安徽霍山戴家院西周文化遗址含液化脉变形物质微观细结构

姚大全, 沈小七, 张小雷, 杨源源, 赵朋, 郑海刚. 安徽霍山戴家院西周文化遗址含液化脉变形物质微观细结构[J]. 地球物理学进展, 2017, 32(2): 538-545. doi: 10.6038/pg20170212
引用本文: 姚大全, 沈小七, 张小雷, 杨源源, 赵朋, 郑海刚. 安徽霍山戴家院西周文化遗址含液化脉变形物质微观细结构[J]. 地球物理学进展, 2017, 32(2): 538-545. doi: 10.6038/pg20170212
YAO Da-quan, SHEN Xiao-qi, ZHANG Xiao-lei, YANG Yuan-yuan, ZHAO Peng, ZHENG Hai-gang. Micro-fine structure of deformation materials of including liquefaction vein in cultural layer of Western Zhou Dynasty on Daijiayuan site, Huoshan, Anhui province[J]. Progress in Geophysics, 2017, 32(2): 538-545. doi: 10.6038/pg20170212
Citation: YAO Da-quan, SHEN Xiao-qi, ZHANG Xiao-lei, YANG Yuan-yuan, ZHAO Peng, ZHENG Hai-gang. Micro-fine structure of deformation materials of including liquefaction vein in cultural layer of Western Zhou Dynasty on Daijiayuan site, Huoshan, Anhui province[J]. Progress in Geophysics, 2017, 32(2): 538-545. doi: 10.6038/pg20170212

安徽霍山戴家院西周文化遗址含液化脉变形物质微观细结构

详细信息
    作者简介:

    姚大全,男,1956年8月生,研究员,主要从事构造地质和地震地质学研究.(E-mail:daquany@aheq.gov.cn)

  • 中图分类号: P313

Micro-fine structure of deformation materials of including liquefaction vein in cultural layer of Western Zhou Dynasty on Daijiayuan site, Huoshan, Anhui province

  • 以梅山—龙河口断裂近侧安徽霍山戴家院遗址再发掘所揭示出的自然变形痕迹为主要研究对象,结合前期工作对比分析,识别编录其变形形态,分析其活动习性,定向采集含液化脉变形物质,在保持原态基础上进行微观分析.发现一系列丰富的微观变形组构和组合,如波浪状、流动构造和定向排列组构,有机颗粒悬浮等;脉体形态多种多样,见原地碎裂,弥漫性裂隙,在脉体及旁侧基质见先成纹层被扰动,被扭曲甚至被冲断,产生微破裂、穿切和揉皱等,多处显现流动-挤压-冲断递进变形过程,呈现丰富的微观变形细节.地震液化脉微观变形特征的提炼对液化脉多尺度的识别研究是有益的.
  • 加载中
  • [1]

    Bartholomew M J, Brodie B M, Willoughby B H, et al. 2002. Mid-Tertiary paleoseismites:Syndepositional features and section restoration used to indicate paleoseismicity, Atlantic Coastal Plain, South Carolina and Georgia[A].//Ettensohn F R, Rast N, Brett C E eds. Ancient Seismites. Geological Society America Special Paper 369[M]. Boulder, Colorado, USA, 63-74.

    [2]

    Davenport C A, Ringrose P S. 1987. Deformation of Scottish Quaternary sediment sequences by strong earthquake motion[A].//Jones M E, Preston R M F eds. Deformation of Sediments and Sedimentary Rocks[M]. London:Geological Society, Special Publication, 29:299-314.

    [3]

    Du Y S, Han X. 2000. Seismo-deposition and seismites[J]. Advance in Earth Sciences (in Chinese), 15(4):389-394, doi:10.3321/j.issn:1001-8166.2000.04.005.

    [4]

    He Y N, Yang Z E. 1985. Study on micro-indications of Paleo-earthquake and its significance[J]. Earthquake Research in China (in Chinese), 1(3):76-81.

    [5]

    Moretti M, Pieri P, Tropeano M. 2002. Late Pleistocene soft-sediment deformation structure interpreted as seismites in paralic deposits in the City of Bari (Apulian foreland, southern Italy)[A].//Ettensohn F R, Rast N, Brett C E eds. Ancient Seismites. Geological Society America Special Paper 369[M]. Boulder, Colorado, USA, 359:75-85.

    [6]

    Obermeier S F. 1996. Use of liquefaction-induced features for paleoseismic analysis-An overview of how seismic liquefaction features can be distinguished from other features and how their regional distribution and properties of source sediment can be used to infer the location and strength of Holocene paleo-earthquakes[J]. Engineering Geology, 44(1-4):1-76.

    [7]

    Tian H S, Yuan J, Zhang S H, et al. 2006. The correlation of liquefied vein structures caused by earthquake in different geological periods in the Yishu fault zone and its vicinity[J]. Acta Sedimentologica Sinica (in Chinese), 24(4):496-501.

    [8]

    Yao D Q. 2004. Macroscopic and microscopic evidence of periodical stick-slip deformation in an active fault[J]. Recent Developments in World Seismology (in Chinese), (4):6-10.

    [9]

    Yao D Q, Shuo Z, Chen A G, et al. 2010. Discovery and initial study of characteristics of the natural deformation vestige of Daijiayuan ruins at Huoshan in Anhui province[J]. Progress in Geophysics (in Chinese), 25(2):454-459, doi:10.3969/j.issn.1004-2903.2010.02.011.

    [10]

    Yao D Q, Shuo Z, Shen X Q, et al. 2009. Significance and microscopic analyzing of deformation in cultural remains of the Nestern Zhou dynasty-late spring and autumn period at Daijiayuan ruins at Huoshan, Anhui Province[J]. Earthquake Research in China (in Chinese), 25(4):424-431.

    [11]

    附中文参考文献

    [12]

    杜远生, 韩欣. 2000. 论震积作用和震积岩[J]. 地球科学进展, 15(4):389-394, doi:10.3321/j.issn:1001-8166.2000.04.005.

    [13]

    何永年, 杨主恩. 1985. 古地震的微观标志研究及其意义[J]. 中国地震, 1(3):76-81.

    [14]

    田洪水, 袁静, 张慎河,等. 2006. 沂沭断裂带及其近区不同地质时期地震液化脉构造对比[J]. 沉积学报, 24(4):496-501.

    [15]

    姚大全. 2004. 活动断层周期性粘滑变形的宏观和微观证据[J]. 国际地震动态, (4):6-10.

    [16]

    姚大全, 朔知, 陈安国,等. 2010. 安徽霍山戴家院遗址自然变形遗迹的发现及其特征初探[J]. 地球物理学进展, 25(2):454-459, doi:10.3969/j.issn.1004-2903.2010.02.011.

    [17]

    姚大全, 朔知, 沈小七,等. 2009. 安徽霍山戴家院西周-春秋晚期文化层物质变形的显微分析及其意义[J]. 中国地震, 25(4):424-431.

  • 加载中
计量
  • 文章访问数:  684
  • PDF下载数:  6
  • 施引文献:  0
出版历程
收稿日期:  2016-06-12
修回日期:  2017-01-16
刊出日期:  2017-04-20

目录