颅脑外伤分类的CT特征   总被引：2，自引：2，他引：0  

马蜂  李恒国 《CT理论与应用研究》1998,7(3):22-25

本文目的在于进一步提高对多种颅脑损伤的认识水平。所用材料和方法为本组１３５例,男９８例,女３７例,年龄４＿７７岁,平均年龄２４．８３岁。车祸伤９３例,跌伤２８例,击伤１４伤,１０１例有昏迷史,全部病例均作头颅ＣＴ轴位平扫。从相互伴发的多种颅脑损伤的角度,详细分析了它们的ＣＴ表现。结果得到了１３５例中,有多种类型颅脑损伤１３３例,单纯脑挫裂伤２例;硬膜外血肿１０４例,合并同一部位骨折７５例,占７２．１５％,合并脑挫裂伤占７０．３７％;硬膜下血肿２０例,位于外力对冲部位１５例．占７５％,合并脑挫伤裂伤１２例,其中１１例邻近硬膜下血肿;外伤后２小时内ＣＴ检查,并于外伤后４小时至５天内ＣＴ复查４７例,发现病变进展３８例,占８０．９５％。结论为硬膜外血肿多伴同部位骨折;在硬膜外血肿中,伴发的脑挫裂伤多位于对冲部位;硬膜下血肿多发生于对冲部位;颅脑损伤后,短期内病变可能会继续发展。  相似文献   

陕西段家坡黄土剖面中布容／松山古地磁界线附近铱异常的发现及其启示   总被引：3，自引：0，他引：3  

马配学  侯泉林 《地质学报》1998,72(2):173-177

利用高灵敏度放射化学中子活化分析方法,对我国陕西段家坡黄土剖面早－中更新统（约０．７３Ｍａ）沉积界线附近铱和其它元素的丰度进行了测定。结果表明,在布容／松山（Ｂ／Ｍ）古地磁界线附近铱的含量明显增大,最大值为４６．３ｐｇ／ｇ。相对于整个剖面的平均背景值（约１５ｐｇ／ｇ）大约富集了３倍。用地壳元素钪进行标准化之后,铱异常十分明显,而其它元素在界线附近则没有变化。黄土剖面上铱异常的赋存层位与西南太平洋钻  相似文献   

Paleomagnetic result of the Lower-Cretaceous from Luanping basin,Hebei Province and its tectonic implications*     

Zhiming  Sun  Zhenyu  Yang  Xinghua  Ma  Yue  Zhao 《中国科学:地球科学(英文版)》1998,41(2):43-50

A paleomagnetic study of about 95 samples from 16 sites sampled in the Early Cretaceous in Luanping basin in Hebei Province was reported. Stepwise thermal demagnetization was used to isolate magnetic components. Most samples have a characteristic direction with a high temperature component above 500°C. The tectonic-corrected data areD = 347.8°,I = 50.4°, α₉₅ = 7.l°, and the corresponding pole position is at 76.1°N, 346.3°E,with dp =6.4°,dm = 3.8°, paleolatitude λ = 31.1°N. This result indicates a counterclockwise post-Cretaceous rotation of 30.7° ±9.8° with respect to the stable Ordos basin in the west of North China Block, and a non-significant northward motion. This rotation could be related to local fault action or structural detachment, or regional NNW-NWWward motion and collision of Kula-Pacific plate with eastern China since the Early Cretaceous.

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粉末冶金在探矿工程中的应用   总被引：1，自引：1，他引：0       下载免费PDF全文

丁华东  马明亮  杨晓华  浩宏奇  金志浩 《探矿工程》1998,(1):43-45

介绍了粉末冶金技术及产品在探矿工程中的应用,回顾了硬质合金钻进的历史;讨论了粉末冶金技术在金刚石钻头制造中的应用,尤其是近几年的进展,综述了钎头用硬质合材料新发展－梯度硬质合金和铁镍代钴硬质合金。  相似文献   

麦饭石对腐殖酸及重金属离子的吸附作用   总被引：4，自引：0，他引：4  

王强 《地质科技情报》1998,(3)

研究了麦饭石对腐殖酸和重金属离子（Ｈｇ２＋,Ｐｂ２＋,Ｃｕ２＋,Ｚｎ２＋,Ｃｄ２＋）的吸附作用,实验结果表明麦饭石对腐殖酸和重金属离子都具有较好的吸附性能,且腐殖酸的存在有利于麦饭石对重金属离子的吸附。ｐＨ值是影响吸附的重要因素,当ｐＨ值为５．０～６．０时,麦饭石同时吸附腐殖酸和重金属离子的效果最好,麦饭石在吸附腐殖酸和重金属离子的同时能溶出微量元素硒,这对于大骨节病的防治有重要意义。  相似文献   

