This paper discusses the meeting of Qalq-a and Oirad nobilities in 1640 and tries to reveal convener and locale of the meeting, as well as purpose of the meeting.
本文探讨了1640年喀尔喀—卫拉特两部会盟的召集人、地点和目的等问题,指出,《1640年喀尔喀—卫拉特法典》的序文、《咱雅班第达传》和清代档案史籍提供的信息证明,喀尔喀部扎萨克图汗召集了这次会盟,会盟是在其领地内举行的,主要目的是抵御来自清的军事威胁。
The Ascalt beryllium deposit in the dome of the altered granite consists of the medi um- and coarse-grained graphic Pegmatite zone, pegmatite zone of greisenization, lepidolitequartz texture zone, albite-quartz-muscovite texture zone, quartz-muscovite-beryl texture zone,and massive quartz core.
阿斯喀尔特原生绿柱石(Be)矿床是─产于蚀变花岗岩体顶部、属高温气成热液成因的伟晶岩型稀有金属矿床,它主要由中、粗粒似文象伟晶岩带、鲤云母-萤石结构带、条带状钠长石-石英-白云母结构带、石英-白云母-绿柱石结构带,石英核共5个内部结构带组成。