北黄海西部的全新世泥质沉积

王桂芝; 高抒; 李凤业

北黄海西部的全新世泥质沉积

1.
中国科学院, 海洋研究所, 山东, 青岛, 266071
2.
南京大学, 海岸与海岛开发教育部重点实验室, 江苏, 南京, 210093

基金项目: 国家自然科学基金(49876018)

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出版历程
- 收稿日期: 2001-09-19
- 修回日期: 2002-07-05

Holocene mud deposits in the west of the northern Huanghai Sea

1.
Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
2.
Ministry of Education Key Laboratory for Coast and Island Development, Nanjing University, Nanjing 210093, China

摘要

摘要: 细颗粒沉积物在海洋动力条件下被侵蚀、搬运、堆积过程及其对自然环境的影响是国际地圈生物圈计划(IGBP)关注的内容之一,陆架区细颗粒沉积物的输运、堆积、再悬浮过程与物质循环有着紧密的关系^[1]。泥质沉积中记录了环境变迁的信息,通过对现代环境下的细颗粒沉积的研究,可以了解沉积物的形成环境及堆积过程,有助于恢复古代的沉积历史和沉积环境。
- 泥质沉积 /
- 粒度 /
- 浅地层剖面 /
- 沉积速率 /
- 北黄海
- mud deposit /
- grain size data /
- shallow seismic profiles /
- deposition rate /
- northern Huanghai Sea

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参考文献(20)

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