Mineralogy of the deposit of albitized granites Kanarata, Sakar Мountain, Southеastern Bulgaria

IF 0.2 Q4 GEOSCIENCES, MULTIDISCIPLINARY
Y. Yanev
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引用次数: 0

Abstract

The Kanarata albitized granite deposit is located on the NE periphery of the Sakar Upper Carboniferous granite batholith, immediately adjacent to its contact with the metamorphic framework. The porphyroid two-mica granites of the batholith are replaced by albite and quartz, and by magnesium-rich minerals in small amounts (some enriched in sodium): Mg-actinolite to Mg-hornblende and Mg-tremolite, phlogopite, chlorite, talc, saponite, as well as accessory rutile, probably titanite and apatite. The only relict mineral is zircon. The newly formed minerals are products of alkaline (magnesium-sodium) metasomatosis of possibly Alpine age. This has led to a change in the chemical composition of the granite, resulting in a decrease in the amount of silicon, iron, calcium, and especially potassium, and an increase in the amount of titanium, aluminum, magnesium, and especially sodium.
保加利亚东南部萨卡尔Мountain Kanarata钠质花岗岩矿床的矿物学
卡纳拉塔钠质花岗岩矿床位于萨卡尔上石炭统花岗岩岩基的东北边缘,紧邻其与变质框架的接触面。岩基的斑状二云母花岗岩被钠长石和石英以及少量富含镁的矿物(一些富含钠)所取代:镁阳起石至镁角闪石和镁透闪石、金云母、绿泥石、滑石、皂石,以及副金红石,可能是钛矿和磷灰石。唯一残留的矿物是锆石。新形成的矿物是可能是阿尔卑斯时代的碱性(镁钠)交代作用的产物。这导致花岗岩的化学成分发生变化,导致硅、铁、钙,尤其是钾的含量减少,钛、铝、镁,尤其是钠的含量增加。
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