С. Н. Кох

Изоморфная емкость мелилитовых твердых растворов при параметрах пирогенного метаморфизма

Partitioning of trace elements between minerals crystallized from Ca-rich Si-undersaturated melts is constrained for the first time in samples of coarse combustion metamorphic (CM) melt rocks (paralavas) from the Hatrurim Formation. The partition coefficients of trace elements (i...