摘要
借助于对南黄海表层沉积物中微体化石的分析，探讨了不同的微体化石数量及组合的分布特点、沉积特征、微体化石浮游有孔虫、钙质超微化石与黑潮、黄海暖流、黄海冷水团、黄海沿岸流之间的关系。同时根据本区的粒度分析资料，把表层沉积物划归为下列类型。南黄海中、西部：1粘土沉积，2．粉研质粘土沉积，3．细砂与粉砂沉积，4砂砾等混杂沉积；东侧：从北至南依次排列为砂、泥质沙、抄质泥和泥质沉积。此外，对南黄海表层沉积物的物源归纳为以下几种：1．黄河源，2．长江源，3．陆架残留砂源，4．（韩国）锦江、汉江等源，5．风尘源。
The area of the Yellow Sea is about 417 thousands square kilometres and is divided into north and South two parts according to the boundary line between the Chengshantou of Shandong Province and the Bailing Islands of Korea. Of which the North Yellow Sea is about 100 thousands square kilometres. The South Yellow Sea is three times as much as the North Yellow Sea. China began to study the sediments of the Yellow Sea from the 1950s and have got much scientific achievement. After 1970s, Institute of Oceanology, the Chinese Academy of Sciences. the Tong ji University, First Institute of Oceanography, state oceanic Administration had investigated and studied the surface and core samples from the Yellow Sea in varying degrees early or late.After the late 1980s, the previous Institute of Marine Geology, Ministry of Geology and Mineral Resources had made a study of the sequence of bedding and the stratigraphic correlation in the Quaternary,Above-mentioned study laid a foundation for the study of the South Yellow Sea.In this paper, the numbers of different microfossils and the distribution character of associations. the sedimentary character'the relationship' among the micro fossils planktonic foraminifera, calcareous nanoplank fossils and Black Stream.the warm current of the Yellow Sea the cold water mass'the coastal current of the Yellow Sea have been studied by means of the analysis of microfossils in the surface sediments from the South Yellow Sea. At same time, according to the data of size, the types of the surface sediments have been divided as follows: in the middle-west areas of the South Yellow Sea, 1. clay 2. silt clay 3. fine-sand and silt 4. sandgravel and mixtum,and in the east area, the sediments are arranged for inturn sand'mud sand,sand mud and mud from the north to the south. In addition,the material resource in the surface sedilnents fronl the South Yellow Sea might be summed up following: 1. the material ources of the Yellow River 2. the material sources of the Changjiang 3. the material sources of the remnant salld 4. the material sources of the Hanjiang and jinjiang etc. (Korean). 5. the material sources of eolian depos.
出处
《沉积学报》
CAS
CSCD
北大核心
1999年第A12期775-781,共7页
Acta Sedimentologica Sinica
基金
国家科技部基础研究项目
中韩科技合作项目
国家海洋局青年基金!97401
