期刊
JOURNAL OF RAMAN SPECTROSCOPY
卷 49, 期 2, 页码 279-286出版社
WILEY
DOI: 10.1002/jrs.5277
关键词
microscopy; Raman; serpentine; serpentinite; ultramafic
类别
资金
- Marsden Fund Council [UOO1417]
- Dodd-Walls Centre
- Otago Centre for Electron Microscopy
Submicron Raman spectroscopy mapping is able to unambiguously distinguish the main serpentine minerals within their in situ microstructural context. The high spatial resolution (similar to 370nm), large-area coverage (up to hundreds of micrometres in each dimension), and ability to map directly on polished thin sections allows novel interpretations to be made regarding the nature and evolution of serpentinite fault rock textures. The potential of this method is illustrated by examining submicron-scale textures of scaly serpentinites (e.g., dissolution seams, mineral growth in pressure shadows, distribution, and intergrowth of serpentine minerals) from a lithospheric-scale shear zone in New Zealand and a subduction-related serpentinite body in California, USA.
作者
我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。
推荐
暂无数据