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OCCURRENCE AND CHEMICAL COMPOSITION OF ZIRCONOLITE (CaZrTi_2O_n)

机译:锆钛矿(CaZrTi_2O_n)的出现和化学组成

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摘要

Zirconolite, ideally CaZrTi_2O_7, is a rare accessory mineral crystallising under different geological conditions and in a wide range of generally SiO_2-poor rock types. It has been observed in: kimberlite; ultrabasic rocks, including metasomatized mantle rocks; anorthosite; dolerite; gabbroic rocks; dioritic rocks (diorite-monzodiorite-granodiorite); syenite and nepheline syenite; sanidinite; carbonatite; metasomatic and metamorphic rocks; and placer deposits. It also occurs in lunar samples, where it has been found in basalts, feldspathic peridotite, lithic fragments, granite, and metamorphosed breccia. Moreover, zirconolite has been reported as a phase in plagioclase-olivine inclusions in the Allende carbonaceous chondrite.
机译:锆石,理想情况下为CaZrTi_2O_7,是一种稀有的辅助矿物,在不同的地质条件下和广泛的贫SiO_2岩石类型中结晶。观察到:金伯利岩;超基性岩石,包括交代的地幔岩石;花岗石白云石辉长岩闪长岩(闪长岩-单闪闪岩-闪长闪闪岩);正长岩和霞石正长岩;蛇纹石碳酸盐岩变质岩和变质岩;和砂金。它也发生在月球样品中,在玄武岩,长石橄榄岩,石块碎片,花岗岩和变质角砾岩中都发现了。此外,据报道,锆石为阿连德碳质球粒陨石中斜长石-橄榄石包裹体中的一相。

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