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首页> 外文期刊>Mineralogical Magazine >Jahnsite—whiteite solid solutions and associated minerals in the phosphate pegmatite at Hagendorf-Sud, Bavaria, Germany
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Jahnsite—whiteite solid solutions and associated minerals in the phosphate pegmatite at Hagendorf-Sud, Bavaria, Germany

机译:Jahnsite-德国巴伐利亚州哈根多夫-苏德的磷酸盐伟晶岩中的白铁矿固溶体和相关矿物

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摘要

Secondary phosphate assemblages from the Hagendorf Sud granitic pegmatite, containing the new Mn-Al phosphate mineral, nordgauite, have been characterized using scanning electron microscopy and electron microprobe analysis. Nordgauite nodules enclose crystals of the jahnsite—whiteite group of minerals, showing pronounced compositional zoning, spanning the full range of Fe/Al ratios between jahnsite and whiteite. The whiteite-rich members are F-bearing, whereas the jahnsite-rich members contain no F. Associated minerals include sphalerite, apatite, parascholzite, zwieselite-triplite solid solutions and a kingsmountite-related mineral. The average compositions of whiteite and jahnsite from different zoned regions correspond to jahnsite-(CaMnMn), whiteite-(CaMnMn) and the previously undescribed whiteite-(CaMnFe) end-members. Mo-Kα CCD intensity data were collected on a twinned crystal of the (CaMnMn)-dominant whiteite and refined in P2/a to wR_(obs) = 0.064 for 1015 observed reflections.
机译:Hagendorf Sud花岗岩伟晶岩的二次磷酸盐组合,包含新的Mn-Al磷酸盐矿物,水铝镁矿,已通过扫描电子显微镜和电子探针分析进行了表征。褐铁矿结节包裹了镁铁矿-白铁矿类矿物的晶体,显示出明显的成分分区,横跨铁锰铁矿和白铁矿之间的铁/铝比的整个范围。富含白铁矿的成员含F,而富含铁矾石的成员不含F。伴生矿物包括闪锌矿,磷灰石,钙锌矿,水滑石-三石固溶体和与金山石有关的矿物。来自不同区域的白铁矿和镁铁矿的平均组成分别对应于镁铁矿-(CaMnMn),白铁矿-(CaMnMn)和先前未描述的白铁矿-(CaMnFe)端基。 Mo-KαCCD强度数据收集在(CaMnMn)占优势的白铁矿的孪晶上,并以P2 / a精炼至wR_(obs)= 0.064,可观察到1015个反射。

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