According to the mineralogy, petrology and isotope geochemistry of the lamprophyre and granite inclusions, it is suggested that there is a concealed intrusive mass in Xikuangshan; themica-plagioclase lamprophyre intruded after granite intrusion.
湖南锡矿山地区云斜煌斑岩是属碱钙性系列的基性岩脉,其在上侵时捕获了石灰岩包体而发生局部同化混杂,致使煌斑岩褪色蚀变。
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