The Character of Grain Size Analysis and Quartz Surface Texture of Sand Dunes in the Dowenriver of Tumen River

MA Feng; LIU Li; WANGAn-ping; CAO Lin

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Article Navigation > Acta Sedimentologica Sinica > 2004 > 22(2): 261-266

MA Feng, LIU Li, WANGAn-ping, CAO Lin. The Character of Grain Size Analysis and Quartz Surface Texture of Sand Dunes in the Dowenriver of Tumen River[J]. Acta Sedimentologica Sinica, 2004, 22(2): 261-266.

Citation:

MA Feng, LIU Li, WANGAn-ping, CAO Lin. The Character of Grain Size Analysis and Quartz Surface Texture of Sand Dunes in the Dowenriver of Tumen River[J]. Acta Sedimentologica Sinica, 2004, 22(2): 261-266.

The Character of Grain Size Analysis and Quartz Surface Texture of Sand Dunes in the Dowenriver of Tumen River

College of Earth Sciences, Jilin University, Changchun 130026

Received Date: 2003-05-29
Rev Recd Date: 2003-08-05
Publish Date: 2004-06-10

Abstract

Through the grain size analysis of sand dunes in the lower reach of the Tumen River, it is found that the frequency cumulative distribution curves are the double peak and the Sk i of the grains are negative,moreover, the change of the grain size is great and the mean value of the standard deviation is 0.64Ф,the sedimentary environment of dunes by the grain size analysis is neriticenvironment; With the analysis of Transmission Eletronic Microscopy (TEM), the shape of the quartz grains are subangular and the principaltraces of mechanical action which underwent are conchoidal breakages and V-shaped percussion pit. The quartz grains havedeveloped chemical action, mainly are middle-strong chemical corrosion; The surface textures of the quartz grains indicate that the sediments are mainly embouchureenvironment; The result of sand dunes'TL age show that the sand dunes were affected by the change of the sea-level in Holocene epoch and experienced the weathering.
- Tumen River,
- grain size analysis,
- surface texture,
- sedimentary environment

References

[1]	曲希玉,刘立,高福红,等. 图门江口附近沙丘的成因. 海洋地质动态,2002,18(6):6～10[Qu Xiyu , Liu Li , Gao Fuhong, et al. The Origin of sand dune in the vicinity of Tumenjiang River. Marine Geology Letters, 2002,18(6):6～10]
[2]	谢又予,催之久,李洪云,等.中国石英砂表面结构特征图谱. 北京:海洋出版社,1984.3～148[Xie Youyu ,Cui Zhijiu ,Li Hongyun, et al. Atlas of quartz sand surface textural features of China Micrographs. Beijing: Marine Publishing House,1984. 3～148]
[3]	Whalley W B, Krinsley D H.A scanning electron microscopy study of surface textures of quartz grains from glacial environments.Sedimentology,1974,21:87～105
[4]	Williams A T, Thomas M C. Analysis of barrier island surface sediments by scanning electron microscopy. Marine Geology,1989,86:101～118
[5]	梁桂香.沉积岩石学实习教材.长春:吉林科学技术出版社,1995. 73～90[Liang Guixiang. Teaching material of the sedimentary petrology. Changchun: Jilin Science and Technology Press, 1995.73～90]
[6]	李珍,张家武,马海洲. 西宁黄土石英颗粒表面结构与黄土物质来源探讨. 沉积学报,1999,17(2):221～225[Li Zhen,Zhang Jiawu,Ma Haizhou.Discussion on the texture features of quartz grains and their origin in the Xining Loess. Acta Sedimentologica Sinica,1999,17(2): 221～225]
