首页> 外文期刊>THE CANADIAN MINERALOGIST >THE FIELD OF STABILITY OF BLUE JADEITE: A NEW OCCURRENCE OF JADEITITE AT SORKHAN, IRAN, AS A CASE STUDY
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THE FIELD OF STABILITY OF BLUE JADEITE: A NEW OCCURRENCE OF JADEITITE AT SORKHAN, IRAN, AS A CASE STUDY

机译:蓝硬玉的稳定性研究领域:以伊朗索尔汗为例,发生了一次新的硬玉

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摘要

A new occurrence of "blue jade" is described. The jadeitite occurs as metasomatic veins in magnesite bodies within meta-ultramafic rocks in the Sorkhan area of southeastern Iran. The veins are composed of almost pure jadeite, 90 to 99.5 mol.percent Jd, contain minor amounts of Ba-bearing K-feldspar, lawsonite and katophoritic amphibole, but unlike other occurrences of "blue" or "lavender jade", do not contain high amounts of Ti. The jadeitite veins formed at low-temperature - high-pressure conditions, around 1.6 GPa and 420 deg C. Such P-T conditions are characteristic of zones of cold subduction in which lawsonite blueschists to lawsonite eclogites typically form. Thermodynamic studies show that the mineral assemblage within the blue jade is strongly pressure- and temperature-dependent. Jadeitites containing two clinopyroxenes (jadeite and omphacite) are stable at high pres-sure (>=0.8 GPa) and low temperature (<=430 deg C) conditions, whereas blue jade with only one clinopyroxene (jadeite) forms at higher temperature or lower pressure. On the basis of these new calculations, P-T conditions of formation are re-examined for all occurrences of blue jade.
机译:描述了新出现的“蓝玉”。翡翠是在伊朗东南部的索尔汗地区的超超镁铁质岩石中的菱镁矿体内以交代静脉的形式存在的。矿脉由几乎纯净的翡翠组成,Jd含量为90至99.5摩尔,含有少量的含Ba钾长石,钙钠石和角闪石闪石,但与其他出现的“蓝色”或“薰衣草玉”不同大量的钛。翡翠矿脉是在低温-高压条件下(约1.6 GPa和420摄氏度)形成的。此类P-T条件是冷俯冲带的特征,在该带中通常形成钙钠榴石蓝晶岩至钙钠榴石榴辉岩。热力学研究表明,蓝玉内部的矿物组合强烈依赖于压力和温度。含有两种斜发辉石(翡翠和绿辉石)的翡翠在高压(> = 0.8 GPa)和低温(<= 430摄氏度)条件下稳定,而仅含一种斜辉石(翡翠)的蓝翡翠在较高温度或更低温度下形成压力。在这些新的计算基础上,针对蓝玉的所有发生情况重新检查了P-T的形成条件。

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