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首页> 外文期刊>Journal of Metamorphic Geology >Calibration of oxygen isotope fractionation and calcite-corundum thermometry in emery at Naxos, Greece
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Calibration of oxygen isotope fractionation and calcite-corundum thermometry in emery at Naxos, Greece

机译:希腊纳克索斯沼泽中氧同位素分馏和方解石 - 刚玉的光学校准

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Corundum (Crn), including sapphire, occurs in emery pods surrounded by marble on the island of Naxos, Greece. The emery formed from bauxite deposited in karst that was metamorphosed to 400-700°C at 20-15 Ma. Many of these rocks initially appeared well suited for refractory accessory mineral (RAM) thermometry, which uses oxygen isotope fractionation between a RAM - corundum - and a modally dominant phase with faster diffusion of oxygen - calcite (Cc) - to determine peak metamorphic temperatures. However, previous attempts at oxygen isotope thermometry were confounded by highly variable fractionations (Δ~(18)O) measured at mm-scale and the uncertain calibration of Δ~(18)O(Cc-Crn) versus temperature. Secondary ion mass spectrometry (SIMS) permits in situ analysis of δ~(18)O in corundum and calcite at the 10-μm scale in adjacent grains where textures suggest peak metamorphic equilibrium was attained. SIMS analyses of adjacent mineral pairs in eight rocks yield values of Δ(Cc-Crn) that systematically decrease from 7.2 to 2.9‰ at higher metamorphic grade. Pairing these data with independent temperature estimates from mineral isograds yields an empirical calibration of 1,000 lnα(Cc-Crn) = 2.72 ± 0.3 × 10~6/T~2 (T in K). The new fractionations (2.7‰ at 1,000 K) are significantly smaller than those calculated from the modified increment method (6.5‰ at 1,000 K; Zheng, Geochimica et Cosmochimica Acta, 1991, 55:2299-2307; Zheng, Mineral Mag, 1994, 58A:1000-1001), which yield unreasonably high temperatures of 630 to 1,140°C when applied to the new Naxos data. The new calibration of Δ(Cc-Crn) can be combined with published fractionations to calculate A-factors for corundum versus a range of 14 other minerals. These new fractionation factors can be used for thermometry or to constrain the genesis of corundum. A compilation of gem corundum δ~(18)O values shows that many igneous sapphires, including important deposits of basalt- associated sapphire, are mildly elevat
机译:Corundum(CRN),包括蓝宝石,发生在希腊纳克索斯岛上的大理​​石包围的沼泽地。由岩石矿沉积在喀斯特的铝土中,在20-15 mA的喀斯特中沉积在400-700°C中。这些岩石中的许多初始出现非常适合耐火材料型矿物(RAM)温度(RAM)温度,其在RAM - 刚玉 - 羟(CC)和改变氧 - 方解石(CC)扩散的模式中的氧同位素分级 - 以确定峰变质温度。然而,以mm级测量的高度可变分馏(δ〜(18)o)和δ〜(18)o(cc-crn)与温度的不确定校准,以前的氧同位素温度的先前尝试。二次离子质谱(SIMS)允许在诸如纹理表明峰变质平衡的相邻颗粒中的10μm刻度下慢率和方解石中δ〜(18)o的δ〜(18)O的原位分析。 SIM在八个岩石中的相邻矿物对分析Δ(CC-CRN)的Δ(CC-CRN)的值,在较高的变质等级下系统地降低了7.2至2.9。将这些数据与来自矿物质的独立温度估计配对产生的经验校准为1,000LNα(CC-CRN)= 2.72±0.3×10〜6 / t〜2(k)。新的分馏(2.7‰以1,000 k)明显小于改性增量方法计算的那些(6.5‰,Zheng,Geochimica Et Cosmochimica Acta,1991,55:2299-2307;郑,矿物Mag,1994, 58A:1000-1001),当应用于新的NAXOS数据时,它产生630至1,140°C的不合理高温。 δ(CC-CRN)的新校准可以与已发表的分馏组合,以计算刚玉的因素,而另外14个其他矿物质。这些新的分馏因子可用于测温或限制刚玉的起源。 Gem Corundumδ〜(18)o值的汇编表明,许多火油蓝宝石,包括玄武岩相关蓝宝石的重要沉积物,是温和的

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