Crystallization and Cooling of the Noril’sk Intrusions According to the Pyroxen’s Geothermometry Data

Abstract

Composition of clinopyroxenes in vertical sections of some ore-bearing basic intrusions in the Noril’sk area has been studied by EPMA. These data formed the basis for the calculation of the pyroxene crystallization temperatures using the El Negro monopyroxene geothermometer (Fe-Mg exchange between M1-M2 positions). The results of the calculations allowed estimating the variations of temperature crystallization within the magmatic chambers from early to the late stages. The temperature varies from 1200 for idiomorphic crystals in equilibrium to liquid and up to 400 degrees (in solid intra exchange) for xenomorphic grains and marginal zones of pyroxenes. We reconstructed the regimes of crystallization of the magmatic chamber by this data. The vertical distribution of paleotemperatures of the intrusive chamber there is the evidence of absence vertical move crystals into such magmatic chambers.