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Dopant incorporation into garnet solid solutions--a breakdown of Goldschmidt's first rule
W van Westrenen1, N L Allan, J D Blundy
1Geophysical Laboratory, Carnegie Institution of Washington, DC 20015, USA.
Abstract:
Atomistic simulations suggest trace elements are more soluble in a 50:50 pyrope (Mg3Al2Si3O12)-grossular (Ca3Al2Si3O12) garnet mixture than in either end-member; consistent with partitioning experiments, and, contrary to Goldschmidt's first rule, large trace element cations may substitute for Mg2+, small trace elements for Ca2+.