河床方向和形态上的反映

Q4 Earth and Planetary Sciences

Geology and Mineral Resources of Siberia Pub Date : 2022-10-01 DOI:10.20403/2078-0575-2022-3-92-98

P. P. Nagevich, E. V. Sergeeva, G. I. Karpizina

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引用次数: 0

摘要

本文提出了作者(2014)关于地球行星断层参考网格的假设，该假设也反映了区域和地方层面的析取位错位置。45亿年以来，它一直决定着地球的整个地质生命。网格由次纬向断层(nw193°- se113°;西南246°-北纬66°);和潜水(东经169°-西北349°;西南191°-东北11°)方向。断层格网的主要方向反映在全球主要河床的位置和形态上，通过对地球各大洲河流平面图像的分析证实了这一点。通过河床的构造解码和追踪断层，研究人员可以追踪它们在河间空间的位置，并假设评估在这些断层带内发现矿床的可能性。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

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REFERENCE GRID OF ЕARTH FAULTS AND ITS REFLECTION IN THE DIRECTION AND CONFIGURATION OF RIVERBEDS

The article presents the author’s hypothesis (2014) about the reference grid of planetary faults of Earth, which also reflect the position of disjunctive dislocations at regional and local levels. It has been determining the entire geological life of Earth for 4.5 billion years of its existence. The grid is represented by faults of sublatitudinal (NW 193° – SE 113°; SW 246° – NE 66°); and submeridional (SE 169° – NW 349°; SW 191° – NE 11°) orientation. Main directions of the fault grid are reflected in the position and configuration of the main riverbeds of the globe, that is confirmed by the analysis of river planimetric images in various continents of Earth. Decoding and tracing faults by the configuration of riverbeds allows researchers to trace their position in interfluvial spaces and hypothetically assess the possibility of finding ore deposits confined to the zones of these faults.

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来源期刊

Geology and Mineral Resources of Siberia Earth and Planetary Sciences-Geology

CiteScore

0.30

自引率

0.00%

发文量