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Analytical method: TIMS

TechniqueTIMS
MaterialWHOLE ROCK
Mineralnone
InstitutionUSGS MENLO PARK, MENLO PARK, CA 94025, USA
ReferenceBacon, C. R.; Adami, L. H.; Lanphere, M. A. (1989) Direct evidence for the origin of low- (super 18) O silicic magmas; quenched samples of a magma chamber's partially-fused granitoid walls, Crater Lake, Oregon. Earth and Planetary Science Letters. 96; 1-2, Pages 199-208. 1989.

Samples analysed with this method

s_1092, s_452, s_799, s_1023, s_1038, s_195, s_1326, s_432, s_1290, s_606, s_582, s_637, s_154, s_803, s_811, s_153, s_160, s_775, s_825, s_435, s_152, s_306, s_198, s_381, s_621, s_1143, s_1216, s_354, s_854, s_533, s_853, s_705