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| 1 | Role of Water in Deformed Omphacite in UHP Eclogite from the Dabie Mountains,Eastern China显示文摘Omphacite grains from UHP eclogite of the Dabie Mountains in eastern China are elongated and showstrong lattice preferred orientations (LPOs). Observations by the transmission electron microscopy (TEM) identified notonly structures of plastic deformation occurring as free dislocation, dislocation loops and dislocation walls, but alsobubbles of water present in the deformed omphacite. The bubbles attach to the dislocation loops which are often connectedto one another via a common bubble. Using infrared spectroscopy (IR), two types of hydrous components are identified ashydroxyl and free-water in the omphacite. An analysis of deformation mechanism of microstructure in omphacite suggeststhat the mineral deformed plastically under UHP metamorphic conditions by dislocation creep through hydrolitic weakening. | SUWen YOUZhendong CONGBolin YEKai | 2003 | Acta Geologica Sinica(English Edition)2003，77，3： | 5 |
| 2 | 大别山双河地区超高压变质岩矿物超微构造的HRTEM研究显示文摘报道了大别山双河地区超高压榴辉岩和硬玉石英岩矿物超微构造及缺陷结构的高分辨透射电镜研究结果。在天然变形绿辉石晶内的自由位错、位错倾斜壁、位错环、位错网、亚晶界、堆垛层错等亚构造中 ,发现了纳米级水分子团 ,这种球形状水分子团包体的存在是导致绿辉石晶体水解弱化和塑性变形的重要因素。在榴辉岩矿物中广泛发育的层错、(10 0 )变形双晶、晶畴结构、界面与晶面的交叉滑移、晶格畸变等变形构造及缺陷结构 ,指示超高压岩石经历了快速折返。在硬玉单晶大约 5 0 0nm的微晶畴内 ,发现了C2 /c和P2 1/n两种结构 ,C2 /c结构的晶体学参数对应于硬玉 ,而P2 1/n结构的晶体学参数对应于绿辉石 ,纳米级P2 1/n出溶结构的存在 ,表明在退变质过程中 ,硬玉在纳米尺度上部分转变为绿辉石 ,并且未能达到平衡。也说明在主体岩石的抬升过程中 ,硬玉晶体伴随有复杂的非平衡退变质作用。对于大别山超高压变质岩的p T轨迹描述及其构造解释具有重要意义。 | 吴秀玲 孟大维 韩郁菁 | 2004 | 地学前缘2004，11，4： | 4 |
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