Provenance Analysis of Mud along the Min-Zhe Coast since 2 ka BP

XIAO Shang-bin; LI An-chun; JIANG Fu-qing; YOU Zheng; CHEN Li

Article Contents

Article Navigation > Acta Sedimentologica Sinica > 2005 > 23(2): 268-274

XIAO Shang-bin, LI An-chun, JIANG Fu-qing, YOU Zheng, CHEN Li. Provenance Analysis of Mud along the Min-Zhe Coast since 2 ka BP[J]. Acta Sedimentologica Sinica, 2005, 23(2): 268-274.

Citation:

XIAO Shang-bin, LI An-chun, JIANG Fu-qing, YOU Zheng, CHEN Li. Provenance Analysis of Mud along the Min-Zhe Coast since 2 ka BP[J]. Acta Sedimentologica Sinica, 2005, 23(2): 268-274.

Provenance Analysis of Mud along the Min-Zhe Coast since 2 ka BP

1.
Institute of Oceanology, Chinese Academy Sciences, Qingdao Shandong 266071;
2.
Well Logging Corporation of CNPC, Beijing 100043;
3.
Exploration and Production Corporation of CNPC, Beijing 100011

Received Date: 2004-07-05
Rev Recd Date: 2004-09-02
Publish Date: 2005-06-10

Abstract

The clay minerals and elements of the mud along the Min-Zhe Coast since 2 kaBP are analyzed. The provenance of the mud is from sediments of the Yangtze River according to the study of clayminerals. The same results are drawn based on cluster analysis and differentiation function ofmetal elements. It is about 83%～85% of the mud from sediments of the Yangtze River since 2 kaBP according to quantitative calculation, and sediments of the Yellow River did not reach the study area. It also shows that there is no apparent effect on the sedimentary environment and sediment provenance when the Yellow River changed its course and moved northward during the last 2 ka.
- mud along the Min-Zhe Coast,
- clay minerals,
- elements geochemistry,
- provenance

References

[1]

1 秦蕴珊,郑铁民. 东海大陆架沉积物分布特征的初步探讨[A].北京:科学出版社,1982. 39-51.

2 金翔龙. 东海海洋地质[M].北京:海洋出版社,1992.185-215.

3 Milliman J D,Qin Y S,Park Y A. Sediments and sedimentary processes in the Yellow Sea[A].Tokyo:Terra Scientific Publishing Company,1989.233-249.

4 DeMaster D J,Mckee B A,Nitrouer C A. Rates of sediment accumulation and particles reworking based on radiochemical measurements from shelf deposits in the East China Sea[J].Continental Shelf Research,1985.143-158.

5 Yang Z S,Saito Y,Guo Z G. Distal mud area as a material sink in the East China Sea[A].Sapporo:Hokkaido University,1994.1-6.

6 郭志刚,杨作升,曲艳慧. 东海陆架泥质区沉积地球化学比较研究[J].沉积学报,2000,(02):284-289.

7 Milliman J D,Beardsley R C,Yang Z S. Modern Huanghe drived on the Outer Shelf of the East China Sea: identification and potential transport mechanism[J].Continental Shelf Research,1985.175-188.

8 YANG Z S,Milliman J D. Fine-grained sediments of the Changjiang and Huanghe rivers and sediment source of the East China Sea[A].北京:海洋出版社,1983.436-446.

9 郭志刚,杨作升,王兆祥. 黄东海海域水团发育对底质沉积物分布的影响[J].青岛海洋大学学报,1995,(01):75-83.

10 郭志刚,杨作升,雷坤. 东海陆架北部泥质区沉积动力过程的季节性变化规律[J].青岛海洋大学学报,1999,(03):507-513.

11 郭志刚,杨作升,张东奇. 冬、夏季东海北部悬浮体分布及海流对悬浮体输运的阻隔作用[J].海洋学报,2002,(05):71-80.

12 范德江,杨作升,孙效功. 东海陆架北部长江、黄河沉积物影响范围的定量估算[J].青岛海洋大学学报,2002,(05):748-756.

13 杨作升,郭志刚,王兆祥. 黄东海陆架悬浮体向其东部深海区输送的宏观格局[J].海洋学报,1992,(02):81-90.

14 孙效功,方明,黄伟. 黄东海陆架区悬浮体输运的时空变化规律[J].海洋与湖沼,2000,(06):581-587.

