| 海底峡谷成因新探 |
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| 引用本文： | 周家乐.海底峡谷成因新探[J].海洋湖沼通报,1991(4):53-56. |
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| 作者姓名： | 周家乐 |
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| 作者单位： | 东方图书公司 |
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| 摘 要： | 海底峡谷,是由于地壳板块运动而形成的一种地质构造。板块不同形式的运动,造成了不同特征的海底峡谷。河流和浊流等因素对地层岩石的冲刷作用,只能改变海底峡谷的外貌,却不是海底峡谷的成因。
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| 关 键 词： | 海底 峡谷 成因 |
ON THE GENESIS OF SUBMARINE CANYON |
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| Zhou Jiale.ON THE GENESIS OF SUBMARINE CANYON[J].Transaction of Oceanology and Limnology,1991(4):53-56. |
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| Authors: | Zhou Jiale |
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| Abstract: | Submarine canyon is a geological structure that formed by plate movement in the crust. As a result of differ movement type of plate, submarine canyon of different features formed washing effect of rivers and turbidity on stratum rocks' could only change the appearance of submarine canyon, but could not change the genesis of submarine canyon. |
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| Keywords: | submarine canyon formation |
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