| CLAY MINERALS IN THE CHINA SEA AND ADJACENT SEAS |
| |
| 引用本文： | 何良彪. CLAY MINERALS IN THE CHINA SEA AND ADJACENT SEAS[J]. 中国科学B辑(英文版), 1989, 0(9) |
| |
| 作者姓名： | 何良彪 |
| |
| 作者单位： | Institute of |
| |
| 摘 要： | The clay minerals in the surface sediments from 354 stations have been analyzed qualita-tively and semiquantitatively. The obtained data are dealt mathematically. According to thecalculated results, the distribution laws and the trends of content changes of clay mineralsare discussed. The studied area is divided into four main provinces of sediments with differ-ent sources. Finally the author approached the laws of the migration and dispersal of thefine-grained matter carried into the seas by the Huanghe River, the Changjiang River, theZhujiang River and the Philippine Archipelagoes, and set up the transport model of the fine-grained matter in the China Sea and adjacent seas.
|
CLAY MINERALS IN THE CHINA SEA AND ADJACENT SEAS |
| |
| HE LIANG-BIAO First Institute of Oceanography,State Oceanic Administration. Qingdao. CLAY MINERALS IN THE CHINA SEA AND ADJACENT SEAS[J]. Science in China(Chemistry), 1989, 0(9) |
| |
| Authors: | HE LIANG-BIAO First Institute of Oceanography State Oceanic Administration. Qingdao |
| |
| Abstract: | The clay minerals in the surface sediments from 354 stations have been analyzed qualita-tively and semiquantitatively. The obtained data are dealt mathematically. According to thecalculated results, the distribution laws and the trends of content changes of clay mineralsare discussed. The studied area is divided into four main provinces of sediments with differ-ent sources. Finally the author approached the laws of the migration and dispersal of thefine-grained matter carried into the seas by the Huanghe River, the Changjiang River, theZhujiang River and the Philippine Archipelagoes, and set up the transport model of the fine-grained matter in the China Sea and adjacent seas. |
| |
| Keywords: | the China Sea clay minerals trend surface provenauce model of migration and dispersal |
| 本文献已被 CNKI 等数据库收录！ |
