桂林理工大学学报2012，Vol.32Issue(1)：36-42,7.DOI:10.3969/j.issn.1674-9057.2012.01.005
台湾软玉的矿物成分、显微结构特征及形成世代
Mineral Composition, Microstructure Characteristics and Generation of Taiwan Nephrite
摘要
Abstract
The nephrite samples from Hualien Fengtien nephrite belt of Taiwan are studied by Fourier transform infrared absorption spectra and XRD, indicating that the nephrite samples are mainly composed of tremolite. The major absorption frequencies of the samples appear around 940 -1 105 cm-1, 650 -760 cm-1, 460 -510 cm-1 and 3 670 cm-1, and the main X-ray spectrogram are 0. 844 3 -0. 845 8 nm( 110) , 0. 271 1 -0. 271 5 nm(151) , 0. 313 1.-0. 313 5 nm(310) and 0. 328 3 -0. 328 6 nm (240).The microstructures of nephrite are felt-like blastic texture, columnar blastic texture, bundle-like blastic texture and parallel fibroblastic texture. The tremolite went through four different generations. The first is coarse columnar. The second is fine columnar, interspersed among the first generation. The third is felt-like aggregate. The fourth is parallel fiber-shaped, formed in last stage.关键词
软玉/透闪石/显微结构/世代/台湾Key words
nephrite/ tremolite/ microstructure/ generation/ Taiwan分类
天文与地球科学引用本文复制引用
任戍明,张良钜,张杰..台湾软玉的矿物成分、显微结构特征及形成世代[J].桂林理工大学学报,2012,32(1):36-42,7.基金项目
国家自然科学基金项目(40572026) （40572026）
广西研究生教育创新计划项目(2010105960709M28) （2010105960709M28）
