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排序方式: 共有168条查询结果,搜索用时 31 毫秒
81.
Wang Jianghai Guangzhou Institute of New Geological Technology Academia Sini Guangzhou GuangdongYang Wenhua Wu Jinping China U niversity of Geosciences W uhan Hubei Jiang M inxi 《《地质学报》英文版》1995,69(2)
On the basis of the detailed field work, compositions and contents of plagioclase and K - feldspar,determination of ordering degree, statistical analysis of plagioclase elongation index, mass-balance calculation and mineral spatial distribution and geochemistry, it is concluded that the migmatites in the Dabie complex are characterized by the presence of thermocenters. There are regular changes in mineral character in the migmatites from the centers outwards. The dominant genetic mechanism is anatexis and metasomatism, whose intensities decrease from the centers outwards. Finally, according to the simulated experiment on Liesegang' s rings and non-linear dynamics (dissipative structure theory), the dynamic mechanism of migmatization is profoundly expouded as consisting of the early-stage metasomatism induced by the thermal anomaly, the cardinal-stage anatexis induced by the early-stage matasomatism and finally the last-stage post-anatexis metasomatism. 相似文献
82.
There are two aspects in the study of irregular mixed-layer clay minerals: one is the kinds and ratios of their basic structural unit layers and the other is the junction probabilities of the unit layers. Irregular mixed-layer illite/smectite clay minerals (I/S) are widespread in nature. While studying the clay minerals from the Permian-Triassic (P/T) boundary bed, the authors found that I/S clay minerals are developed in all P/T boundary clay layers in areas from the northwest to southeast of China. Systematic mineralogical studies of the I/S clay minerals from Hunan, Hubei, Sichuan and Zhejiang were made by means of X-ray, infrared spectroscopic, electron microscopic and chemical analyses and a deepened study of the stacking sequences of their structural unit layers was conducted by the MacEwan one—dimentional direct Fourier transform. It was found that the stacking of the illite and smectite crystal layers along the c axis can be derived from Fibonacci sequences. Hence, the authors propose that such I/S clay minerals are possessed of two—dimentional crystal lattice and one—dimentional quasicrystal lattice. 相似文献
83.
关于东昆仑地区前寒武纪地质的几点认识 总被引:13,自引:3,他引:13
以1∶25万区域地质调查资料为基础,对东昆仑造山带前寒武纪地质演化的几个关键问题进行了探讨。东昆仑地区3206Ma±14Ma的锆石207Pb/206Pb年龄信息表明,该区存在古太古代基底。代表东昆仑地区基底的"金水口岩群"可以解体为太古宙—古元古代的白沙河岩群和中元古代的小庙岩群,两者是2个不同构造旋回的产物。东昆仑地区万宝沟群的时代应限定在中元古代,而不能延续到新元古代。东昆仑地区的年代构造格架显示,前寒武纪存在3次强烈的区域性构造热事件,分别发生在2400~2500Ma、1800~1900Ma和大约1000Ma。1000Ma左右的聚合事件导致中元古代分隔的不同小陆块的有限裂解小洋盆闭合,陆块聚合形成"西域板块",并可能是整个Rodinia超大陆的组成部分。 相似文献
84.
85.
MAPGIS 为地质图件数字制图提供了现代化的技术手段,可大大提高工作效率,改善工作质量,应用前景广阔。在宜昌市矿产资源规划1:20万地质图件的编制工作中,对在 MAPGIS 环境下绘制大型地质图件的数据准备、流程设计.矢量化、误差校正、拓扑上色、子图库添加等进行了成功的尝试。 相似文献
86.
