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泥质潮坪磁组构特征及其意义研究
引用本文:丛友滋,李从先.泥质潮坪磁组构特征及其意义研究[J].海洋地质与第四纪地质,1997,17(1):13-16.
作者姓名:丛友滋  李从先
作者单位:[1]国家海洋局第一海洋研究所 [2]上海同济大学
摘    要:在1988年-1993年期间,对河北歧口及上海南汇海岸带泥质潮坪现行滩面积浦西曹杨新村近代亚潮坪沉积剖面进行了沉积动力环境与沉积动力环境与沉积磁组构特征测量分析。现行开敞海岸同物源潮坪沉积磁且构参量量值特征显示出,其K值高滩为高值,低潮滩次之,中潮滩为低。亚近开敞海岸泥质潮坪沉积剖面磁组构测量结果;K值是区分潮坪沉积动力活动带的高分辨率标志;P、L、F、q是分析潮坪沉积结构的分辨率标志;q是分析潮

关 键 词:沉积  湖泊  泥质潮坪  磁组构特征  高分辨率

MAGNETIC FABRIC CHARACTERISTICS OF TIDAL MUD FLAT AND ITS STUDY SIGNIFICANCE
Cong Youzi,Han Guozhong.MAGNETIC FABRIC CHARACTERISTICS OF TIDAL MUD FLAT AND ITS STUDY SIGNIFICANCE[J].Marine Geology & Quaternary Geology,1997,17(1):13-16.
Authors:Cong Youzi  Han Guozhong
Abstract:The measurements and analyses of sedimentary dynamics and magnetic fabrics were done for modern tidal mud flat sediments at the coast of Qikou in Hebei Province and Nanhui in Shanghai and also for subrecent tidal flat Sedimentary Profile at Caoyangxincun in Shanghai during 1988 to 1993.Value characteristics of magnetic fabric parameters of different modern coastal tidal flat sediments with the same sources show:high tidal flat has high K value,mesotidal flat has low K value and low tidal flat has middle K value.The measurement results of magnetic fabric of the tidal mud flat sedimentary profile in subrecent open coast show that K is the high resolution parameter to differentiate dynamic zones of tidal flat deposition,P,L,F,and q are those to analyze tidal flat sedimentary textures,and q is that to study tidal flat sedimentary microstructures and tidal flat storm events,and assemblage of K,P,L,F and q can be used to distinguish,with high resolution,low tidal flat sedimentary facies and sublittoral zone sedimentary facies.
Keywords:homologous  tidal  flat  deposition      magnetic  fabric  parameter      high  resolution  
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