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Formation Depth of Coesite-Bearing Eclogite,Dabie UHPM Zone,China
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作者 LuGuxian LiuRuixun +1 位作者 WangFangzheng ChenJing 《Journal of China University of Geosciences》 SCIE CSCD 2004年第2期206-215,共10页
The plastic deformation of garnet in coesite bearing eclogite, quartz eclogite and garnet amphibolite of the UHPM complex in Yingshan County in the Dabie Mountains has been studied. The stress generated by the strong... The plastic deformation of garnet in coesite bearing eclogite, quartz eclogite and garnet amphibolite of the UHPM complex in Yingshan County in the Dabie Mountains has been studied. The stress generated by the strong tectonic movement was an important component of the total pressure that resulted in the formation of the eclogite in the Dabie UHPM zone. The three dimensional tectonic principal stresses and additional tectonic stress induced hydrostatic pressure [ p s=( σ 1+ σ 2+ σ 3)/3] are reconstructed according to the differential stress and the strain ratio ( α ) of the garnet in the minor coesite bearing eclogite of the Yingshan County. Then the gravity induced hydrostatic pressure ( p g) is calculated following the equation p minus p s, where p is estimated to be 2.8 GPa based on the quartz coesite geobarmeter. Therefore, the thickness of the rock column overlying the coesite bearing eclogite in the Ying shan County is determined ≥32 km. This estimation, significantly different from ≥100 km, the previous one obtained solely based on the weight/specific weight ratio (W/SW), offers a proper explanation for the puzzle that no tracer of the addition of mantle derived material has been found in the Dabie UHPM zone during the process of UHPM, although a number of researchers claim that this process took place at the depth of the mantle (≥100 km). It is concluded that attention should be paid to the additional tectonic stress induced hydrostatic pressure in the study of UHPM zones. 展开更多
关键词 Dabie UHPM zone formation depths additional tectonic stress-induced hydrostatic pressure coesite-bearing eclogite tectonic physicochemistry plastic deformation garnet
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Ultrastructural Observation of Fallopian Tubes in Patients with Pelvic Congestion Syndrome after Oviductal Ligation
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作者 张瑜 蔡光宗 +1 位作者 刘健 魏家芳 《Journal of Reproduction and Contraception》 CAS 1997年第1期22-26,共5页
The morphological basis of bilateral lower abdominal pain was studied by means of ultrastructural observation in patients with pelvic congestion syndrome after oviductal ligation. Fallopian tubes of 14 cases were coll... The morphological basis of bilateral lower abdominal pain was studied by means of ultrastructural observation in patients with pelvic congestion syndrome after oviductal ligation. Fallopian tubes of 14 cases were collected during operation. Of them, 10 patients suffered from pelvic congestion syndrome, 4 cases were normal used as control, the 8 small segments from the tubal isthmus were removed during ligation. The essential changes of the fallopian tubes in patients with this syndrome were the marked swelling of the C-type unmyelinated nerve fibers, the decrease in density of axoplasm and in number of microtubules and microfilaments. The Schwann's cells were swollen as well. Furthermore, the mitochondria revealed mild to moderate swelling, their cristae decreased and shortened. However, the changes of the endings of efferent nerve fibers were not obvious.The ultrastructural changes of C-type unmyelinated nerve fibers except the endings of efferent nerve fibers were closely related to the bilateral lower abdominal pain in patients with this syndrome. 展开更多
关键词 Ultrastructure of nerve fibers Fallopian tube Pelvic congestion syndrome Oviductal ligation
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Magnetic Properties of Diluted Magnetic Semiconductor Zn1-xMnxO Nanowires
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作者 常永勤 徐向宇 +2 位作者 罗旭辉 龙毅 叶荣昌 《Chinese Physics Letters》 SCIE CAS CSCD 2005年第4期991-994,共4页
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Two different illites in Luochuan loess, Northern Shaanxi Province 被引量:6
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作者 CHENLi ZHANGLifei +3 位作者 WANGHejin ZHOULiping CHENJing YUANBaoyin 《Chinese Science Bulletin》 SCIE EI CAS 2005年第1期82-87,共6页
Two different illites in samples from S0 to L10 loess-paleosol sequence at Heimugou section in Luochuan are identified by decomposition of X-ray diffraction (XRD) curve, transmission electronic microscopy (TEM) and en... Two different illites in samples from S0 to L10 loess-paleosol sequence at Heimugou section in Luochuan are identified by decomposition of X-ray diffraction (XRD) curve, transmission electronic microscopy (TEM) and energy dis- persive X-ray detector (EDX) analyses. Type I illite displays relatively poor crystallinity, wide and blunt XRD peaks, the highest content of which in <2 μm clay minerals is up to 55%. Type II 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 inAl3+. 展开更多
关键词 伊利石 黄土 陕西 能量分散X射线探测 X射线衍射分析 转换电子显微镜 粘土矿物
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Coating thick MgB_(2) layer on stainless steel substrate 被引量:5
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作者 CHENChinping FENGQingrong +12 位作者 GANZizhao XlONGGuangcheng XUJun LIUYufei KONGLingwen LILin JIAZhang GUOJingpu ZHUANGChenggang DINGLili CHENLiping LIFen ZHANGKaicheng 《Chinese Science Bulletin》 SCIE EI CAS 2005年第7期719-720,共2页
关键词 硼化镁 不锈钢 超传导现象 合金 MRI-CT系统
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