条纹长石为交代成因。
条纹长石是正长石或微斜长石与钠长石交生的产物，其中正长石或微斜长石多于钠长石。
Perthite is orthoclase or microcline and albite over the product, which is more than orthoclase or microcline albite.
如果在大的钾长石晶体上，见有根须状的细脉，而且细脉的颜色又较浅，则为条纹长石。
If the large K-feldspar crystals, see roots like veins and veinlets, color is shallow, is perthitic.
与这些大型-超大型钼矿床有关的岩体顶部都发育了钾长石石英条纹岩。
Potash feldspar quartz crenulate often appears on the top of rock masses which are related to the molybdenum deposits.
这种条纹的粉色源自于一种名为钾长石的结晶矿物质。
The bands get their pink color from a crystallized mineral called potassium feldspar.
这种条纹的粉色源自于一种名为钾长石的结晶矿物质。
The bands get their pink color from a crystallized mineral called potassium feldspar.
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