15 Saito Y,Yang Z S. Historical change of the Huanghe (Yellow River) and its impact on the sediment budget of the East China Sea[A].Sapporo:Hokkaido University,1994.7-12.

16 肖尚斌,李安春. 东海内陆架泥区沉积物的环境敏感粒度组分[J].沉积学报,2005,(01):122-129.

17 范德江,杨作升,毛登. 长江与黄河沉积物中粘土矿物及地化成分的组成[J].海洋地质与第四纪地质,2001,(04):7-12.

18 贺松林. 东海近岸带沉积物陆源矿物组份的比较研究[J].华东师范大学学报(自然科学版),1991,(01):78-86.

19 杨守业,李从先. 元素地球化学特征的多元统计方法研究-长江与黄河沉积物元素地球化学研究[J].矿物岩石,1999,(01):63-67.

20 屈翠辉,郑建勋,杨绍晋. 黄河、长江、珠江下游控制站悬浮物的化学成分及其制约因素的研究[J].Chinese Science Bulletin,1984,(17):1063-1066.

21 赵一阳,鄢明才. 黄河、长江、中国浅海沉积物地球化学元素丰度比较[J].Chinese Science Bulletin,1992,(13):1201-1204.

22 杨守业,李从先. 长江与黄河现代表层沉积物元素组成及其示踪作用[J].自然科学进展,1999,(10):930-937.

23 Yang S Y,Li C X,Jung H S,Lee H J. Discrimination of geochemical compositions between the Changjiang and the Huanghe sediments and its application for the identification of sediment source in the Jiangsu coastal plain, China[J].Marine Geology,2002,(3/4):229-241.

24 Taylor S R. The continental crust: its composition and evolution, an examination of the geochemical record preserved in sedimentary rocks[M].Blackwell Scientific Publication Oxford,1985.

25 Fralick P W,Kronberg B I. Geochemical discrimination of clastic sedimentary rock sources[J].Sedimentary Geology,1995.111-124.

26 郭志刚,杨作升,范德江. 东海陆架北部表层细粒级沉积物的级配及意义[J].青岛海洋大学学报,2002,(05):741-747.

27 Rollinson H R. Using Geochemical Data: Evaluation, Presentation, Interpretation[M].Longman Scientific and Technical,1993.

28 Cullers R L,Barret T,Carlson R. REE and mineralogic changes in Holocene soil and stream sediment[J].Chemical Geology,1987.275-297.

29 赵一阳,鄢明才. 中国浅海沉积物地球化学[M].北京:科学出版社,1994.

30 Kremling K,Streu P. Saharan dust influenced trace element fluxes in deep North Atlantic Subtropical water[J].Deep-Sea Research,1993,(06):1155-1168.

31 蓝先洪. 珠江三角洲第四纪沉积物TiO2/A1203值及地质意义[J].台湾海峡,1992,(03):227-232.

32 范德江,孙效功,杨作升. 沉积物物源定量识别的非线性规划模型--以东海陆架北部表层沉积物物源识别为例[J].沉积学报,2002,(01):30-33.

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Get Citation

PDF

XML

Article Metrics

Article views(702) PDF downloads(814) Cited by()

Proportional views

Provenance Analysis of Mud along the Min-Zhe Coast since 2 ka BP

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

2. Well Logging Corporation of CNPC, Beijing 100043;

3. Exploration and Production Corporation of CNPC, Beijing 100011

Received Date: 2004-07-05

Rev Recd Date: 2004-09-02

Publish Date: 2005-06-10

Key words:

Abstract: The clay minerals and elements of the mud along the Min-Zhe Coast since 2 kaBP are analyzed. The provenance of the mud is from sediments of the Yangtze River according to the study of clayminerals. The same results are drawn based on cluster analysis and differentiation function ofmetal elements. It is about 83%～85% of the mud from sediments of the Yangtze River since 2 kaBP according to quantitative calculation, and sediments of the Yellow River did not reach the study area. It also shows that there is no apparent effect on the sedimentary environment and sediment provenance when the Yellow River changed its course and moved northward during the last 2 ka.

HTML

Reference (1)

[1]

Provenance Analysis of Mud along the Min-Zhe Coast since 2 ka BP

Abstract

References

Proportional views

通讯作者: 陈斌, bchen63@163.com

Article Metrics

Proportional views

Related