The surface sediment grade of the bar becoming finer gradually along the bar westwards. It can continue to exist under the action of the long period common wave...
由于该水下沿岸沙坝是因台风浪破碎形成的，故它能够在台风浪过后长期的常风浪作用下继续存在。
The surface sediment grade of the bar becoming finer gradually along the bar westwards. It can continue to exist under the action of the long period common wave...
由于该水下沿岸沙坝是因台风浪破碎形成的，故它能够在台风浪过后长期的常风浪作用下继续存在。
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