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| 东海陆架浙-闽沿岸泥质沉积研究进展 | |
| 引用本文： | 徐方建,李安春,黄敬利.东海陆架浙-闽沿岸泥质沉积研究进展[J].海洋通报,2012,31(1):97-104. |
| 作者姓名： | 徐方建 李安春 黄敬利 |
| 作者单位： | 1. 中国石油大学(华东)地球科学与技术学院,山东青岛266555;中国科学院海洋研究所,海洋地质与环境重点实验室,山东青岛266071;山东省油藏地质重点实验室,山东东营257061 2. 中国科学院海洋研究所,海洋地质与环境重点实验室,山东青岛266071 3. 中国海洋石油南海东部石油管理局,广东深圳,518067 |
| 基金项目： | 国家自然科学基金(41106040)，山东省自然科学基金(ZR2010DL009)，中央高校基本科研业务费专项资金(10CX04004A)。 |
| 摘 要： | 比较全面的回顾了关于东海浙-闽沿岸泥质体以及其形成前的沉积演化历史、泥质沉积的物质来源及其东亚季风/古气候记录等方面的研究进展。分析了目前关于浙-闽沿岸沉积研究中所存在的问题,即,泥质体的物质来源与形成,长江入海历史的陆架沉积物记录,8.2 ka冷事件,年代框架调整及区域对比,代用指标指示意义等多方面问题。提出在东海浙-闽沿岸泥质区,我们需要更多高分辨率的钻孔进行综合研究,其中应该特别加强对泥质沉积物的研究,以期对海陆交界敏感地带的"源到汇"以及全球变化研究取得突破性进展。 |
| 关 键 词： | 物源 泥质沉积物 东亚季风 东海 陆架 末次冰消期 |
| 收稿时间： | 2011/7/11 0:00:00 |
| 修稿时间： | 2011/9/14 0:00:00 |
Research progress in the mud deposits along the Zhe-Min coast of the East China Sea continental shelf |
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| XU Fangjian,LI Anchun and HUANG Jing-li.Research progress in the mud deposits along the Zhe-Min coast of the East China Sea continental shelf[J].Marine Science Bulletin,2012,31(1):97-104. | |
| Authors: | XU Fangjian LI Anchun and HUANG Jing-li |
| Institution: | 1. School of Geosciences, China University of Petroleum, Qingdao 266555, China; 2. Key Lab. of Marine Geology and Environment, Institute of Oceanology, CAS, Qingdao 266071, China; 3. Shandong Key Lab. of Reservoir Geology, China University of Petroleum, D;Key Lab. of Marine Geology and Environment, Institute of Oceanology, CAS, Qingdao 266071, China;CNOOC Nanhai East Petroleum Bureau, Shenzhen 518067, China |
| Abstract: | This paper provides a brief review on the development of researches in the fields of the Zhe-Min mud deposits of the East China Sea.Progress in the sedimentary evolution history before this mud deposits,and information of provenance and East Asian monsoon evolution are summarized.The deficiency that exists in the present research is analyzed,namely,the provenance and formation of the mud deposits,historical mud records of the Yangtze River entering sea,8.2 ka event,the age model readjustment and regional comparison,implication of the various proxies and so on.This paper concludes that more core sediments with higher resolution are needed for the future studies.More attention should be paid on the research of mud deposits,in order to obtain breakthrough in "source to sink" and global change in the sensitive land-sea interacting zone. |
| Keywords: | provenance mud sediment East Asian monsoon East China Sea continental shelf last deglaciation |
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