Extraterrestrial factors and their role in the Earth's tectonic evolution in the Early Precambrian

被引:8
作者
Glukhovskii, M. Z. [1 ]
Kuz'min, M. I. [2 ]
机构
[1] Russian Acad Sci, Inst Geol, Moscow 119017, Russia
[2] Russian Acad Sci, AP Vinogradov Inst Geochem, Siberian Branch, Irkutsk 664033, Russia
基金
俄罗斯基础研究基金会;
关键词
early Earth; lunar-terrestrial interaction; impact events; tectonic evolution; LU-HF; PLATE-TECTONICS; MANTLE PLUMES; SOUTH-AFRICA; CONTINENTAL LITHOSPHERE; CRUSTAL EVOLUTION; WESTERN-AUSTRALIA; ARCHEAN GRANITES; DETRITAL ZIRCONS; GNEISS COMPLEX;
D O I
10.1016/j.rgg.2015.06.001
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The paper is focused on the fundamental problem of influence of extraterrestrial factors on the Earth's geologic and tectonic evolution. Extraterrestrial factors played a decisive role in the Earth's genesis, the formation of the first Hadean continental crust, and the beginning of the Archean era. Their significant influence persisted in the later epochs: Even in the Phanerozoic, extraterrestrial factors might have had a considerable influence on the environment. The sialic cores of protocontinental crust (4.4-3.9 Ga) with first-generation greenstone zones (3.8-3.2 Ga) and the global system of granite-greenstone belts (3.1-2.7 Ga) formed in the rotation-plume regime, mainly in the subequatorial hot belt. The formation of these global structures was, to a large extent, influenced by asteroid impacts, which caused the impact-triggered genesis of mantle plumes. Dramatic changes in the subsequent geologic history began at 2.7-2.0 Ga; at 2.0 Ga they terminated with the Moon's transition to an orbit similar to the present-day one (50 +/- 3 Earth's radii), accompanied by the abrupt slowdown of the Earth's axial rotation, the termination of formation of the layer D '', and the start of recent plate tectonics, which is accompanied by the plume tectonics. (C) 2015, V.S. Sobolev IGM, Siberian Branch of the RAS. Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:959 / 977
页数:19
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