'Special Points' of Oceanic Volcanism:Typical Features of the Structure and Evolution of the Bottom Topography

E.V.Zhuleva

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'Special Points' of Oceanic Volcanism:Typical Features of the Structure and Evolution of the Bottom Topography

机译：海洋火山作用的“特殊点”：底部地形结构和演化的典型特征

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A geomorphological study of oceanic "special points"-areas of anomalously active recent volcanism confined to massifs of intraplate volcanic structures-is performed.The distribution of special points over the ocean floor is assessed,and the depths of magmatic chambers and general characteriscs of the volcanites formed are given.The location of spoecial points on major intraplate volcanic structures is analyzed.The spatial and temmporal succession of the topography evolution along the extension of volcanic chains is revealed.The Principal factors of the evolution of volcanic mounds are the suberation conditions of their formation and the gradual isostatic subsidence of the ocean floor.

机译：进行了海洋“特殊点”的地貌研究-异常活跃的近期火山活动仅限于板内火山结构的断层。评估了特殊点在海床上的分布，以及岩浆室的深度和一般特征给出了形成的火山岩，分析了板内主要火山构造上的闪点的位置，揭示了沿火山链延伸的地貌演化的空间和时间顺序。它们的形成和海床的逐渐等静陷。

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《Oceanology》 |2003年第5期|共5页
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E.V.Zhuleva;
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正文语种 eng
中图分类海洋学;
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'Special Points' of Oceanic Volcanism:Typical Features of the Structure and Evolution of the Bottom Topography

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