Genetic relationship of metamorphic reaction and dehydration-melting     

Fulai Liu  Qihan Shen  Yuansheng Eng  Xuechun Xu  Rui Ma 《中国科学D辑(英文版)》1998,41(1):49-56

The high-temperature and pressure experimental data of garnet, sillimantite and biotite-bearing potash feldspar gneiss (SGBG, natural block rock) has shown that metamorphic reactions between garnet and melt, and mineral assemblage evolutional features are not only controlled byP-T condition, but also genetically correlate with dehydration-melting of biotite and partial melting of felsic minerals. Combining experimental data with theoretical analyses, the genetic mechanism of metamorphic reaction and its dynamic significance have been demonstrated in the process of metamorphic evolution of khondalite series on the border of Jin (Shanxi Province)-Inner Mongolia. Project supported by the Youth Geologist Foundation of Ministry of Geology and Mineral Resources of China, the Post-docter Foundation and the National Natural Science Foundation of China (Grant No. 49572138).  相似文献   

Seasonal acceleration of the rate of total ozone decreases over Central Europe: impact of tropopause height changes     

Janusz W. Krzy?cin  Ma?gorzata Degórska  Bonawentura Rajewska-Wich 《Journal of Atmospheric and Solar》1998,60(18):1755-1762

Total ozone data from some European stations have been analyzed to detect the ozone decrease in different seasons from 1979 to 1995. The differences between the winter–spring (December–March) and summer (May–August) total ozone means have decreased distinctly during the last three decades, by 10 Dobson Units per decade, showing that the winter–spring decrease is significantly stronger than the summer one. Applying a multiple regression model to the monthly means of tropopause height, positive trends in the summer and winter–spring seasons have been found, especially since 1979. This corresponds to the accelerating ozone decrease then. The possibility of using tropopause height variations as an indicator of dynamical variability in the total ozone trend model is discussed. The total ozone response to the changes of tropopause height seems to be independent of timescale over which the tropopause-total ozone relationship has been examined (month-to-month, interannual). The total ozone trends, as well as the accelerated rate of ozone decrease since 1979 in the winter–spring and summer seasons, respectively, are reduced by about 0.5–1% per decade after inclusion of the tropopause height effect on the ozone model.  相似文献   

青藏高原三维变形运动学的时段划分和新构造分区   总被引：80，自引：3，他引：77  

马宗晋  张家声 《地质学报》1998,72(3):211-227

青藏高原形成至今经历了4个互有叠接的构造期。α期以南北缩短和向北推移为主,主要发生在45～35 Ma期间,β期表现为长周期缓慢隆升,在35～5.3 Ma期间占主导地位;γ期为短周期快速隆升阶段,自5.3Ma开始,3.0 Ma以后逐渐达到高峰;δ期以东西向伸展变形为特征,3.0 Ma以前出现在喜马拉雅地区,3.0 Ma以后遍及整个高原.第四纪以后表现为占主导地位的变形运动形式。根据γ期和δ期构造变动在空间和时间上的不均匀性,把青藏高原划分为西藏、羌塘和柴达木3个构造域。  相似文献   

长江中下游及邻区基底和花岗岩成矿元素丰度背景的研究   总被引：7，自引：0，他引：7  

马振东  张本仁 《地质学报》1998,72(3):267-275

本文系统地研究了长江中下游及邻区的结晶基底,褶皱基底及花岗岩岩基成矿元素丰度背景,从而为区域Ｃｕ、Ａｕ,Ｗ、Ｓｎ等成矿作用提供了一套完整的基础地球化学数据,用此来作为窥视地壳组成及成矿作用时空演变的窗口。  相似文献   

Paleomagnetic result of the Lower-Cretaceous from Luanping basin,Hebei Province and its tectonic implications*     

Sun Zhiming  Yang Zhenyu  Ma Xinghua  Zhao Yue 《中国科学D辑(英文版)》1998,41(2):43-50

A paleomagnetic study of about 95 samples from 16 sites sampled in the Early Cretaceous in Luanping basin in Hebei Province was reported. Stepwise thermal demagnetization was used to isolate magnetic components. Most samples have a characteristic direction with a high temperature component above 500°C. The tectonic-corrected data areD = 347.8°,I = 50.4°, α₉₅ = 7.l°, and the corresponding pole position is at 76.1°N, 346.3°E,with dp =6.4°,dm = 3.8°, paleolatitude λ = 31.1°N. This result indicates a counterclockwise post-Cretaceous rotation of 30.7° ±9.8° with respect to the stable Ordos basin in the west of North China Block, and a non-significant northward motion. This rotation could be related to local fault action or structural detachment, or regional NNW-NWWward motion and collision of Kula-Pacific plate with eastern China since the Early Cretaceous.  相似文献