大洋钻探与中国边缘海沉积地质学  

OCEAN DRILLING AND SEDIMENTARY GEOLOGY OF CHINA MARGINAL SEAS

作　　者：石学法[1] 

机构地区：[1]中国科学院海洋研究所,青岛266071

出　　处：《海洋科学》1996年第3期47-50,共4页Marine Sciences

摘　　要：边缘海沉积地质学研究在大洋钻探计划中占据着重要地位，也是我国的优势所在，应该成为我国ＯＤＰ近期工作的主要内容。本文讨论了与ＯＤＰ有关的几个中国边缘海沉积地质学问题：古黑潮的演变与陆海相互作用，长江、黄河入海时间及其对海洋沉积作用的影响，冲绳海槽的沉积相和沉积体系，古季风与海平面变化，这些问题的深入研究与解决将会为实现ＯＤＰ的学术目标、为全球变化研究做出重要贡献。The sedimentary geology of marginal seas occupies an important position in the Ocean Drilling Program (ODP), it is a superior field of our country and thus should become the major parts of our recent ODP researches. This paper discusses several problems of sedimentary geology of marginal seas related with ODP as follows: The evolution of palaeocurrent and the interplay of sea and land ;the time that the Yangtze River and the Yellow River flowed into sea and its effect on marine sedimentary processes; the sedimentary facies and the sedimentary system of the Okinawa Trough; the palaeomonsoon and sealevel changes. The deep research and resolution of these problems will make great contributions to the realization of ODP objects and the study of global changes.

关 键 词：大洋钻探 边缘海 沉积地质学 全球变化 

分 类 号：P756.5[天文地球—海洋科学] P736.2