Iridescent plagioclase in Peristerite area is albite oligoclase;Iridescent plagioclase in B φ ggild area is andesine labradorite.
在晕连生区产生晕彩的为钠奥,在沃基尔德连生区产生晕彩的为中拉。
Iridescent plagioclase in Peristerite area is albite oligoclase;Iridescent plagioclase in B φ ggild area is andesine labradorite.
在晕连生区产生晕彩的为钠奥,在沃基尔德连生区产生晕彩的为中拉。
Many diorite porphyrite and albite aplite dikes are found in the gold district and its surrounding areas.
晚期在浅部为风化淋富集成矿。
The association of albite-bearing silicolites, phyllite and limestone seems to be an important prospecting indicator.
含钠硅质岩、千枚岩、灰岩合是找矿评价的重要标志。
The albite component increases while anorthic component decreases in detrital plagioclase.The plagioclase turned into an end - member component of albite.
碎屑中钠分逐渐增多,钙分逐渐减少,最终形成纯钠端元的钠。
Albite and labradorite both belong to plagioclase series, but they are the two different varieties.According to the characters of inclusion and transparency, iridescent ...
晕彩钠和晕彩拉都属系列,但却是两个不同的宝品种。
Mineral constituents consist mainly of jadeite, aegirine-augite, magnesio-riebeckite, winchite, magnesio-hornblende, actinolite, quartz, albite, rutile and sphene.
主要成矿物为硬玉、霓辉、镁纳闪、蓝透闪、镁角闪、阳起、英、钠、金红和榍。
Paragenetic association II include illite、albite、dissolved authigenetic quarze and kaolinite、dolomite、ankerite and ferrocalcite, the paragenetic association formed alkali environment;
成岩共生合II由自生伊利、自生钠、自生英与高岭溶解、白云、铁白云、铁方解成,该合形成于碱性成岩环境;
The feldspar group contains tectosilicate minerals with similar properties, including orthoclase, albite and labradorite. Feldspars make up more than 60% of the upper crust of the earth.
系列包含网状矽酸盐的矿物并且有相似的属性,包括正,钠以及拉.构成了60%的上层地壳.
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