矿石为花岗伟晶结构，似文象结构和块状、条带状构造。
Ores are of pegmatite granites texture, graphic and massive, banded structure.
勾勒去令人惊异的不对称的条带和半透明的晶体构造。
The blue draws out the amazing asymmetrical banding and translucent crystal formations.
条带（条纹）状和豆鲕状构造是本矿床的主要矿石构造。
The major ores of this deposit have a banded(streaky), pisolitic or oolitic structure.
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