缘东海运动
又称缘东海变动(PeriTunghai disturbance)。小滕文次郎(1916)命名。新生代期间东中国海域周边的地壳变动。古近纪形成自朝鲜半岛东海岸太白山变位线(disloeation lines of the ThaiPaik San range)经日本九州西侧及琉球弧外侧至中国台湾省呈弧形构造线，并有古近纪及新近纪的沉积。上新—更新世时，断裂、褶皱运动极为剧烈，太平洋一侧的断层于琉球弧前构成深海，内侧则自琉球以至樱岛形成火山山脉。
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contributed at 2011-10-12
Classification(s)
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Earth System(in Chinese) Tectonic movement
Detailed Description
| English |
|---|
| Name | PeriTunghai tectonic movement |
| Chinese |
|---|
| Name | 缘东海运动 |
| Description | 又称缘东海变动(PeriTunghai disturbance)。小滕文次郎(1916)命名。新生代期间东中国海域周边的地壳变动。古近纪形成自朝鲜半岛东海岸太白山变位线(disloeation lines of the ThaiPaik San range)经日本九州西侧及琉球弧外侧至中国台湾省呈弧形构造线，并有古近纪及新近纪的沉积。上新—更新世时，断裂、褶皱运动极为剧烈，太平洋一侧的断层于琉球弧前构成深海，内侧则自琉球以至樱岛形成火山山脉。 |
How to Cite
NNU_Group (2011). 缘东海运动, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/51475cd9-f357-4071-8ed0-523742be09f3
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