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.
结果表明：矿石以鲕状构造为主，具有典型的同心环带结构。
The research results showed that the main ore structure is oolitic with a typical band structure of concentric rings.
主要矿物是高岭石，常见豆状、鲕状和碎屑状构造。
Their main mineral is kaolinite, usually in pisolitic, oolitic or clastic structure.
主要矿物是高岭石，常见豆状、鲕状和碎屑状构造。
主要矿物是高岭石，常见豆状、鲕状和碎屑状构造。
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