The feldspars in shoshonite series volcanic rocks from Shengyuan Basin, Jiangxi Province, show typical mineral characteristics, such as plagioclase phenocryst with reversed zoning texture and replacement-edulcoration rim texture, abundant plagioclase microcrystal in groundmass, and the electron-microprobe analysis shows K-feldspar rims around the plagioclase microcrystal, which is an evidence identifying the rocks to be the shoshonite series. By studying the characteristics of feldspar mineral assemblage, the genesis and physico-chemical conditions in the formation of shoshonite series volcanic rocks are discussed.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址:北京市海淀区学院路29号 邮编:100083 电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700 |