高级搜索

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

鄂尔多斯盆地白垩纪沙漠石英沙颗粒表面特征

江新胜 徐金沙 潘忠习

江新胜, 徐金沙, 潘忠习. 鄂尔多斯盆地白垩纪沙漠石英沙颗粒表面特征[J]. 沉积学报, 2003, 21(3): 416-420.
引用本文: 江新胜, 徐金沙, 潘忠习. 鄂尔多斯盆地白垩纪沙漠石英沙颗粒表面特征[J]. 沉积学报, 2003, 21(3): 416-420.
JIANG Xin-sheng, XU Jin-sha, PAN Zhong-xi. Microscopic Features on Quartz Sand Grain Surface in the Cretaceous Desert of Ordos Basin[J]. Acta Sedimentologica Sinica, 2003, 21(3): 416-420.
Citation: JIANG Xin-sheng, XU Jin-sha, PAN Zhong-xi. Microscopic Features on Quartz Sand Grain Surface in the Cretaceous Desert of Ordos Basin[J]. Acta Sedimentologica Sinica, 2003, 21(3): 416-420.

鄂尔多斯盆地白垩纪沙漠石英沙颗粒表面特征

基金项目: 国家自然科学基金项目(批准号:49572113)资助
详细信息
    作者简介:

    江新胜,男,1956年出生,博士,研究员,古生物学和地层学

  • 中图分类号: P534.53

Microscopic Features on Quartz Sand Grain Surface in the Cretaceous Desert of Ordos Basin

  • 摘要: 沉积环境的判别是沉积盆地分析、古地理、古气候研究和储层评价的重要手段。石英具有较大的硬度和较高的化学稳定性,因而其沉积物颗粒表面特征能很好地反映沉积环境,而通过扫描电镜研究石英颗粒表面微细特征是分析沉积环境行之有效的方法。尽管鄂尔多斯盆地早白垩纪志丹群存在沙漠沉积已被广为接受,但石英颗粒表面微细特征分析还比较薄弱。对采自鄂尔多斯盆地白垩纪志丹群洛河组 (K1l)和罗汉洞组 (K1lh)的沙丘沙进行石英颗粒表面微细特征分析的结果表明,其石英沙颗粒表面特征具有明显的风成特征,及易与水成特征相区别。因此,本研究从石英沙颗粒表面特征方面进一步肯定了鄂尔多斯盆地白垩纪古沙漠的存在
  • [1] 陈丽华,缪昕,于众.扫描电镜在地质上的应用[M].北京:科学出版社,1986[Chen Lihua, Miao Xin, Yu Zhong. Application of scanning electron microscope on geology[M]. Beijing: Science Press, 1986]
    [2] 陈丽华,缪昕,魏宝和. 扫描电镜在石油地质上的应用[M].北京:科学出版社,1990[Chen Lihua, Miao Xin, Wei Baohe. Application of scanning electron microscope on oil-geology[M]. Beijing: Science Press, 1990]
    [3] 谢又予.中国石英砂表面结构特征图谱[M].北京:海洋出版社,1984[Xie Youyu. Atlas of quartz sand surface textural features of China micrographs[M]. Beijing: Oceanic Press, 1984]
    [4] 江新胜,李玉文.中国中东部白垩纪沙漠的时空分布及其气候意义[J].岩相古地理,1996,16 (2) : 42~51[Jiang Xinsheng, Li Yuwen. Spatio-temporal distribution of the Cretaceous deserts in central and eastern China and its climatic significance.[J]. Sedimentary Facies and Palaeogeography, 1996,16(2): 42~51]
    [5] Jiang Xinsheng, Li Yuwen, Fu Qingping. Temporal and spatial distribution of Cretaceous deserts in middle and eastern China and its climatic significance[C]. Proc 30th International Congress. No. 8. The Netherlands : VSP International Publishers, 1997, (8) : 73~80
    [6] 江新胜,潘忠习,付清平.鄂尔多斯盆地早白垩世沙漠古风向变化规律及其气候意义[J].中国科学 (D辑),2000, 30 (2): 195~201[Jiang Xinsheng, Pan Zhongxi, Fu Qingping. Regularity of paleowind directions of the Early Cretaceous desert in Ordos Basin and climatic significance[J]. Science in China (Series D),2000,30(2):195~201]
    [7] 江新胜,潘忠习,付清平.白垩纪时期东亚大气环流格局初探[J].中国科学(D辑),2000, 30 (5) : 526~532[Primary study on pattern of General circulation of atmosphere before uplift of the Tibetan Plateau in eastern Asia[J].Science in China (Series D),2000,30(5):526~532]
    [8] 齐骅,李玉文,李国栋.鄂尔多斯盆地志丹群中的沙漠相[J].岩相古地理,1993, 14 (2) : 64~65[Qi Hua,Li Yuwen,Li Guodong.Desert facies in the Zhidan Group in the Ordos Basin[J]. Sedimentary Facies and Palaeogeography,1993,14(2):64~65]
    [9] 齐骅,李国栋.鄂尔多斯盆地志丹群沉积时期的古沙漠盆地体系[J].西北地质科学,1996,17 (1) : 63~89[Qi Hua,Li Guodong.The systems of paleodesert basins in sedimentary period of Zhidan Group,Ordos Basin[J].Northwest Geoscience,1996,17(1):63~89]
    [10] 李思田.含能源盆地沉积体系-中国内陆和近海主要沉积体系类型的典型分析[M].武汉:中国地质大学出版社,1996[Li Sitian.The depositional systems of energy resource bearing basins-typical analyses for main inland and near shore depositional system types[M].Wuhan:China University of Geosciences Press,1996]
    [11] 李孝泽,董光荣,靳鹤龄等.鄂尔多斯白垩系沙丘岩的发现[J].科学通报,1999,44 (8): 874~877[Li Xiaoze,Dong Guangrong,Jin Heling et al.Discovery of Ordos Cretaceous dune rock and its significance[J].Chinese Science Bulletin,1999,44(8):874~877]
    [12] 程守田,刘星.风成古沙漠沉积体系[J].地学前缘, 1999, 6 (增刊): 80[Cheng Shoutian,Liu Xing.Eolian palaeo-desert depositional system[J]. Earth Science Frontiers, 1996, 6(Suppl.):80]
    [13] 程守田,刘星,郭秀蓉等.古沙漠沉积及其层序单元-以鄂尔多斯盆地白垩系为例[J].地球科学,2000, 25 (6): 587~591[Cheng Shoutian, Liu Xing, Guo Xiurong et al. Palaeo-desert depositional and sequence stratigraphic units:An example from Cretaceous continental palaeo-desrt basin in Ordos[J]. Earth Science-Journal of China University of Geosciences,2000,25(6): 587~591]
    [14] 刘星,程守田,郭秀蓉.陆相干旱盆地充填的沙漠层序-以鄂尔多斯盆地白垩系为例[J].西北地质,2000, 33 (1): 50~55[Cheng Shoutian, Liu Xing, Guo Xiurong. The desert filling sequence of arid continental basin: An example from Cretaceous in Ordos Basin[J]. Northwestern Geology, 2000, 33 (1): 50~55]
    [15] 江新胜,陈乐尧,李玉文.西南区白垩纪第三纪沙漠及沉积学问题[J].岩相古地理,1992, (5) : 1~66[Jiang Xinsheng, Chen Leyao, Li Yuwen. Cretaceous-Tertiary deserts in southwestern China and desert sedimentology[J]. Sedimentary Facies and Palaeogeography, 1992, (5): 1~66]
    [16] Cooke R, Warren A, Goudie A. Desert Geomorphology. London: UCL Press, 1993
    [17] 江新胜,潘忠习.中国白垩纪沙漠中的戈壁沉积[J].矿物岩石,2001, 3: 74~80[Jiang Xinsheng, Pan Zhongxi. Gobi sediments in the Cretaceous desert of China[J]. Journal of Mineralogy and Petrology, 2001, 3: 74~80]
  • 加载中
计量
  • 文章访问数:  504
  • HTML全文浏览量:  11
  • PDF下载量:  493
  • 被引次数: 0
出版历程
  • 收稿日期:  2003-03-07
  • 修回日期:  2003-06-11
  • 刊出日期:  2003-09-10

