摘要
通过对黄陵地区孔兹岩系构造背景、岩石化学、微量稀土、变质矿物组合、岩石微相特征研究,初步勾画出晋宁期造山运动与黄陵孔兹岩系变质演化历程。明确黄陵地区孔兹岩系为一套变质的富铝质沉积岩组合,在晋宁期造山运动期间该套岩系经历四期变质作用。为今后黄陵地区孔兹岩系研究提供重要参考。
Based on the study of the structure background of Khondalite, geochemistry, REE and micro-elements, metamorphic paragnetic association minerals, and the micro-characteristics of rock, the author sketches the evolvement history of Jinning movement and the metamorphism Khondalite lithology in Huangling area. The khondalite lithology is composed of a suit of metamorphic aluminium-sedimentary rock. During the Jinning movement, the sedmentary rock experienced four stages of metamorphism. The result will provide an important evidence for the study of Khodalite lithology in the future.
出处
《资源环境与工程》
2007年第3期226-231,共6页
Resources Environment & Engineering