Experimental modeling of ferropericlase formation under upper mantle conditions

上地幔条件下铁方镁石形成的实验模型

• 批准号: 406051903
• 负责人: Professor Dr. Alan Butler Woodland
• 金额: --
• 依托单位: Abteilung Petrologie und Geochemie
• 依托单位国家: 德国
• 项目类别: Research Grants
• 财政年份: 2018
• 资助国家: 德国
• 起止时间: 2017-12-31 至 2019-12-31
• 项目状态: 已结题
• 来源: https://gepris.dfg.de/gepris/projekt/406051903?language=en
• 关键词: Experimental; modeling; ferropericlase; formation; under

Ferropericlase, (Mg, Fe)O, is one of the major phases in the lower mantle. It occurs in diamonds from a number of localities worldwide either as single inclusions or together with ultrahigh pressure phases such as Mg-Perovskite (bridgemanite). Ferropericlase on its own or together with olivine is stable even at 1 atm. Diamonds with ferropericlase inclusions alone may therefore also originate in the transition zone or even the upper mantle for appropriate bulk rock compositions. Simultaneous with diamond formation, ferropericlase may precipitate from carbonatitic melts or grow by decomposition of subducted carbonates induced by redox reactions. In order to explore the possibility of ferropericlase crystallization in the upper mantle, we will conduct equilibrium experiments involving ferropericlase and silico-carbonate melt at ~6-10 GPa and temperatures up to 1600°C. An experimental configuration will be employed where carbonate and metal phases are separated by an olivine layer. Thus, the process of oxidation (Fe+1/2O2=FeO) and reduction (MgCO3=MgO+C+O2) will be spatially separated, and conditions will be investigated where ferropericlase and graphite/diamond crystallize directly from Mg-rich silico-carbonate melt. Experiments will be conducted in the high-mg# portion of the FeO-MgO-CaO-SiO2-CO2-C system with the goals of: (1) determining the composition of silico-carbonate melt in equilibrium with ferropericlase and olivine as a function of pressure and temperature, and (2) simulating ferropericlase crystallization via reduction of silico-carbonate melt with simultaneous formation of graphite or diamond.

铁方长石（Mg，Fe）O是下地幔中的主要矿物相之一。它存在于世界各地的金刚石中，或者作为单个包裹体，或者与镁-过氧化氢（硼镁石）等高压相一起存在。铁镁长石本身或与橄榄石一起即使在1个大气压下也是稳定的。因此，仅含铁方镁石包裹体的金刚石也可能起源于过渡带，甚至是上地幔，以获得适当的大块岩石成分。在金刚石形成的同时，铁方镁石可以从碳酸盐熔体中沉淀出来，或者通过氧化还原反应引起的俯冲碳酸盐的分解而生长。为了探索上地幔铁方镁石结晶的可能性，我们将在~6-10 GPa和高达1600°C的温度下进行铁方镁石和硅碳酸盐熔体的平衡实验。实验配置将采用碳酸盐和金属相分离的橄榄石层。因此，氧化（Fe+1/2 O2 =FeO）和还原（MgCO 3 =MgO+C+O2）的过程将在空间上分开，并将研究铁方镁石和石墨/金刚石直接从富镁的硅碳酸盐熔体结晶的条件。实验将在FeO-MgO-CaO-SiO_2-CO_2-C系统的高Mg ~#部分进行，目的是：（1）确定与铁方镁石和橄榄石平衡的硅-碳酸盐熔体的组成作为压力和温度的函数，和（2）通过还原硅-碳酸盐熔体同时形成石墨或金刚石来模拟铁方镁石结晶。