Coherent solvus of disordered alkali feldspar: experiment, atom probe tomography and thermodynamic model

IF 3.5 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
D. Heuser, R. Dubosq, E. Petrishcheva, G. Bian, C. Rentenberger, C. L. Lengauer, B. Gault, G. Habler, R. Abart
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Abstract

At temperatures above about 600 °C, alkali feldspar forms a continuous solid solution between the Na and K end members. Towards lower temperatures a miscibility gap opens, and alkali feldspar of intermediate composition exsolves, forming an intergrowth of relatively more Na-rich and K-rich lamellae. During exsolution, the crystal structure usually remains coherent across the lamellar interfaces, a feature that may be preserved over geological times. Due to the compositional dependence of the lattice parameters, coherent intergrowth requires that the lamellae are elastically strained. The associated elastic strain energy counteracts exsolution, and the solvus delimiting the misciblity gap for coherent intergrowth lies below the solvus for strain free phase equilibria. To determine the coherent solvus, homogeneous gem quality alkali feldspar of intermediate composition was annealed at conditions falling into the two-phase region of the phase diagram. Thereby a coherent intergrowth of approximately 10–20 nanometers wide lamellae was produced. Lamellar compositions were determined with atom probe tomography defining points on the coherent solvus. In parallel, the coherent solvus was calculated using a thermodynamic mixing model calibrated on the same alkali feldspar as used for the exsolution experiments and accounting for the elastic strain energy associated with coherent lamellar intergrwoth. The experimentally determined and the calculated coherent solvus are in excellent agreement indicating that phase equilibria in coherent lamellar intergrowth of alkali feldspar are adequately described, providing a sound basis for the interpretation of phase relations in coherently exsolved alkali feldspar.

Abstract Image

无序碱长石的相干溶解:实验、原子探针断层扫描和热力学模型
在约 600 °C 以上的温度下,碱性长石在 Na 和 K 两端成分之间形成连续的固溶体。在温度较低时,混溶间隙打开,中等成分的碱性长石发生外溶解,形成相对富含更多 Na 和 K 的薄片。在溶解过程中,晶体结构通常在薄片界面上保持一致,这一特征可能会在地质年代中保留下来。由于晶格参数与成分有关,相干互生要求薄片受到弹性应变。相关的弹性应变能抵消了外溶作用,相干互生的混溶隙的溶点低于无应变相平衡的溶点。为了确定相干溶解度,在相图两相区域的条件下对中等成分的均匀优质碱长石进行了退火处理。由此产生了宽约 10-20 纳米的层状相干互生。通过原子探针断层扫描确定了相干溶胶上的点,从而确定了薄片成分。与此同时,利用热力学混合模型对相干溶解度进行了计算,该模型在用于外溶解实验的相同碱性长石上进行了校准,并考虑到了与相干薄片互生有关的弹性应变能。实验得出的相干溶解度与计算得出的相干溶解度非常吻合,表明相干片层间生长的碱长石的相平衡得到了充分的描述,为解释相干外溶解碱长石的相关系提供了坚实的基础。
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来源期刊
Contributions to Mineralogy and Petrology
Contributions to Mineralogy and Petrology 地学-地球化学与地球物理
CiteScore
6.50
自引率
5.70%
发文量
94
审稿时长
1.7 months
期刊介绍: Contributions to Mineralogy and Petrology is an international journal that accepts high quality research papers in the fields of igneous and metamorphic petrology, geochemistry and mineralogy. Topics of interest include: major element, trace element and isotope geochemistry, geochronology, experimental petrology, igneous and metamorphic petrology, mineralogy, major and trace element mineral chemistry and thermodynamic modeling of petrologic and geochemical processes.
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