渤海东部与黄海北部表层沉积物的粒度特征及其沉积环境

张剑; 李日辉; 王中波; 张训华; 黄龙; 孙荣涛

doi:10.16562/j.cnki.0256-1492.2016.05.001

渤海东部与黄海北部表层沉积物的粒度特征及其沉积环境

1. 国土资源部油气资源和环境地质重点实验室, 中国地质调查局青岛海洋地质研究所, 青岛 266071;

2. 青岛海洋科学与技术国家实验室, 青岛 266071;

3. 山东理工大学资源与环境工程学院, 淄博 255000

基金项目:
国家自然科学基金项目(41206053)；中国地质调查局国土资源大调查项目(GZH200800501,GZH201400201,DD20160137)；“大陆架科学钻探”项目(GZH201100202)

详细信息

作者简介: 张剑(1981-),男,硕士,助理研究员,主要从事海洋地质、工程地质、海洋环境和沉积动力学研究,E-mail:yuzu79@sina.com

中图分类号: P736.21

收稿日期: 2016-04-28

修回日期: 2016-05-20

GRAIN SIZE CHARACTERISTICS OF SURFACE SEDIMENTS IN THE EAST BOHAI SEA AND THE NORTHERN YELLOW SEA AND THEIR IMPLICATIONS FOR ENVIRONMENTS

1. Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Ministry of Land and Resources, China Geological Survey Qingdao Institute of Marine Geology, Qingdao 266071, China;

2. Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao Institute of Marine Geologs, Qingdao 266071, China;

3. School of Resource and Environment Engineering, Shandong University of Technology, Zibo 255000, China

Received Date: 28 April 2016

Revised Date: 20 May 2016

摘要

摘要: 渤海东部和黄海北部表层沉积物粒度组成分析揭示,沉积物主要由砂、粉砂、粉砂质砂和砂质粉砂组成,部分海域出现含砾沉积物。总体分布表现为南细北粗、东西分带的特点,形成以平行岸线的条带状分布格局为主体的南北不同的镶嵌形态,由岸及海、由北向南呈现由粗到细的分布特征。沉积物分布主要受物质来源、地形以及海洋环流控制,根据沉积物成因划分出老铁山水道-辽东-渤中浅滩砂质沉积区、山东半岛沿岸流泥质沉积区、北黄海中部泥质沉积、南黄海中部泥质沉积区、西朝鲜湾潮流沙脊沉积区、渤海中部泥质沉积区,并讨论了不同沉积区的沉积环境。
- 表层沉积物 /
- 粒度 /
- 沉积环境 /
- 渤海 /
- 黄海
Abstract: Grain size analysis is a tool widely applied in sediment classification and environmental interpretation. There occur sand, silt, silty sand and sandy silt in the areas of eastern Bohai and northern Yellow seas, with a few gravelly sediments. The spatial distribution of sediments shows a W-E zonation of grain size, roughly parallel to the coast lines. They are coarser in northern area and finer along southern area in general, and become finer along the direction from the coast to the sea. The grain size distribution pattern depends upon the factors of provenance, seabed topography and ocean circulation. According to the seabed deposits, 6 depositional areas can be identified, including the areas of the Laotieshan Channel-Liaodong-Bozhong tidal sandy deposits, the Shandong Peninsula coastal muddy deposits, the Central North Yellow Sea muddy deposits, the Central South Yellow Sea muddy deposits, the West Korean Gulf tidal sand ridge deposits and the Central Bohai Sea muddy deposits. All of the sedimentary environments of the depositional areas are discussed in details in the paper.
- surface sediment /
- grain size /
- sedimentary environment /
- the Boshi Sea /
- the Yellow Sea

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渤海东部与黄海北部表层沉积物的粒度特征及其沉积环境

1. 国土资源部油气资源和环境地质重点实验室, 中国地质调查局青岛海洋地质研究所, 青岛 266071; 2. 青岛海洋科学与技术国家实验室, 青岛 266071; 3. 山东理工大学资源与环境工程学院, 淄博 255000

作者简介: 张剑(1981-),男,硕士,助理研究员,主要从事海洋地质、工程地质、海洋环境和沉积动力学研究,E-mail:yuzu79@sina.com

GRAIN SIZE CHARACTERISTICS OF SURFACE SEDIMENTS IN THE EAST BOHAI SEA AND THE NORTHERN YELLOW SEA AND THEIR IMPLICATIONS FOR ENVIRONMENTS

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1. 国土资源部油气资源和环境地质重点实验室, 中国地质调查局青岛海洋地质研究所, 青岛 266071;

2. 青岛海洋科学与技术国家实验室, 青岛 266071;

3. 山东理工大学资源与环境工程学院, 淄博 255000