| 不同层序岩相中的不稳定带和岩石的特征变化 |
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| 引用本文： | 尤里K.伯林. 不同层序岩相中的不稳定带和岩石的特征变化[J]. 沉积与特提斯地质, 1995, 15(2): 150-153. |
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| 作者姓名： | 尤里K.伯林 |
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| 作者单位： | 俄罗斯莫斯科罗蒙诺索夫大学地质系 |
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| 摘 要： | 盆地形成的原因包括:构造圈深部地带物质的不稳定状态、软流圈厚度的增加和继而地壳厚度的减小。大多数沉积盆地均有一些高能不稳定层,反映了岩石特征的非线性交换。
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THE INSTABLE ZONES IN DIFFERENT LITHOFACIES OF SEQUENCE AND PROPERTY CHANGES OF THE ROCKS |
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| Yu. K. Burlin. THE INSTABLE ZONES IN DIFFERENT LITHOFACIES OF SEQUENCE AND PROPERTY CHANGES OF THE ROCKS[J]. Sedimentary Geology and Tethyan Geology, 1995, 15(2): 150-153. |
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| Authors: | Yu. K. Burlin |
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| Affiliation: | Geological Department,Moscow Lomonosov University,V-234 Vorobjevy Cory,Moscow,119899,Russia |
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| Abstract: | The reasons of basin''s formation are:unsteady states of substance in deep zones of tectono-sphere,increasing of asthenosphere thickness and decreasing of the crust thickness consequent-ly. There are some levels of energetic instability in most of sedimentary basins. It reflects in nonlinear exchanging of properties of the rocks. |
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