Experimental investigation of F, Cl, and OH partitioning between apatite and Fe-rich basaltic melt at 1.0-1.2 GPa and 950-1000 °C (2015)
Attributed to:
Secular evolution of water in the lunar mantle
funded by
STFC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.2138/am-2015-5233
Publication URI: http://dx.doi.org/10.2138/am-2015-5233
Type: Journal Article/Review
Parent Publication: American Mineralogist
Issue: 8-9