石英边界的碎形分析作为延展率代理用于追踪地球的压力历史
Mehdi Abdolzadeh1, Seyed Rahim Hosseini2, Iraj Rasa3
1Department of Mineral and Ground Water Resources, Faculty of Earth Sciences, Shahid Beheshti University, Tehran, Iran. mehdi.abdolzadeh@gmail.com.
Scientific reports
|February 18, 2026
概括
这项研究使用碎形分析来估计伊朗Chahzar推力区的应变率. 结果显示,比预期的更高的应变率,表明在中层地岩中局部变形.
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
- 变态石器学 变态石器学
背景情况:
- 了解变形岩石的应变速率是重建带构造史的关键.
- 伊朗桑丹杰-西尔贾恩变态区的查扎尔推力区为变形动力学研究提供了理想的环境.
- 石英微结构受到温度,拉伸率和流体含量的影响.
研究的目的:
- 通过石英颗粒边界的碎形分析,估计查扎尔推力区的延展率和评估变形条件.
- 应用盒计数方法来量化再结晶石英粒的碎形维度 (D),作为变形的代理.
- 为了解中层地岩中的应变适应和orogenic系统中的构造过程做出贡献.
主要方法:
- 自然变形岩石的微观结构分析.
- 使用盒式计数方法对石英颗粒边界进行碎形分析.
- 分形维度 (D) 的量化作为变形条件的代理.
主要成果:
- 估计的应变速率范围从10−10.9s−1到10−6.8s−1.
- 这些比率明显高于典型报告的自然菌株比率 (10−1210−15 s−1).
结论:
- 查扎尔推力区表现出一种变形模式,其特点是偶发性或局部性应变强化.
- 这些发现增强了对中层地岩中应变适应的理解.
- 这项研究提供了对全球类似的orogenic系统中构造过程的见解.
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