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:鄂霍茨克海位于西太平洋边缘海最北部 .受欧亚大陆板块和太平洋板块的作用 ,有十分复杂的地质地球物理特征 .鄂霍茨克海不仅有海隆 ,还有三个著名的盆地 .其中的千岛盆地 ,是研究鄂霍茨克海的一个窗口 .本文通过对大量相关资料的二次开发 ,详细地讨论了鄂霍茨克海的地球物理场特征、沉积特点、热流分布及深部结构特点 ,并对该边缘海的形成演化进行了初步的探讨 .我们认为 ,对鄂霍茨克海研究的结果 ,将对中国边缘海地质特征的研究起到帮助和借鉴作用
: The Sea of Okhotsk is located in the northernmost part of the western Pacific margin.It has very complicated geological and geophysical characteristics under the action of the Eurasia plate and the Pacific plate.The Sea of Okhotsk not only has seamounts but also has three famous basins, The Qiandao Basin is a window for studying the Sea of Okhotsk.This paper discusses in detail the geophysical field characteristics, sedimentary characteristics, heat flow distribution and deep structure characteristics of the Okhotsk Sea through the secondary development of a large amount of relevant data. The formation and evolution of the marginal sea have been discussed tentatively.We think that the study of the Okhotsk Sea will help and study the geological characteristics of the marginal sea in China