Heuser D, Dubosq R, Petrishcheva E, Bian G, Rentenberger C, Lengauer C L, Gault B, Habler G, Abart R
Department of Lithospheric Research, University of Vienna, Vienna, Austria.
Department Microstructure Physics and Alloy Design, Max Plank Institut für Eisenforschung GmbH, Düsseldorf, Germany.
Contrib Mineral Petrol. 2024;179(6):68. doi: 10.1007/s00410-024-02150-z. Epub 2024 Jun 6.
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.
The online version contains supplementary material available at 10.1007/s00410-024-02150-z.
在温度高于约600℃时,碱性长石在钠长石和钾长石端元之间形成连续固溶体。随着温度降低,出现混溶间隙,中间成分的碱性长石会出溶,形成相对富钠和富钾薄片的交生体。在出溶过程中,晶体结构通常在薄片界面处保持连贯,这一特征可能在地质时期得以保留。由于晶格参数与成分有关,连贯交生要求薄片产生弹性应变。相关的弹性应变能会抵消出溶作用,界定连贯交生混溶间隙的溶线低于无应变相平衡的溶线。为了确定连贯溶线,将中间成分的均质宝石级碱性长石在相图的两相区域条件下进行退火。由此产生了宽度约为10 - 20纳米的连贯交生薄片。用原子探针断层扫描确定薄片成分,从而确定连贯溶线上的点。同时,使用一个热力学混合模型计算连贯溶线,该模型以与出溶实验所用相同的碱性长石为基础进行校准,并考虑了与连贯薄片交生相关的弹性应变能。实验测定的连贯溶线与计算结果高度吻合,表明碱性长石连贯薄片交生中的相平衡得到了充分描述,为解释连贯出溶碱性长石中的相关系提供了坚实基础。
在线版本包含可在10.1007/s00410 - 024 - 02150 - z获取的补充材料。