| XIE QINCHUN,YE YINOAN,LU BINGWEN.TOPOGRAPHY AND SEDIMENTATION OF THE EAST CHINA SEA SHELFBREAK[J].Acta Oceanologica Sinica,1985,(2):276-288 |
| TOPOGRAPHY AND SEDIMENTATION OF THE EAST CHINA SEA SHELFBREAK |
| TOPOGRAPHY AND SEDIMENTATION OF THE EAST CHINA SEA SHELFBREAK |
| 投稿时间：1984-01-20 修订日期：1984-07-10 |
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| 中文关键词: |
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| 中文摘要: |
| The shelfbreak of the East China Sea lies in an area with a marked change in gradient between the continental shelf and the slope (west wall of Okinawa Trough), depth ranging from 132 to 162 m with an average of about 147 m, and the width ranging from 4 to 18 km.The types of the shelfbreak differ markedly from the north to the south, having an abrupt break in the south and a gradual break in the middle and the north.Without permanent deposition of fine-grained material formed at the shelfbreak zone, it serves only as a temporary resting place for terrigenous sediments moving toward the Okinawa Trough through submarine canyons as important transport conduits. |
| 英文摘要: |
| The shelfbreak of the East China Sea lies in an area with a marked change in gradient between the continental shelf and the slope (west wall of Okinawa Trough), depth ranging from 132 to 162 m with an average of about 147 m, and the width ranging from 4 to 18 km.The types of the shelfbreak differ markedly from the north to the south, having an abrupt break in the south and a gradual break in the middle and the north.Without permanent deposition of fine-grained material formed at the shelfbreak zone, it serves only as a temporary resting place for terrigenous sediments moving toward the Okinawa Trough through submarine canyons as important transport conduits. |
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