A new occurrence of extremely rare Ferro-Chloro-Pargasite in Tudor, Ontario
A new occurrence of extremely rare Ferro-Chloro-Pargasite in Tudor, Ontario
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DOI：
10.1007/s00531-017-1492-7
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发表时间：
2017-06
影响因子：
2.3
通讯作者：
E. Duesterhoeft;P. Raase;Philipp Gremler
中科院分区：
文献类型：
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作者：
E. Duesterhoeft;P. Raase;Philipp Gremler
富氯角闪石是交代岩石呈蓝色的原因。在薄片中（图2），铁氯硼镁石因其独特的多色性而引人注目，从深蓝色（γ）到灰紫色或灰绿色（β）到浅黄色（α）。特别是深蓝色是常见氯闪石的典型特征
The Cl-rich amphibole is responsible for the bluish color of the metasomatized rocks. In thin section (Fig. 2), ferro-chloro-pargasite attracts attention by its unique pleochroism, ranging from deep blue (γ) to gray–violet or gray–green (β) to pale yellow (α). Especially, the deep blue color is a typical feature of common chloro-amphiboles