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Crystal-chemical controls on trace element partitioning between garnet and anhydrous silicate melt

Abstract:

We performed experiments at 3.0 GPa and 1530-1565 °C to investigate the effects of crystal composition on trace element partitioning between garnet and anhydrous silicate melt. Bulk compositions along the pyrope (Py: Mg3Al2Si3O12)-grossular (Gr: Ca3Al2Si3O12) join, doped with a suite of trace elements (Li, B, K, Sc, Ti, Sr, Y, Zr, Nb, Cd, In, REE, Hf, Ta, Th, and U) produced homogeneous garnets, ranging in composition from Py84Gr16 to Py9Gr91, in equilibrium with melt. Trace element partition...

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Publication status:
Published

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Journal:
AMERICAN MINERALOGIST
Volume:
84
Issue:
5-6
Pages:
838-847
Publication date:
1999-01-01
ISSN:
0003-004X
Source identifiers:
163830
Language:
English
Pubs id:
pubs:163830
UUID:
uuid:a57b5dc6-9d55-4572-bfbf-31601a9e7369
Local pid:
pubs:163830
Deposit date:
2012-12-19

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