[7]	王祥珍,吴时国,李传荣, 等.南极普里兹湾柱样中石英颗粒的表面结构.极地研究,1997,9(2):91～104[Wang Xiangzhen, Wu Shiguo, Li Chuanrong. Surface textures of quartz grains from a core of the Antarctic Prydz Bay. Chinese Journal of Polar Research,1997,9(2):91～104]
[8]	王颖,迪纳瑞尔 B.石英砂表面结构模式图集. 北京: 科学出版社,1985,2～9[Wang Ying ,Bhan Deonarine. Model atlas of surface textures of quartz sand. Beijing: Science Press,1985. 2～9
[9]	陈方,朱大奎.海岸、内陆沙漠与大陆架沙质沉积石英颗粒表面结构的对比研究.地理学报,1999,54(2):134～141[Chen Fang, Zhu Dakui. A critical evaluation of the hypothesis of Chinese continental shelf desertification. Acta Geographica Sinica,1999,54(2):134～141]
[10]	蓝东兆,许江,陈承惠.冲绳海槽晚第四纪沉积硅藻及其古海洋学意义.台湾海峡,2000,19(4):419～425[Lan Dongzhao, Xu Jiang,Chen Chenghui. Late quaternary sedimentary diatom okinawa trough and its paleoceanographical significance. Journal of Oceanography in Taiwan Strait,2000,19(4):419～425]
[11]	成都地质学院陕北队.沉积岩(物)粒度分析及应用.北京:地质出版社,1978,90～100[The geology team of Chengdu college of geology. Application Analysis of Grain Size. Beijing: Geology Publishing House,1978.90～100]
[12]	Friedman G M. Distinction between dune beach and river sands from their textural characteristics. Sedimentary Petrology, 1961,31:514～529
[13]	Friedman G M. In defense of point counting analysis: hypothetical experiments versus real rocks. Sedimentology,1965,4:252～253
[14]	Friedman G M. Dynamic processes and statistical parameters compared for size frequency distribution of beach and river sands. Sedimentary Petrology,1967,37:327～354
[15]	黄求获,徐文强.我国不同海区沉积物石英颗粒表面的微结构.海洋科学,1997,2:43～47[Huang Qiuhuo, Xu Wenqiang .Surface microtextures of quartz grains in the sediments of China Seas.Marine Science, 1997,2:43～47]
[16]	陈丽华,缪昕,于众. 扫描电镜在地质上的应用.北京:科学出版社,1986.21-44[Chen Lihua,Miao Xin, Yu Zhong. The practical application of transmission electronic microscopy in geology. Beijing: Science Press,1986. 21～44]
[17]	赵希涛,唐领余,沈才明.江苏建湖庆丰剖面全新世气候变迁和海面变化.海洋学报,1994,16(1):78～88[Zhao Xitao, Tang Lingyu, Shen Caiming. Holocene climate and the change of sea level in Jianhu County, Jiangsu Province. Acta Oceanologica Sinica,1994, 16(1):78～88]
[18]	吴学忠,王绍鸿,赵希涛.江苏建湖地区全新世孢粉组合及其地质、古地理意义.地理科学,1996,16(3):252～259[Wu Xuezhong, Wang Shaohong, Zhao Xitao. Holocene sporo-pollen assemblages and their poleogenographical significance in Jianhu County,Jiangsu Province. Scientia Geographica Sinica,1996,16(3):252～259]
[19]	Tsukada M. Vegetation and climate during the last glacial maximum in Japan. Quatenary Research, 1983, 19:212～235
[20]	滕继奎, 张勃夫. 珲春经济开发区环境地质问题研究.吉林地质,1997,16(3):36～41[Teng Jikui,Zhang Bofu. A study on the environmental geology in the Hunchun Economic Development Zone. Jilin Geology, 1997,16(3):36～41]
[21]	丁立.图门江地区的气候环境. 吉林气象,1997,4:23～25[Ding Li. The Weathering and Environment of Tumen. Jilin Weather, 1997,4: 23～25]
[22]	Pye K. Models of transgressive coastal dune building episodes and their relationgship to Quaternary sea level changes: a discussion with reference to evidence from eastern Australia. In: Clark M W, ed. Coastal research: UK perspectives. Geo-books Regency House, 1984. 81～104

