Rotation Nature of Tectogenesis of Continental Margins and Breakdown of the Laurasian and Gondwanan Supercontinents

V. P. Utkin

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Rotation Nature of Tectogenesis of Continental Margins and Breakdown of the Laurasian and Gondwanan Supercontinents

机译：大陆边缘构造发生的旋转性质与劳拉斯和冈瓦南超大陆的破裂

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Numerous fundamental works, published mainly prior to the domination of the plate tectonics paradigm in science, are devoted to the role of Earth's rotation in planetary tectonics. The problem of shearing levels of continentals existed in the rotation model of the continental drift suggested by A. Wegener. Based on the analysis of voluminous materials, first of all, seismotomography, Pushcharovsky [9] elaborated a new model of the mantle structure with its tectonically isolated geospheres. According to Peive, slippage of the geospheres relative to each other is governed by rotation factors. We believe that this model eliminates the problem of shearing levels of continental mass and allows us to solve global tectonogeodynamic problems by developing the continental drift theory suggested by A. Wegener.

机译：许多基本著作，主要是在板块构造范式在科学领域中占主导地位之前出版，致力于地球自转在行星构造中的作用。 A. Wegener提出的大陆漂移旋转模型中存在大陆剪切水平的问题。在对大量物质进行分析的基础上，首先，进行地震层析成像，Pushcharovsky [9]构造了一个地幔结构的新模型，该模型具有构造上孤立的地球。根据Peive的说法，地球相对于彼此的滑动是由旋转因子控制的。我们认为，该模型消除了大陆质量剪切水平的问题，并通过发展A. Wegener提出的大陆漂移理论，使我们能够解决全球构造动力学问题。

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《Doklady Earth Sciences》 |2007年第7期|p.1000-1003|共4页
作者
V. P. Utkin;
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Far East Geological Institute, Far East Division, Russian Academy of Sciences, pr. Stoletiya Vladivostoka 159, Vladivostok, 690022 Russia;

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正文语种 eng
中图分类天文学、地球科学;
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Rotation Nature of Tectogenesis of Continental Margins and Breakdown of the Laurasian and Gondwanan Supercontinents

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