主要矿体形态呈似层状、豆荚状，与地层产状一致。

Orebodies take stratoid and lensoid forms, with their dip and strike consistent with the attitude of the wall rocks.

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主要矿体形态呈似层状、豆荚状，与地层产状一致。

Orebodies take stratoid and lensoid forms, with their dip and strike consistent with the attitude of the wall rocks.

youdao