Direct evidence for the origin of low-18O silicic magmas:...

Direct evidence for the origin of low-18O silicic magmas: quenched samples of a magma chamber's partially-fused granitoid walls, Crater Lake, Oregon

Charles R. Bacon, Lanford H. Adami, Marvin A. Lanphere
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Volume:
96
Year:
1989
Language:
english
Pages:
209
DOI:
10.1016/0012-821x(89)90132-5
File:
PDF, 797 KB
english, 1989
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