在无形SiO2中的石英多孔性在花岩切割带的花岩切割带
Jacques Précigout1, Cécile Prigent2, Gina McGill3
1Institut des Sciences de la Terre d'Orléans (ISTO), Univ. Orléans, CNRS, BRGM, UMR7327, Orléans, France. jacques.precigout@univ-orleans.fr.
Scientific reports
|February 1, 2026
概括
地球地的变形在富含石英的岩石中产生了微观的孔隙. 这些孔由无形二氧化连接在一起,在岩石变形过程中由缩应力和流体溶解形成.
科学领域:
- 地质地质地质地质地质地
- 构造学 构造学 构造学 构造学
- 材料科学 材料科学 材料科学
背景情况:
- 石英丰富的岩石中的多孔性在变态大陆地中很常见.
- 角形,金字塔形孔的起源以及它们在岩石变形中的作用尚不清楚.
研究的目的:
- 研究塑性变形石英聚合物的孔隙形成机制.
- 澄清花岩剪切带中变形,多孔性和无形之间的关系.
主要方法:
- 电子显微镜 (SEM和TEM) 从花岩剪切带中变形的石英.
- 孔隙分布,形状和相互连接的分析.
- 测量脱位密度和评估残余应力.
主要成果:
- 在颗粒边界和石英基结构内观察到的孔隙.
- 通过无形的二氧化 (SiO2) 层,孔隙的相互连接.
- 脱位密度低于预测,表明剩余应力和部分无形化.
结论:
- 孔隙形成与应力度和流体溶解成机械无形石英有关.
- 质疑现有的关于粘性变形过程中的毛孔产生假设.
- 支持压力诱导的无形化作为石质层岩石变形的关键过程.
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