冲绳海槽南部沉积层序的粒度特征

李军; 高抒; 孙有斌; 曾志刚

冲绳海槽南部沉积层序的粒度特征

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南京 210093;
3.
中国科学院研究生院北京 100039

基金项目: 国家重点基础研究规划项目(973)(编号G2000046702)；国家自然科学基金(批准号:40106006和40176020)；中国科学字知识创新工程项目(KZCX2-207)联合资助

详细信息

作者简介:
李军,男,1974年出生,博士研究生,海洋地质

中图分类号: P736.2

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文章访问数: 550
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Grain-size Variations of Terrigenous Sediment Sequences in the South Okinawa Trough

1.
Institute of Oceanology, Chinese Academy of Sciences, Qingdao Shandong 266071;
2.
Key Laboratory of Coast and Island Development, MOE, Nanjing University, Nanj ing 210093;
3.
Graduate School of Chinese Academy of Sciences, Beijing 100039

摘要

摘要: 对取自冲绳海槽南部的A2 3孔经前处理后的沉积物样品进行了粒度测试,探讨了陆源沉积层序的粒度特征。沉积物平均粒径、分选系数、偏态、峰态等粒度参数的变化显示出A2 3孔的沉积层序以 4 0 0cm为界可分为上、下两段,下段各参数稳定,代表了比较稳定的水动力条件的沉积环境;上段则波动较大,小规模浊流沉积频繁发育,暗示了不稳定的沉积环境。浊流层内粗粒与细粒组分含量及粒度分布的变化具有明显的规律性。通过分析A2 3孔陆源沉积层序的各沉积参数特征,认为冲绳海槽南部的沉积环境和动力在时间尺度上有较大的变化,东海陆架物质向南部海槽的输运可能是以峡谷为通道的重力作用引起的床底沉积作用为主。另外,对陆源碎屑和全样粒度结果的对比,显示了前处理方法对于海洋沉积物粒度分析的重要性.
- 冲绳海槽 /
- 陆源碎屑 /
- 粒度参数与分布 /
- 浊流沉积
Abstract: Terrigenous detritus samples extracted from a piston core A23, located in the so uthern Okinawa Trough, were analyzed in terms of the grain-size characteristics. The results show that the terrigenous sequences in the core can be divided int o two parts on the basis of the variations in the grain-size parameters. The l ower sequence is characterized by constant grain-size parameters; whilst the up per part is controlled by turbidite layers with a thickness of about 2～20 cm, which caused very large variations of the parameters. The large variation of gra in-size composition and distribution of the turbidite sequences significantly disturbed the normal formation of the sediment sequences. The gain-size distri bution modes and parameters of a turbidite bed were analyzed in detail, which sh ow very regular variation in the bed. According to all grain-size character istics of the core, the depositional environment and sediment dynamics is very c omplex and the main mechanism of the transportation of the terrigenous material from East China Sea Shelf to the trough is in the form of bedload through canyo ns. Furthermore, pretreatment to the marine sediments is important, which enable s us to compare the grain-size characteristics between terrigenous detritus and the bulk grain-size.
- terrigenous sequences /
- grain-size parameters and distribution /
- turbidite sediment /
- Okinawa Trough

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参考文献(27)

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冲绳海槽南部沉积层序的粒度特征

作者简介:
李军,男,1974年出生,博士研究生,海洋地质

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Grain-size Variations of Terrigenous Sediment Sequences in the South Okinawa Trough

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冲绳海槽南部沉积层序的粒度特征

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南京 210093;

3. 中国科学院研究生院北京 100039

作者简介:
李军,男,1974年出生,博士研究生,海洋地质

English Abstract

Grain-size Variations of Terrigenous Sediment Sequences in the South Okinawa Trough

1. Institute of Oceanology, Chinese Academy of Sciences, Qingdao Shandong 266071;

2. Key Laboratory of Coast and Island Development, MOE, Nanjing University, Nanj ing 210093;

3. Graduate School of Chinese Academy of Sciences, Beijing 100039

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[1]	李忠. “从最高到最深”—从第17届国际沉积学大会看沉积学研究前沿 . 沉积学报, 2006, (6): 928-933.
[2]	李忠. “从最高到最深”—从第17届国际沉积学大会看沉积学研究前沿 . 沉积学报, 2006, 24(06): 928-933.

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冲绳海槽南部沉积层序的粒度特征

作者简介: 李军,男,1974年出生,博士研究生,海洋地质

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Grain-size Variations of Terrigenous Sediment Sequences in the South Okinawa Trough

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冲绳海槽南部沉积层序的粒度特征

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 南京 210093; 3. 中国科学院研究生院 北京 100039

作者简介: 李军,男,1974年出生,博士研究生,海洋地质

English Abstract

Grain-size Variations of Terrigenous Sediment Sequences in the South Okinawa Trough

1. Institute of Oceanology, Chinese Academy of Sciences, Qingdao Shandong 266071; 2. Key Laboratory of Coast and Island Development, MOE, Nanjing University, Nanj ing 210093; 3. Graduate School of Chinese Academy of Sciences, Beijing 100039

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目录

友情链接

期刊在线

联系我们

作者简介:
李军,男,1974年出生,博士研究生,海洋地质

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南京 210093;

3. 中国科学院研究生院北京 100039

作者简介:
李军,男,1974年出生,博士研究生,海洋地质

1. Institute of Oceanology, Chinese Academy of Sciences, Qingdao Shandong 266071;

2. Key Laboratory of Coast and Island Development, MOE, Nanjing University, Nanj ing 210093;

3. Graduate School of Chinese Academy of Sciences, Beijing 100039