| Tao Chunhui,Jin Xianglong,Lu Wenzheng,Hua Zugen.The application of the fractal geometry in the study of sea-floor volcano[J].Acta Oceanologica Sinica,1997,(3):387-394 |
| The application of the fractal geometry in the study of sea-floor volcano |
| The application of the fractal geometry in the study of sea-floor volcano |
| 投稿时间：1995-10-04 修订日期：1997-01-25 |
| DOI： |
| 中文关键词: Fractal fractal dimension sea floor volcano contour |
| 英文关键词:Fractal fractal dimension sea floor volcano contour |
| 基金项目: |
| 作者 | 单位 | | Tao Chunhui | Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China | | Jin Xianglong | Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China | | Lu Wenzheng | Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China | | Hua Zugen | Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China |
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| 中文摘要: |
| A fractal dimension measurement was made to the contours of the sea floor volcano of the South China Sea in this paper. It was found that the contours of the volcano end there are have stable fractal dimensions in its vicinity. The topography of the volcano end its vicinity can be divided into three parts by using fractal dimension:the mouth of the volcano, the steep waist part of the volcano end the plane sea floor near the volcano. Their fractal dimensions are about 1.12 which are lower than those of the lend. This points out that the basalt volcano has scale inflexibility even it is not very old, and it will have a fractal dimension with little difference after received some marine deposit. |
| 英文摘要: |
| A fractal dimension measurement was made to the contours of the sea floor volcano of the South China Sea in this paper. It was found that the contours of the volcano end there are have stable fractal dimensions in its vicinity. The topography of the volcano end its vicinity can be divided into three parts by using fractal dimension:the mouth of the volcano, the steep waist part of the volcano end the plane sea floor near the volcano. Their fractal dimensions are about 1.12 which are lower than those of the lend. This points out that the basalt volcano has scale inflexibility even it is not very old, and it will have a fractal dimension with little difference after received some marine deposit. |
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