首页> 外文期刊>Neues Jahrbuch fur Mineralogie, Abhandlungen >Ferronigerite with dominant substitution Ti Sn_(-1) in muscovite+chlorite aggregate from massive quartz nodule associated with a petalite-rich aplite-pegmatite of the Barroso-AIvao pegmatite field, Northern Portugal
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Ferronigerite with dominant substitution Ti Sn_(-1) in muscovite+chlorite aggregate from massive quartz nodule associated with a petalite-rich aplite-pegmatite of the Barroso-AIvao pegmatite field, Northern Portugal

机译:葡萄牙北部Barroso-AIvao伟晶岩田富白云母-辉绿岩伴生的块状石英结核中白云母+绿泥石聚集体中具有主要取代Ti Sn _(-1)的铁镍铁矿

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摘要

Zoned to homogeneous, euhedral to subhedral tabular crystals (up to ~ 100 um in size) of feiTonigerite-6N6S 'ferro- nigerite-2N1S with Ti-enriched core occur in fine-grained muscovite+chlorite aggregate from a quartz nodule enclosed in a mica schist host. The quartz nodule is located close to the petalite-rich aplite-pegmatite dike Lousas from the Barroso-Alvao pegmatite field. Ferronigerite-6N6S exhibits dominant substitution TiSn ,, Sn/(Sn+Ti) = 0.99-0.61 and Fe > Zn > Mg > Mn. Normalization to 66 cations yielded SUM Sn+Ti from 5.94 apfu in Ti-rich to 6.64 apfu in Sn-rich compositions and high SUM negative charges 190.43 and 191.95; normalization to 186 negative charges gave SUM Sn+Ti 5.80-6.43 and low SUM cations = 63.96-64.46, respectively. Calculation of Li by normalization to 66 cations and 192 negative charges (OH = 6) yielded SUM Sn+Ti = 5.73-6.21 apfu and SUM oxides = 99.20-100.86. These data are closest to the ideal formula of ferronigerite-6N6S although calculated Li contents of 0.88 to 1.12 wt. percent Li_2O (2.35-3.12 apfu) seem to be too high. The quartz nodule consists of an aggregate of zoned tourmaline, medium-grained aggregate of muscovite and fine-grained aggregate of muscovite+chlorite (likely a pseudomorph after cordierite-sekaninaite). This finegrained aggregate contains accessory ferronigerite, fluorapatite, paragonite, beryl, staurolite, and rutile with rare small grains (< 1 mu m) of Fe, Mn, Y, Nb, Ta, and Ti-oxides. The studied assemblage represents a new paragenetic type of nigerite showing obvious peraluminous signature, high amount of Fe and Mg along with close relationship to a highly evolved granitic rock. The geochemi-cal signature of this assemblage indicates influx of highly evolved fluids enriched in F, P, B, Sn, Zn, Be, Nb, Ta and potentially Li into the quartz nodule.
机译:feiTonigerite-6N6S 具有富钛核的铁镍铁矿-2N1S分布于细粒白云母+亚氯酸盐聚集体中,形成均质,从正方到亚面形的片状晶体(尺寸最大〜100 um)云母片岩宿主。石英结核位于靠近Barroso-Alvao伟晶岩田的富花瓣的磷灰石-透辉石岩卢萨斯堤上。铁镍铁矿-6N6S表现出主要取代TiSn,Sn /(Sn + Ti)= 0.99-0.61,且Fe> Zn> Mg> Mn。标准化为66个阳离子后,SUM Sn + Ti从富含Ti的5.94 apfu变为富含Sn的6.64 apfu,并具有高SUM负电荷190.43和191.95;归一化为186个负电荷分别得到SUM Sn + Ti 5.80-6.43和低SUM阳离子= 63.96-64.46。通过归一化为66个阳离子和192个负电荷(OH = 6)计算Li,得出SUM Sn + Ti = 5.73-6.21 apfu,SUM氧化物= 99.20-100.86。尽管计算出的Li含量为0.88至1.12wt。%,但这些数据最接近于理想的铁镍铁矿-6N6S的分子式。 Li_2O(2.35-3.12 apfu)百分比似乎太高。石英结核由带状电气石的聚集体,白云母的中粒聚集体和白云母+亚氯酸盐的细粒聚集体组成(可能是堇青石-闪锌矿之后的假晶型)。这种细粒状骨料含有副铁镍矿,氟磷灰石,方钠石,绿柱石,十字沸石和金红石,并具有罕见的小颗粒(<1微米)的铁,锰,钇,铌,钽和钛氧化物。所研究的组合物代表一种新型的黑闪石共生类型,其显示出明显的高铝特征,高含量的铁和镁以及与高度演化的花岗岩的密切关系。该组合的地球化学特征表明,富含F,P,B,Sn,Zn,Be,Nb,Ta和潜在的Li的高度演化的流体涌入石英结核。

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