MAJOR, TRACE AND RARE EARTH ELEMENT GEOCHEMISTRY OF AMPHIBOLE NEAR THE ROOF OF A MAFIC MAGMA CHAMBER
All amphiboles in mafic and ultramafic rocks are calcic, with (Ca+Na)B ≥ 1.34 and NaB < 0.67 apfu, and SiIV between 6.1 and 7.3. They range in composition from tschermakite, to tschermakitic hornblende, to magnesio-hornblende and display a dominance of edenite (Na,KA + AlIV = SiIV) substitution. Each sample exhibits remarkably uniform Mg/(Mg+Fe2+) over a wide range in Si and the mafic rock amphiboles have lower (0.5 to 0.7) Mg/(Mg+Fe2+), compared to the ultramafic rocks (0.7 and 0.9). REE profiles of amphiboles from mafic rocks are all bow-shaped, and are characterized by depletion in LREE (La/Sm ≈ 0.61), a slight depletion in HREE (Gd/Yb ≈ 1.55) and a negative Eu anomaly, which is attributed to co-precipitation of plagioclase. REE profiles of ultramafic amphiboles are divided into two groups: Group A amphiboles occur in all specimens analyzed and are very similar to the profiles of the mafic rocks. In contrast, Group B amphiboles display relative enrichment in light REEs (La/Sm ≈ 2.05), have lower ΣREE, and lack a negative Eu anomaly. Group B amphiboles are more enriched in Th and U and show a more pronounced depletion in Ta, Nb, Ti and Y. Group B amphiboles grew in a reaction relationship with olivine and pyroxene. Groups A and B are virtually indistinguishable with respect to the major elements, suggesting that REE and selected trace elements when combined with textural observations may provide additional insights into crystallization history.