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作 者:CHEN Qingqiang 1,3 , LI Congxian\+1 and CONG Youzi\+2 1. Marine Geology Laboratory, Tongji University, Shanghai 200092, China 2. First Institute of Oceanography, State Oceanic Administration of China, Qingdao 266003, China 3. Guangzhou Institute of
出 处:《Chinese Science Bulletin》1998年第22期1917-1921,共5页
基 金:theNationalNaturalScienceFoundationofChina(GrantNos .4 96 76 2 882 94 76 2 80 )
摘 要:Comparison of magnetic fabric parameters of deposits in different modern sedimentary environments indicates that values of \%P, F\% and \%L\% of eolian deposits are lower obviously than those of hydrogenic ones respectively. On relationship diagrams of magnetic fabric parameters, data points of eolian samples concentrated in limited area near origin of coordinates indicate that dynamic intensity is lower with less variation; while those of hydrogenic ones depart from origin of coordinates suggest higher intensity of sedimentary dynamics. Analyses of dynamic characteristics of different sedimentary environments indicate that values of magnetic fabric parameters of deposits are determined by dynamic types and characteristics of depositional processes. Magnetic fabric analyses of deposits are effective in determination of sedimentary environments.Comparison of magnetic fabric parameters of deposits in different modern sedimentary environments indicates that values ofP, F andL of eolian deposits are lower obviously than those of hydrogenic ones respectively. On relationship diagrams of magnetic fabric parameters, data points of eolian samples concentrated in limited area near origin of coordinates indicate that dynamic intensity is lower with less variation; while those of hydrogenic ones depart from origin of coordinates suggest higher intensity of sedimentary dynamics. Analyses of dynamic characteristics of different sedimentary environments indicate that values of magnetic fabric parameters of deposits are determined by dynamic types and characteristics of depositional processes. Magnetic fabric analyses of deposits are effective in determination of sedimentary environments.
关 键 词:magnetic FABRIC PARAMETERS SEDIMENTARY environment transporting medium.
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