Dissolution of orthopyroxene in basanitic magma between 0.4 and 2 GPa: further implications for the origin of Si-rich alkaline glass inclusions in mantle xenoliths
Cliff S. J. ShawVolume:
135
Language:
english
Pages:
19
DOI:
10.1007/s004100050501
Date:
May, 1999
File:
PDF, 575 KB
english, 1999