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扬子地台西缘江浪变质核杂岩结构及对成矿的控制 被引量:61
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作者 傅昭仁 宋鸿林 颜丹平 《地质学报》 EI CAS CSCD 北大核心 1997年第2期113-122,共10页
扬子地台西缘江浪变质核杂岩体的基本结构,划分为堆垛层、褶叠层及板岩带等三个构造地层系统,其间为构造滑脱面所分割,在该类变质核杂岩体中发育有一个中间流变层。本文建立了堆垛层的新概念,认为它是造山带中深部地壳常见的基本构造型... 扬子地台西缘江浪变质核杂岩体的基本结构,划分为堆垛层、褶叠层及板岩带等三个构造地层系统,其间为构造滑脱面所分割,在该类变质核杂岩体中发育有一个中间流变层。本文建立了堆垛层的新概念,认为它是造山带中深部地壳常见的基本构造型式。同时,阐述了该变质核杂岩体中铜矿的构造空间配置及构造过程对成矿作用的控制,建立了该杂岩体内铜矿的成穹-成矿模式,认为川西雅碧江流域地区有较好的找矿远景。 展开更多
关键词 变持核 杂岩结构 铜矿床 成矿 层控矿床
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Research on characters of surrounding rock in complex geology conditions and supporting time 被引量:9
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作者 Yu Weijian Gao Qian +1 位作者 Zhai Shuhua Zhang Meihua 《Engineering Sciences》 EI 2008年第2期91-96,共6页
The methods combined by test, field monitoring and theoretical analysis were adopted to do the systemic research on the rock mass from micro-structure to macro-deformation, and rheological model of Jinchuan rock mass ... The methods combined by test, field monitoring and theoretical analysis were adopted to do the systemic research on the rock mass from micro-structure to macro-deformation, and rheological model of Jinchuan rock mass was established to discuss the reasonable supporting time. Resuhs show that supporting after suitable stress and displacement release can benefit for the long-term stability of surrounding rock. 展开更多
关键词 complex geological conditions surrounding rock characteristic test supporting time theological characteristic
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Micro Structural Development of in Situ Heated and Deformed Pure and Silica Gel-Doped Polycrystalline Halite Using High Energy Synchrotron Radiation
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作者 Caterina E. Tommaseo 《Journal of Earth Science and Engineering》 2015年第1期27-43,共17页
This paper presents an experimental investigation of the microstructural development upon in situ compression and heating of pure and SiO2 gel-doped (5 wt%) polycrystalline halite, with grain sizes ranging from 45 ... This paper presents an experimental investigation of the microstructural development upon in situ compression and heating of pure and SiO2 gel-doped (5 wt%) polycrystalline halite, with grain sizes ranging from 45 μm to 〉70 μm (cold pressed at 200 MPa and heated at 150 ℃ for one week), using high energy synchrotron x-ray radiation. Texture development of the samples was studied at room temperature, 100, 200 and 300 ℃. At each temperature, the samples were axially compressed keeping the load constant at every -500 N step up to the maximum 2,400 N (- 48 MPa). At the different loads and temperatures, 2D images and load/elongation curves were recorded in situ to get information about the texture development and the rheological behaviour of the potycrystalline halite samples. At high stresses, the doped halite samples show an increase in the elastic moduli and in the microstrain The results were confirmed by the single grain orientation analyses using the FABLE program, where a sharpening of the texture was observed. 展开更多
关键词 Polycrystalline halite in situ experiments microstructural development silica gel.
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