概括
挪威的伪太基石 在挪威.
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
- 石化学 石化学是一门学科.
背景情况:
- 伪太基石通常是由地震断层过程中摩擦融化而形成的.
- 它们在伯根弧度的出现为深层地过程提供了洞察力.
研究的目的:
- 调查贝尔根弧线中伪太基石形成的起源和条件.
- 了解生态化在伪甲基质生成中的作用.
主要方法:
- 伪太基利特微岩的岩石分析 (安法,石榴石,石,石英).
- 热力学建模以确定稳定的矿物质组合和P-T条件.
主要成果:
- 伪太基石含有生态石面矿物质,表明在~800°C和18-19 kbar (深度>60公里) 形成.
- 这些岩石在格伦维尔的颗粒物中发现,这些颗粒物在卡莱多尼亚的orogeny过程中经历了液体诱导的生态化.
- 生态化使宿主岩石的体积减少了10%左右.
结论:
- 伪基石很可能是由于流体诱导的生态化导致的快速应激放松而形成的.
- 这项研究表明,地深层流体活动,相位转换和地震断层之间存在联系.
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