摘要
Abstract
This study comprehensively analyzed the basic gemological characteristics,X-ray fluorescence spectros-copy(XRF),infrared spectroscopy,Raman spectroscopy,and other aspects of green apophyllite samples with dif-ferent tones in the Huanggangliang area of Inner Mongolia,and systematically explored the chemical composition and spectral characteristics of green apophyllites samples with different tones.Through high-pressure X-ray diffrac-tion(HPXRD)spectroscopy testing,the crystal structure characteristics of the mineral under high-pressure environ-ment were analyzed in depth,providing key clues for revealing the stable depth of existence of apophyllites after subduction into the crust during geological movement.The research results indicate that the apophyllites in the Huanggangliang area of Inner Mongolia belong to fluorine apophyllites,the content of Fe3+and crystalline water ex-ert a significant influence on the intensity of the green color in apophyllites.In the HPXRD experiment,as the pressure increases,the axial length and cell volume of apophyllites gradually decrease,especially the compression rate of the c-axis is higher than that of the a-axis.At the pressure nodes of 9.0 GPa and 15.3 GPa,a sudden change in compression rate was observed,accompanied by the emergence of new diffraction peaks and the splitting and disappearance of old diffraction peaks.This discovery reveals two distinct phase transitions of apophyllites crys-tals in high-pressure environments.This study provides strong scientific basis for identifying apophyllites and searching for mineral resources,and also provides a new perspective and understanding for further research on apophyllites in the field of geology.关键词
鱼眼石/内蒙古黄岗梁/化学成分/晶体结构/谱学分析Key words
apophyllite/Huanggangliang in Inner Mongolia/chemical composition/crystal structure/spectral analysis分类
天文与地球科学
