| 南海北部表层沉积物中黏土和碎屑矿物组成及其地质意义 |
| |
| 引用本文： | 高水土,张德玉,陈荣华,赵庆英. 南海北部表层沉积物中黏土和碎屑矿物组成及其地质意义[J]. 海洋学报, 2008, 30(1): 86-92 |
| |
| 作者姓名： | 高水土 张德玉 陈荣华 赵庆英 |
| |
| 作者单位： | 国家海洋局,第二海洋研究所,浙江,杭州,310012;国家海洋局,第二海洋研究所,国家海洋局,海底科学重点实验室,浙江,杭州,310012;国家海洋局,第一海洋研究所,山东,青岛,266061 |
| |
| 基金项目： | 国家自然科学基金 , 国家专项基金 |
| |
| 摘 要： | 以X-射线衍射仪和偏光显微镜为主要手段,对南海调查区表层底质沉积物中黏土和碎屑矿物组分进行分析和研究,结果表明黏土矿物主要有伊利石、蒙皂石、高岭石和绿泥石,其组合特征在不同区域表现出明显的差异。碎屑成分主要由生物壳(钙质和硅质)、轻矿物(石英、长石为主)和含量低但种类多的重矿物组成。一般认为物质来源是调查区沿岸风化岩石遭受进一步剥蚀后细小组分通过水动力搬运沉积而成的。钙质和硅质生物壳分布受南海碳酸盐补偿深度(CCD)的控制。
|
| 关 键 词： | 表层沉积物 黏土和碎屑矿物 南海北部 |
| 文章编号： | 0253-4193(2008)01-0086-07 |
| 收稿时间： | 2006-04-28 |
| 修稿时间： | 2006-04-28 |
Composition of clay and detrital minerals in surface sediment of the northern South China Sea and geological significance |
| |
| GAO Shui-tu,ZHANG De-yu,CHEN Rong-hua and ZHAO Qing-ying. Composition of clay and detrital minerals in surface sediment of the northern South China Sea and geological significance[J]. Acta Oceanologica Sinica (in Chinese), 2008, 30(1): 86-92 |
| |
| Authors: | GAO Shui-tu ZHANG De-yu CHEN Rong-hua ZHAO Qing-ying |
| |
| Affiliation: | 1.Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China;Key Laboratory of Submarine Geosciences of State Oceanic Administration, Second Institute of Oceanogranhy, State Oceanic Administration, Hangzhou 310012, China2.First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China |
| |
| Abstract: | The compositions of clay and detrital minerals in the surface sediment of the northern South China Sea are studied based on the analyses of X-ray diffraction and micro scope observations.It is found that clay minerals consist mainly of illite, smectite, kaolinite and chlorite.Distribution characeteristics of the clay and detrital minerals are apparently different in the western and eastern areas.Detrital compositions are mainly microf ossils (calcareous and siliceous), light minerals (quartz and feldspar), and many kinds of heavy minerals with low contents.The research result shows that the detrital materials are derived from the fine eroded debris in the coastal areas by the sea current.The distributions of calcareous and siliceous micro fossils are apparently controlled by the carbonate dissolution. |
| |
| Keywords: | surface sediment clay and detrital minerals northern South China Sea |
| 本文献已被 维普 万方数据 等数据库收录！ |
| 点击此处可从《海洋学报》浏览原始摘要信息 |
|
点击此处可从《海洋学报》下载全文 |
|
