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朝鲜南海内陆架晚第四纪沉积演化Ｓ．ＣｈｕｌＰａｒｋ等朝鲜南海大陆架为一巨厚的陆源碎屑沉积物堆积的地区．其中心陆架在深海和底部特征的基础上可被分为窄的内陆架和宽的中部陆架，内陆架区（深＜５ｓｍ）是晚第四纪沉积的沉积中心，沉积物主要来自部分河流．大量来自...
Late Quaternary sedimentary evolution of the South China Sea continental shelf. ChulPark and other South China Sea shelf for a huge accumulation of terrigenous clastic sediments. Its central shelf can be divided into a narrow inland shelf and a wide central shelf on the basis of deep-sea and bottom features. The inner shelf area (depth <5sm) is the depositional center of late Quaternary sediments mainly from part river. A lot of from ...