Two different illites in Luochuan Loess, northern Shaanxi province

被引:8
|
作者
Chen, L
Zhang, LF [1 ]
Wang, HJ
Zhou, LP
Chen, J
Yuan, BY
机构
[1] MOE, Key Lab Orogen Belt & Crustal Evolut, Beijing 100871, Peoples R China
[2] Peking Univ, Sch Earth & Space Sci, Beijing 100871, Peoples R China
[3] Peking Univ, Sch Phys, Electron Microscopy Lab, Beijing 100871, Peoples R China
[4] Peking Univ, Coll Environm Sci, Beijing 100871, Peoples R China
[5] Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
来源
CHINESE SCIENCE BULLETIN | 2005年 / 50卷 / 01期
关键词
loess; illite; decomposition of XRD; TEM;
D O I
10.1360/04wd0149
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Two different illites in samples from So to L-10 loess-paleosol sequence at Heimugou section in Luochuan are identified by decomposition of X-ray diffraction (XRD) curve, transmission electronic microscopy (TEM) and energy dispersive X-ray detector (EDX) analyses. Type I illite displays relatively poor crystallinity, wide and blunt XRD peaks, the highest content of which in < 2 mu m clay minerals is up to 55%. Type 11 illite shows good crystallinity, narrow and sharp XRD peaks. The contents of these two types of illites show mutually exclusive relationship in the studied section. The EDX analyses indicate that in contrast to the illite with good crystallinity, the illite with poor crystallinity is enriched in K+, Si4+ and depleted in Al3+.
引用
收藏
页码:82 / 87
页数:6
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