南黄海表层沉积物中微体化石的沉积特点及物源分析

程振波; 石学法; 陈志华; 鞠小华

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南黄海表层沉积物中微体化石的沉积特点及物源分析

程振波, 石学法, 陈志华, 鞠小华

文章导航 > 沉积学报 > 1999 > 17(S1): 775-781

程振波, 石学法, 陈志华, 鞠小华. 南黄海表层沉积物中微体化石的沉积特点及物源分析[J]. 沉积学报, 1999, 17(S1): 775-781.

引用本文:

程振波, 石学法, 陈志华, 鞠小华. 南黄海表层沉积物中微体化石的沉积特点及物源分析[J]. 沉积学报, 1999, 17(S1): 775-781.

CHENG Zhen-bo, SHI Xue-fa, CHEN Zhi-hua, Ju Xiaohua. The Analysis of the Sedimentary Character of the Microfossils and the Material Resource in the Surface Sediments from the South Yellow Sea[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 775-781.

Citation:

CHENG Zhen-bo, SHI Xue-fa, CHEN Zhi-hua, Ju Xiaohua. The Analysis of the Sedimentary Character of the Microfossils and the Material Resource in the Surface Sediments from the South Yellow Sea[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 775-781.

程振波, 石学法, 陈志华, 鞠小华. 南黄海表层沉积物中微体化石的沉积特点及物源分析[J]. 沉积学报, 1999, 17(S1): 775-781.

引用本文:

程振波, 石学法, 陈志华, 鞠小华. 南黄海表层沉积物中微体化石的沉积特点及物源分析[J]. 沉积学报, 1999, 17(S1): 775-781.

Citation:

CHENG Zhen-bo, SHI Xue-fa, CHEN Zhi-hua, Ju Xiaohua. The Analysis of the Sedimentary Character of the Microfossils and the Material Resource in the Surface Sediments from the South Yellow Sea[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 775-781.

南黄海表层沉积物中微体化石的沉积特点及物源分析

国家海洋局第一海洋研究所,青岛 266003

基金项目: 国家科技部基础研究项目;中韩科技合作项目;国家海洋局青年基金(97401)

详细信息

作者简介:
程振波，男，1956年出生，副研究员，海洋地质及微体古生物。

中图分类号: P736.21;Q913.6

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文章访问数: 358
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The Analysis of the Sedimentary Character of the Microfossils and the Material Resource in the Surface Sediments from the South Yellow Sea

First Institute of Oceanography,SOA. Qingdao Shandong China 266003

摘要

摘要: 借助于对南黄海表层沉积物中微体化石的分析，探讨了不同的微体化石数量及组合的分布特点、沉积特征、微体化石浮游有孔虫、钙质超微化石与黑潮、黄海暖流、黄海冷水团、黄海沿岸流之间的关系。同时根据本区的粒度分析资料，把表层沉积物划归为下列类型。南黄海中、西部：1粘土沉积，2．粉研质粘土沉积，3．细砂与粉砂沉积，4砂砾等混杂沉积；东侧：从北至南依次排列为砂、泥质沙、抄质泥和泥质沉积。此外，对南黄海表层沉积物的物源归纳为以下几种：1．黄河源，2．长江源，3．陆架残留砂源，4．（韩国）锦江、汉江等源，5．风尘源。
- 微体化石 /
- 沉积特点 /
- 类型 /
- 物源
Abstract: The area of the Yellow Sea is about 417 thousands square kilometres and is divided into north and South two parts according to the boundary line between the Chengshantou of Shandong Province and the Bailing Islands of Korea. Of which the North Yellow Sea is about 100 thousands square kilometres. The South Yellow Sea is three times as much as the North Yellow Sea. China began to study the sediments of the Yellow Sea from the 1950s and have got much scientific achievement. After 1970s,Institute of Oceanology,the Chinese Academy of Sciences the Tongji University First Institute of Oceanography,state Oceanic Administration had investigated and studied the surface and core samples from the Yellow Sea in varying degrees early or late. After the late 1980s,the previous Institute of Marine Geology,Ministry of Geology and Mineral Resources had made a study of the sequence of bedding and the stratigraphic correlation in the Quaternary.Above-mentioned study laid a foundation for the study of the South Yellow Sea. In this paper,the numbers of different microfossils and the distribution character of associations the sedimentary character the relationship among the microfossils planktonic foraminifera、calcareous nanoplank-fossils and Black Stream、the warm current of the Yellow Sea、the cold water mass、the coastal current of the Yellow Sea have been studied by means of the analysis of microfossils in the surface sediments from the South Yellow Sea. At same time,according to the data of size,the types of the surface sediments have been divided as follows:in the middle-west areas of the South Yellow Sea,1. clay 2. silt clay 3. fine-sand and silt 4. sand-gravel and mixtum,and in the east area,the sediments are arranged for inturn sand 、mud sand、sand mud and mud from the north to the south. In addition,the material resource in the surface sediments from the South Yellow Sea might be summed up following:1. the material cources of the Yellow River 2. the material sources of the Changjiang 3. the material sources of the remnant sand 4. the material sources of the Hanjiang and ]in- jiang etc. (Korean). 5. the material sources of eolian depos.
- microfossils /
- sedimentary character /
- type /
- material sources