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The Character of Grain Size Analysis and Quartz Surface Texture of Sand Dunes in the Dowenriver of Tumen River

College of Earth Sciences, Jilin University, Changchun 130026

Received Date: 2003-05-29

Rev Recd Date: 2003-08-05

Publish Date: 2004-06-10

Key words:

Abstract: Through the grain size analysis of sand dunes in the lower reach of the Tumen River, it is found that the frequency cumulative distribution curves are the double peak and the Sk i of the grains are negative,moreover, the change of the grain size is great and the mean value of the standard deviation is 0.64Ф,the sedimentary environment of dunes by the grain size analysis is neriticenvironment; With the analysis of Transmission Eletronic Microscopy (TEM), the shape of the quartz grains are subangular and the principaltraces of mechanical action which underwent are conchoidal breakages and V-shaped percussion pit. The quartz grains havedeveloped chemical action, mainly are middle-strong chemical corrosion; The surface textures of the quartz grains indicate that the sediments are mainly embouchureenvironment; The result of sand dunes'TL age show that the sand dunes were affected by the change of the sea-level in Holocene epoch and experienced the weathering.

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Reference (22)

[1]	曲希玉,刘立,高福红,等. 图门江口附近沙丘的成因. 海洋地质动态,2002,18(6):6～10[Qu Xiyu , Liu Li , Gao Fuhong, et al. The Origin of sand dune in the vicinity of Tumenjiang River. Marine Geology Letters, 2002,18(6):6～10]
[2]	谢又予,催之久,李洪云,等.中国石英砂表面结构特征图谱. 北京:海洋出版社,1984.3～148[Xie Youyu ,Cui Zhijiu ,Li Hongyun, et al. Atlas of quartz sand surface textural features of China Micrographs. Beijing: Marine Publishing House,1984. 3～148]
[3]	Whalley W B, Krinsley D H.A scanning electron microscopy study of surface textures of quartz grains from glacial environments.Sedimentology,1974,21:87～105
[4]	Williams A T, Thomas M C. Analysis of barrier island surface sediments by scanning electron microscopy. Marine Geology,1989,86:101～118
[5]	梁桂香.沉积岩石学实习教材.长春:吉林科学技术出版社,1995. 73～90[Liang Guixiang. Teaching material of the sedimentary petrology. Changchun: Jilin Science and Technology Press, 1995.73～90]
[6]	李珍,张家武,马海洲. 西宁黄土石英颗粒表面结构与黄土物质来源探讨. 沉积学报,1999,17(2):221～225[Li Zhen,Zhang Jiawu,Ma Haizhou.Discussion on the texture features of quartz grains and their origin in the Xining Loess. Acta Sedimentologica Sinica,1999,17(2): 221～225]
[7]	王祥珍,吴时国,李传荣, 等.南极普里兹湾柱样中石英颗粒的表面结构.极地研究,1997,9(2):91～104[Wang Xiangzhen, Wu Shiguo, Li Chuanrong. Surface textures of quartz grains from a core of the Antarctic Prydz Bay. Chinese Journal of Polar Research,1997,9(2):91～104]
[8]	王颖,迪纳瑞尔 B.石英砂表面结构模式图集. 北京: 科学出版社,1985,2～9[Wang Ying ,Bhan Deonarine. Model atlas of surface textures of quartz sand. Beijing: Science Press,1985. 2～9
[9]	陈方,朱大奎.海岸、内陆沙漠与大陆架沙质沉积石英颗粒表面结构的对比研究.地理学报,1999,54(2):134～141[Chen Fang, Zhu Dakui. A critical evaluation of the hypothesis of Chinese continental shelf desertification. Acta Geographica Sinica,1999,54(2):134～141]
[10]	蓝东兆,许江,陈承惠.冲绳海槽晚第四纪沉积硅藻及其古海洋学意义.台湾海峡,2000,19(4):419～425[Lan Dongzhao, Xu Jiang,Chen Chenghui. Late quaternary sedimentary diatom okinawa trough and its paleoceanographical significance. Journal of Oceanography in Taiwan Strait,2000,19(4):419～425]
[11]	成都地质学院陕北队.沉积岩(物)粒度分析及应用.北京:地质出版社,1978,90～100[The geology team of Chengdu college of geology. Application Analysis of Grain Size. Beijing: Geology Publishing House,1978.90～100]
[12]	Friedman G M. Distinction between dune beach and river sands from their textural characteristics. Sedimentary Petrology, 1961,31:514～529
[13]	Friedman G M. In defense of point counting analysis: hypothetical experiments versus real rocks. Sedimentology,1965,4:252～253
[14]	Friedman G M. Dynamic processes and statistical parameters compared for size frequency distribution of beach and river sands. Sedimentary Petrology,1967,37:327～354
[15]	黄求获,徐文强.我国不同海区沉积物石英颗粒表面的微结构.海洋科学,1997,2:43～47[Huang Qiuhuo, Xu Wenqiang .Surface microtextures of quartz grains in the sediments of China Seas.Marine Science, 1997,2:43～47]
[16]	陈丽华,缪昕,于众. 扫描电镜在地质上的应用.北京:科学出版社,1986.21-44[Chen Lihua,Miao Xin, Yu Zhong. The practical application of transmission electronic microscopy in geology. Beijing: Science Press,1986. 21～44]
[17]	赵希涛,唐领余,沈才明.江苏建湖庆丰剖面全新世气候变迁和海面变化.海洋学报,1994,16(1):78～88[Zhao Xitao, Tang Lingyu, Shen Caiming. Holocene climate and the change of sea level in Jianhu County, Jiangsu Province. Acta Oceanologica Sinica,1994, 16(1):78～88]
[18]	吴学忠,王绍鸿,赵希涛.江苏建湖地区全新世孢粉组合及其地质、古地理意义.地理科学,1996,16(3):252～259[Wu Xuezhong, Wang Shaohong, Zhao Xitao. Holocene sporo-pollen assemblages and their poleogenographical significance in Jianhu County,Jiangsu Province. Scientia Geographica Sinica,1996,16(3):252～259]
[19]	Tsukada M. Vegetation and climate during the last glacial maximum in Japan. Quatenary Research, 1983, 19:212～235
[20]	滕继奎, 张勃夫. 珲春经济开发区环境地质问题研究.吉林地质,1997,16(3):36～41[Teng Jikui,Zhang Bofu. A study on the environmental geology in the Hunchun Economic Development Zone. Jilin Geology, 1997,16(3):36～41]
[21]	丁立.图门江地区的气候环境. 吉林气象,1997,4:23～25[Ding Li. The Weathering and Environment of Tumen. Jilin Weather, 1997,4: 23～25]
[22]	Pye K. Models of transgressive coastal dune building episodes and their relationgship to Quaternary sea level changes: a discussion with reference to evidence from eastern Australia. In: Clark M W, ed. Coastal research: UK perspectives. Geo-books Regency House, 1984. 81～104

The Character of Grain Size Analysis and Quartz Surface Texture of Sand Dunes in the Dowenriver of Tumen River

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通讯作者: 陈斌, bchen63@163.com

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