内土尾淤积区沉积物为凝聚成小球的粘土及黑云母，它来自九龙江悬沙与海岸工程抛入的泥沙。
The sediments of Nei-Tu-Wei siltation regions are spheroidal coagulant clay and biotite. which are formed by suspended silt of the Jiulon…
内土尾淤积区沉积物为凝聚成小球的粘土及黑云母，它来自九龙江悬沙与海岸工程抛入的泥沙。
The sediments of Nei-Tu-Wei siltation regions are spheroidal coagulant clay and biotite. which are formed by suspended silt of the Jiulon…
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