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参考文献(1)

[1]

1 刘敏厚，吴世迎，王永吉.黄海晚第四纪沉积[M].北京:海洋出版社，1987

2 金风均Bong Kyum Kim, et al. Foraminifera in the bottom sedimenu off the South-eastern coast of Korea[J]. Technical Bulletin CCOP. 1970, 3 (1) :147-163

3 郑执中，郑守仪.黄海和东海浮游有孔虫生态的研究[J].海洋与湖沼,1962,4(1-2):60-85，图版I

4 汪品先.海洋微体古生物论文集[M].北京:海洋出版社，1980. 60-83

5 李文勤.黄渤海表层沉积物中钙质超微化石分布规律与黄海暖流流路[J].黄渤海海洋，1991,9(1):7-11

6 郑光膺.黄海第四纪地质[M].北京:科学出版社，1991

7 Cheng Zhenbo, Fu Mingzuo, Ju Xiaohua. The geological significance of fossils in the coastal loess in the Bohai Straits and Liaodong Peninsula[J].Acta Oceanologica Sinica,1997,16(1): 71-83

8 Milliman J D,Meade R H. World-wide delivery of river sediments to the oceans[J]. 1. Geol.,1993,91:1一21.

9 Wang Z, Luo M, Li W. On submarine sediments and deposition process of west part of the South Huanghai Sea.In proc. Int Sym. In; L. Yure ed. On Sedimentation on the Continental shelf,with Spec. Ref. to the East .China Sea[C]. Beijin:China Ocean Press, 1983.689-695

10 Bong Chool Suk. Sedimentology and history of sea level changes inthe East China Sea and adjacent seas[A]. In,Taira A,Masuda F,eds. Sedimentary Facies in the Active Plate Margin [C]. Terra-pub. Tokyo,1989. 215-231

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南黄海表层沉积物中微体化石的沉积特点及物源分析

国家海洋局第一海洋研究所,青岛 266003

基金项目: 国家科技部基础研究项目;中韩科技合作项目;国家海洋局青年基金(97401)

作者简介:
程振波，男，1956年出生，副研究员，海洋地质及微体古生物。

收稿日期: 1999-03-26
修回日期: 1999-05-04
刊出日期: 1999-12-10

中图分类号: P736.21;Q913.6

关键词:

微体化石 /

沉积特点 /

类型 /

物源

摘要: 借助于对南黄海表层沉积物中微体化石的分析，探讨了不同的微体化石数量及组合的分布特点、沉积特征、微体化石浮游有孔虫、钙质超微化石与黑潮、黄海暖流、黄海冷水团、黄海沿岸流之间的关系。同时根据本区的粒度分析资料，把表层沉积物划归为下列类型。南黄海中、西部：1粘土沉积，2．粉研质粘土沉积，3．细砂与粉砂沉积，4砂砾等混杂沉积；东侧：从北至南依次排列为砂、泥质沙、抄质泥和泥质沉积。此外，对南黄海表层沉积物的物源归纳为以下几种：1．黄河源，2．长江源，3．陆架残留砂源，4．（韩国）锦江、汉江等源，5．风尘源。

English Abstract

The Analysis of the Sedimentary Character of the Microfossils and the Material Resource in the Surface Sediments from the South Yellow Sea

