Role of syn-eruptive plagioclase disequilibrium crystallization in basaltic magma ascent dynamics
The quantification of timing for crystallization and exsolution processes are fundamental to our understanding of basaltic magma ascent dynamics. Here, the authors constrain timings to show that plagioclase reaches equilibrium in 1-2 hours, whereas ascent times were <1 hour.
| প্রধান লেখক: | , , , |
|---|---|
| বিন্যাস: | প্রবন্ধ |
| ভাষা: | English |
| প্রকাশিত: |
Nature Portfolio
2016-12-01
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| মালা: | Nature Communications |
| অনলাইন ব্যবহার করুন: | https://doi.org/10.1038/ncomms13402 |