4篇
您的检索式：作者名="Cong Youzi"
|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 1 | Relationship between magnetic fabric parameters and dynamic characteristics of deposits in different environments显示文摘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. | 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 | 1998 | Chinese Science Bulletin1998，43，22： | 1 |
| 2 | Studies on sedimentary events in Mariana Trough and characteristics of geomagnetic field change显示文摘Studies on sedimentary events in Mariana Trough and characteristics of geomagnetic field changeCongYouzi;HanGuozhong;ChengGuo... | Cong Youzi Han Guozhong Cheng Guoliang Sun Yuhang Wei Qingyun and Jiang Li | 1996 | Acta Oceanologica Sinica1996，15，4： | 0 |
| 3 | Magnetic fabric characteristics of late Quaternary strata in Shanghai area显示文摘The result of measurements and analyses on magnetic fabrics data for the late Quaternary core at Caoyangxincun in Shanghai shows that abrupt changes of magnetic fabric curves coincide with the boundaries between the marine strata and underlying stiff clay. Littoral, neritic, subtidal and tidal flat facies in the marine strata have distinct magnetic fabric characteristics. The curves of the parameters, K, P, L, q, display clear boundaries between various facies, which could serve as a new method for the stratigraphic subdivision and correlation. | Daidu Fan Qingqiang Cheng Youzi Cong Congxian Li | 1998 | Chinese Science Bulletin1998，43，18： | 0 |
| 4 | Paleocurrent of the tidal sand body in Subei coastal plain显示文摘Based on analysis of magnetic febric and magnetic relict, the paleocurrents recorded in drilling cores in Subei coastal plain are bidirectional. NE_SW in the northern core and NW_SE in the southern core. The paleocurrent pattern in the area is similar to that of the tidal current system in the South Yellow Sea. So it is inferred that the convergent_divergent tidal current system existed during stage of sand body formation, and they should be radial in plane. | Zhang Jiaqiang Li Congxian Cong Youzi | 1998 | Chinese Science Bulletin1998，43，12： | 0 |
您所在的机构暂未开通此部分的功能，请联系管理员