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Pressure‐Dependence of Rare Earth Element Distribution in Amphibolite‐ and Granulite‐ Grade Garnets. A LA‐ICP‐MS Study
Author(s) -
Bea Fernando,
Montero Pilar,
Garuti Giorgio,
Zacharini Federica
Publication year - 1997
Publication title -
geostandards newsletter
Language(s) - English
Resource type - Journals
eISSN - 1751-908X
pISSN - 0150-5505
DOI - 10.1111/j.1751-908x.1997.tb00674.x
Subject(s) - granulite , rare earth element , rare earth , geology , geochemistry , mineralogy , geomorphology , facies , structural basin
Using an excimer (KrF) laser ablation ICP‐MS system, we studied the distribution of REE in garnets from metapelites and metabasites from Ivrea‐Verbano (Western Alps, Italy) and from the Peña Negra Anatectic Complex (Central Iberia), finding systematic variations that correlate well with the metamorphic grade. Chondrite‐normalized REE patterns of garnets from amphibolite‐grade metapelites have lower‐than‐chondrite levels from La to Sm, a very small or no Eu anomaly, and a steep rise in the abundance of heavy REE as the atomic number increases. Metapelitic garnets from the amphibolite‐granulite transition have a marked Eu negative anomaly and are enriched in MREE such that Sm is 10‐15 times chondrite and the pattern is almost flat from Dy to Yb‐Lu. In garnets from granulite‐grade metapelites, the intensity of the Eu anomaly and the relative concentration of Nd, Sm, Gd and Tb increase, with almost flat chondrite‐normalized patterns from Sm to Lu. Garnets from mafic granulites are remarkably similar to those of metapelitic garnets equilibrated at the same pressure, except for the Eu anomaly. The apparent paradox of enhanced uptake of larger REE ions with increasing pressure is attributed to the 3M 2+ 2REE 3+ + vacancy substitution, which produces a net decrease in the dimensions of the unit‐cell of garnet. Variations in REE patterns depend essentially on the pressure and have little dependence on either temperature, bulk‐composition of garnet, or REE whole‐rock composition, so they could represent a new approach for geobarometric studies. The best numerical parameter to express pressure‐related variations of REE distribution in garnets is the Gd/Dy ratio which does not seem perceptibly affected by disequilibrium partitioning. The regression equation between GASP pressure and the average Gd/Dy garnet is P = 3.6 + 5.6 Gd/Dy. This equation seems to be reliable for garnets: (1)equilibrated within a pressure range of 4‐9 kbar, (2) coexisting with modal monazite; and (3) with unit‐cell dimensions under 11.46 Å.