The origin of calcite in calc-silicate rocks from the Kokchetav ultrahigh-pressure metamorphic complex

Understanding calcite genesis in ultrahigh-pressure crustal rocks is a key to the reconstruction of the evolution of ultrahigh-pressure metacarbonate rocks. Here, we present new data and a new model on the genesis and the P-T conditions of the formation of calcite found in the ultrahigh-pressure calc-silicate rocks from the Kokchetav massif. In the studied sample aragonite inclusions coexist with Type A calcite inclusions (previously interpreted as mineral inclusions) and the inclusions of Type B calcite (previously interpreted as derived from the crystallization of carbonatitic melt) in cores of garnet porphyroblasts. The most Mg-rich calcite from Type A inclusions coexisting with aragonite inclusions in one garnet growth zone shows X-Ca = 0.935 implying their crystallization during a retrograde metamorphic stage at P similar to 2.3 GPa and T similar to 870 degrees C along the P-T path. Type A calcite and aragonite inclusions were also found coexisting in one growth zone with K-bearing clinopyroxene inclusion (omega[K2O] = 0.5 wt.%). Such a high K2O-content in clinopyroxene testify that the pressure of inclusion capture exceeded 3.5 GPa, which contradicts the P-T conditions estimated by X-Ca in magnesian calcite. Thus, Type A calcite inclusions were initially captured as an aggregate of aragonite+ magnesian calcite at ultrahigh pressure metamorphic stage (P >= 3.5 GPa, T = 900-1,000 degrees C) and then re-equilibrated at lower conditions (P <= 2.3 GPa and T <= 870 degrees C). The trace element composition of aragonite and Type A and Type B calcite from inclusions was also studied to clarify calcite genesis in these inclusions. Aragonite shows high LREE (5-57 ppm) and Sr-content (600-800 ppm). Calcite from Type A inclusions shows low LREE (2.9-19.8 ppm) and Sr-content (490-670 ppm). Calcite from Type B inclusions forms two groups according to the LREE and Sr content distribution (Type B1 and Type B2). Trace element distribution in Type B1 calcite is identical to that of Type A calcite, while Type B2 calcite shows high LREE (6.8-64.9 ppm) concentrations along with low Sr-content (180-340 ppm). Type A and Type B1 calcite is interpreted to have been re-equilibrated. Type B2 calcite inclusions crystallized from the hydrous carbonatitic melt.