辉石最常见的次生变化是蛇纹石化和纤闪石化。
The most common secondary changes of pyroxene are the petrochemistry and the petrochemistry.
分布在大弄地区岩墙状及岩脉状强透闪石化岩石，过去一直被认为是闪长岩。
Strong tremolitization rocks in shape of rock walls and rock veins, distributed in the Dalong area, have been viewed as the diorites at all times.
结合矿石化学分析和镜下鉴定结果，证实闪石类矿物与磁性铁有着密切关系。
Combined with the chemical analysis and the microscopic identification results, it is confirmed that amphibole minerals have a close relationship with magnetic iron.
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