目录

    鄂尔多斯盆地白垩纪沙漠石英沙颗粒表面特征

      基金项目:  国家自然科学基金项目(批准号:49572113)资助
      作者简介:

      江新胜,男,1956年出生,博士,研究员,古生物学和地层学

    • 中图分类号: P534.53

    摘要: 沉积环境的判别是沉积盆地分析、古地理、古气候研究和储层评价的重要手段。石英具有较大的硬度和较高的化学稳定性,因而其沉积物颗粒表面特征能很好地反映沉积环境,而通过扫描电镜研究石英颗粒表面微细特征是分析沉积环境行之有效的方法。尽管鄂尔多斯盆地早白垩纪志丹群存在沙漠沉积已被广为接受,但石英颗粒表面微细特征分析还比较薄弱。对采自鄂尔多斯盆地白垩纪志丹群洛河组 (K1l)和罗汉洞组 (K1lh)的沙丘沙进行石英颗粒表面微细特征分析的结果表明,其石英沙颗粒表面特征具有明显的风成特征,及易与水成特征相区别。因此,本研究从石英沙颗粒表面特征方面进一步肯定了鄂尔多斯盆地白垩纪古沙漠的存在

    English Abstract

    江新胜, 徐金沙, 潘忠习. 鄂尔多斯盆地白垩纪沙漠石英沙颗粒表面特征[J]. 沉积学报, 2003, 21(3): 416-420.
    引用本文: 江新胜, 徐金沙, 潘忠习. 鄂尔多斯盆地白垩纪沙漠石英沙颗粒表面特征[J]. 沉积学报, 2003, 21(3): 416-420.
    JIANG Xin-sheng, XU Jin-sha, PAN Zhong-xi. Microscopic Features on Quartz Sand Grain Surface in the Cretaceous Desert of Ordos Basin[J]. Acta Sedimentologica Sinica, 2003, 21(3): 416-420.
    Citation: JIANG Xin-sheng, XU Jin-sha, PAN Zhong-xi. Microscopic Features on Quartz Sand Grain Surface in the Cretaceous Desert of Ordos Basin[J]. Acta Sedimentologica Sinica, 2003, 21(3): 416-420.
    参考文献 (17)

    目录

      /

      返回文章
      返回