First Institute of Oceanography,SOA. Qingdao Shandong China 266003

Received Date: 1999-03-26
Rev Recd Date: 1999-05-04
Publish Date: 1999-12-10

Keywords:

Abstract: The area of the Yellow Sea is about 417 thousands square kilometres and is divided into north and South two parts according to the boundary line between the Chengshantou of Shandong Province and the Bailing Islands of Korea. Of which the North Yellow Sea is about 100 thousands square kilometres. The South Yellow Sea is three times as much as the North Yellow Sea. China began to study the sediments of the Yellow Sea from the 1950s and have got much scientific achievement. After 1970s,Institute of Oceanology,the Chinese Academy of Sciences the Tongji University First Institute of Oceanography,state Oceanic Administration had investigated and studied the surface and core samples from the Yellow Sea in varying degrees early or late. After the late 1980s,the previous Institute of Marine Geology,Ministry of Geology and Mineral Resources had made a study of the sequence of bedding and the stratigraphic correlation in the Quaternary.Above-mentioned study laid a foundation for the study of the South Yellow Sea. In this paper,the numbers of different microfossils and the distribution character of associations the sedimentary character the relationship among the microfossils planktonic foraminifera、calcareous nanoplank-fossils and Black Stream、the warm current of the Yellow Sea、the cold water mass、the coastal current of the Yellow Sea have been studied by means of the analysis of microfossils in the surface sediments from the South Yellow Sea. At same time,according to the data of size,the types of the surface sediments have been divided as follows:in the middle-west areas of the South Yellow Sea,1. clay 2. silt clay 3. fine-sand and silt 4. sand-gravel and mixtum,and in the east area,the sediments are arranged for inturn sand 、mud sand、sand mud and mud from the north to the south. In addition,the material resource in the surface sediments from the South Yellow Sea might be summed up following:1. the material cources of the Yellow River 2. the material sources of the Changjiang 3. the material sources of the remnant sand 4. the material sources of the Hanjiang and ]in- jiang etc. (Korean). 5. the material sources of eolian depos.

程振波, 石学法, 陈志华, 鞠小华. 南黄海表层沉积物中微体化石的沉积特点及物源分析[J]. 沉积学报, 1999, 17(S1): 775-781.

引用本文:

程振波, 石学法, 陈志华, 鞠小华. 南黄海表层沉积物中微体化石的沉积特点及物源分析[J]. 沉积学报, 1999, 17(S1): 775-781.

Citation:

CHENG Zhen-bo, SHI Xue-fa, CHEN Zhi-hua, Ju Xiaohua. The Analysis of the Sedimentary Character of the Microfossils and the Material Resource in the Surface Sediments from the South Yellow Sea[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 775-781.

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南黄海表层沉积物中微体化石的沉积特点及物源分析

作者简介:
程振波，男，1956年出生，副研究员，海洋地质及微体古生物。

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The Analysis of the Sedimentary Character of the Microfossils and the Material Resource in the Surface Sediments from the South Yellow Sea

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南黄海表层沉积物中微体化石的沉积特点及物源分析

国家海洋局第一海洋研究所,青岛 266003

作者简介:
程振波，男，1956年出生，副研究员，海洋地质及微体古生物。

English Abstract

The Analysis of the Sedimentary Character of the Microfossils and the Material Resource in the Surface Sediments from the South Yellow Sea

First Institute of Oceanography,SOA. Qingdao Shandong China 266003

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南黄海表层沉积物中微体化石的沉积特点及物源分析

作者简介: 程振波，男，1956年出生，副研究员，海洋地质及微体古生物。

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The Analysis of the Sedimentary Character of the Microfossils and the Material Resource in the Surface Sediments from the South Yellow Sea

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出版历程

目录

南黄海表层沉积物中微体化石的沉积特点及物源分析

国家海洋局第一海洋研究所,青岛 266003

作者简介: 程振波，男，1956年出生，副研究员，海洋地质及微体古生物。

English Abstract

The Analysis of the Sedimentary Character of the Microfossils and the Material Resource in the Surface Sediments from the South Yellow Sea

First Institute of Oceanography,SOA. Qingdao Shandong China 266003

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
程振波，男，1956年出生，副研究员，海洋地质及微体古生物。

作者简介:
程振波，男，1956年出生，副研究员，海洋地质及微体古生物。