< p >有几个选项。< / p > - During decompression, biotite is no longer stable and the hydrogen volatilises, leaving behind fine-grained intergrowth of oxide and silicate minerals.
- Oxidation of the rims during exposure of the lava to the atmosphere. Higher Fe3+ contents would make the biotite darker.
It is impossible to tell without a detailed electron microscopy analysis. However, my guess it that it is option 1.