NJG56-3-05
1976
Compositional gradient in interstitial hornblende from a Norwegian garnet websterite
56
3
309-314

Hornblende formed at the grain boundaries between pyrope, diopside, and enstatite of a Norwegian gamet websterite exhibits concentration gradient. The pattem of the concentration gradient is explained by the material flow through the interstitial homblende, by which local equilibrium is reached among homblende and anhydrous minerals.

0029-196X
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