Evidence for low-temperature ultrapotassic siliceous fluids in subduction zone environments from experiments in the system K2OMgOAl2O3SiO2H2O (KMASH)
- 1 November 1992
- Vol. 28 (3-6) , 421-434
- https://doi.org/10.1016/0024-4937(92)90017-s
Abstract
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