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首页> 外文期刊>Mineralogical Magazine >Micron- to nano-scale intergrowths among members of the cuprobismutite series and paderaite: HRTEM and microanalytical evidence
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Micron- to nano-scale intergrowths among members of the cuprobismutite series and paderaite: HRTEM and microanalytical evidence

机译:铜镁橄榄石系列和红铁矿成员之间的微米至纳米级共生:HRTEM和微观分析证据

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Coherent intergrowths, at the lattice scale, between cuprobismutite (N = 2) and structurally related paderaite along both major axes (ISA and 17 A repeats) of the two minerals are reported within skarn from Ocna de Fier, Romania. The structural subunit, DTD, 3 layers of paderaite, is involved at interfaces of the two minerals along the 15 A repeat, as well as in transposition of 1 paderaite unit to 2 cuprobismutite units along the 17 A repeat in slip defects. Lattice images obtained by HRTEM across intervals of 200--400 nm show short- to long-range stacking sequences of cuprobismutite and paderaite ribbons. Such nanoscale slabs mimic jam-scale intergrowths observed in back-scattered electron images at three orders of magnitude greater. These slabs are compositionally equivalent to intermediaries in the cuprobismutite-paderaite range encountered during microanalysis. Hodrushite (A' = 1.5) is identified in the Jim-scale intergrowths, but its absence in the lattice images indicates that, in this case, formation of polysomes between structurally related phases is favoured instead of stacking disorder among cuprobismutite homologues. The tendency for short-range ordering and semi-periodic occurrence of polysomes suggests they are the result of an oscillatory chemical signal with periodicity varying from one to three repeats of ISA, rather than simple 'accidents' or irregular structural defects. Lead distribution along the polysomes is modelled as an output signal modulated by the periodicity of stacking sequences, with Pb carried within the D units of paderaite. This type of modulator acts as a patterning operator activated by chemical waves with amplitudes that encompass the chemical difference between the minerals. Conversion of the paderaite structural subunit DTD to the C unit of cuprobismutite, conserving interval width, emphasizes that polysomatic modularity also assists interference of chemical signals with opposite amplitudes. Observed coarsening of lattice-scale intergrowths up to the jim-scale implies coupling between diffusion-controlled structural modulation. and rhythmic precipitation at the skarn front during crystallization.
机译:罗马尼亚Ocna de Fier的矽卡岩中报道了沿两种矿物的两个长轴(ISA和17 A重复序列)在铜镁长石(N = 2)和结构相关的红土之间晶格尺度上的连贯共生。结构性亚基DTD,三层铜铁矿,涉及沿15 A重复序列的两种矿物的界面,以及沿滑移缺陷沿1 A重复序列将1个铜铁矿单元转换为2个铜铍锰矿单元。通过HRTEM在200--400 nm的间隔内获得的晶格图像显示了长铜锰铁矿和红土带的短至长距离堆叠序列。这样的纳米级平板模仿了在反向散射电子图像中观察到的果酱级共生现象,其增长了三个数量级。这些平板的成分等同于微量分析过程中遇到的铜镁橄榄石-贝得石范围内的中间体。在吉姆规模的共生体中鉴定出钙铁矿(A'= 1.5),但在晶格图像中不存在钙铁矿,这表明在这种情况下,与结构相关的相之间形成多核小体是有利的,而不是在铜镁榴石同系物之间形成堆积障碍。多核糖体的短程有序和半周期性出现的趋势表明,它们是振荡化学信号的结果,其周期性从ISA的1到3次重复变化,而不是简单的“事故”或不规则的结构缺陷。沿着多核糖体的铅分布被建模为由堆积序列的周期性调制的输出信号,铅在铅铁矿的D单元中携带。这种类型的调制器充当由化学波激活的构图算子,其振幅包含矿物之间的化学差。铜铁矿结构亚基DTD转换为铜铍锰矿的C单元,同时保留了区间宽度,强调了多体模块性还有助于干扰振幅相反的化学信号。观察到的晶格尺度共生的粗化直至吉姆尺度意味着扩散控制的结构调制之间的耦合。结晶过程中,矽卡岩前缘有节律性沉淀。

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