“绿泥石”造句

在这些矿物中, 高岭石, 伊利石和绿泥石最常见.
Of these minerals, kaolinite, illite and chlorite are commonest.

绿泥石呈卷曲网状或折迭片状.
Corrensite forms networks of crinkled or folded sheets.

兰杰地区的强烈绿泥石化岩石据信可能是蚀变粒玄岩.
In the Ranger area highly chloritic rocks were believed to be altered dolerites.

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