Characteristics of Element Migration in the Process of Wall-Rock Alteration in the Shibangou Gold Deposit,Western Henan 总被引:2,自引:0,他引:2
WEI Junhao LI Jianwei YUAN Yanbin Faculty of Earth Resources China University of Geosciences Wuhan Hubei 《《地质学报》英文版》1999,73(2):201-207
The Shibangou gold deposit in western Henan is associated with irregular quartz veinlets occurring in altered shear zones dissecting a dioritic intrusion. The altered shear zones are characterized by silicification, pyriti-zation, sericitization, chloritization and K-feldspar alteration. Zoning of altered rocks adjacent to the Au-bearing quartz veins is obviously exhibited. Fine-grained sulphides and quartz veinlets of different ages and small-scale fissures are widely distributed in the central part of the altered zones. Major mineralization types in this gold deposit are Au-bearing quartz vehlets and altered rocks in the shear zones. Samples were collected from drilling cores according to the alteration zoning and mineralization type and all samples were analyzed for major and trace elements. Mass balance, volume change (fv=97.3-71.9%) and major element variation sequences are studied in terms of major elements. The changes of mobile components (SiO2, K.2O, Fe2O3 and CaO) and immobile component (Al2O3 相似文献
87.
WANG Wenkui ZHAO Shanrong LEI Xinrong WU Youcai China University of Geosciences Wuhan Hubei 《《地质学报》英文版》2000,74(2):190-193
The research on morphology of mineral crystals in China includes classical goniometry of 100 minerals such as hsianghualite, orthobrannerite, jamesonite and bertrandite and surface microtopography of 20 minerals such as wolframite and diamond, among which 5 new minerals and 34 uranium minerals were discovered and measured by Chinese mineralogists. These have enriched mineralogy and crystal morphology and strengthened the study of information of morphological genesis. 相似文献
88.
HOU Jianjun LAI Hongyan HUANG Bangqin CHEN Jixin College of Fisheries Huazhong Agricultural University Wuhan China College of Life Sciences Hubei Normal University Huangshi China State Key Laboratory of Marine Environmental Science Environmental Science Research Center Xiamen University Xiamen China Key Laboratory of Freshwater Fish Germplasm Resources Biotechnology Yangtse River Fisheries Research Institute Jinzhou China State Key La... 《海洋学报(英文版)》2009,28(2)
Partial rDNA sequences of Prorocentrum minimum and Takayama pulchella were amplified, cloned and sequenced, and these sequence data were deposited in the GenBank. Eight oligonucleotide probes (DNA probes) were designed based on the sequence analysis. The probes were employed to detect and identify P. minimum and T. pulchella in unialgal and mixed algal samples with a fluorescence in situ hybridization method using flow cytometry. Epifluorescence micrographs showed that these specific probes labeled with flu... 相似文献
89.
DENG Jun HUANG Dinghu WANG Qingfei HOU Zengqian LU Qingtian YAOLingqing XIN Hongbo ZHANG Qiang WEI YanguangKey Laboratory of Lithospheric Tectonics Exploration China University of Geosciences Beijing Ministry of Education Beijing China University of Geosciences Wuhan Hubei Institute of Mineral Resources Chinese Academy of Geological Sciences Beijing 《《地质学报》英文版》2004,78(1):267-272
Almost all intraplate caprocks experienced strong deformation during the convergence of microplates, and then disintegrated into many secondary geologic units with the special characters, such as irregular boundaries and particular structural assemblages. In order to understand the formation mechanism of these special phenomena, a rheological experiment on the structural scenery of the Tongling area is carried out. The result shows that the primary regular and uniform boundaries of the Tongling area becomes irregular because of the enclosing and confinement of surrounding geological units in the process of "compression-shearing-rotation-drag"; simultaneously, two specific "drag depressions" developed at two opposite corners of the block. The former and the later phenomena can be regarded as a typical regional-scale rheological effect and necessary outcome of intraplate deformation respectively. 相似文献
90.
WANG An WANG Guocan LI Dewei XIE Defan LIU Demin Faculty of Earth Sciences China University of Geosciences Wuhan Hubei China State Key Laboratory of Geological Processes Mineral Resources China 《《地质学报》英文版》2009,83(1)
The Hohxil region in the northern Qinghai-Tibet Plateau is occupied by numerous plateau lakes,which have long been inferred as being tectonic products.However,so far little evidence has been found to support this tentative inference.Field survey and morphotectonic analysis of TM satellite images in the eastern segment of the Hohxil region revealed that Kusai Lake and Yelusu Lake are S- shaped pull-apart basins,which were dominated by left strike-slip master faults trending WNW-ESE. The pull-apart distanc... 相似文献