Garnet growth in natural high pressure regime: a key tool in unravelling the pressure-temperature path of rocks involved in mountain belt orogeny

机译：天然高压制度的石榴石生长：解开山腰orgeny岩石压力温度路径的关键工具

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A study of a natural system concerning the growth of minerals (garnet) into metapelite host rocks from Calabria (southern Italy), which underwent pressure up to 1.2 GPa, is presented. Through the application of a thermodynamic model it was possible to determine P and T conditions achieved during metamorphic evolution of these rocks useful to reconstruct the related tectonic settings of poly-orogenic metamorphic complexes.

机译：提出了一种关于矿物质（石榴石）生长到来自Calabria（南部意大利）的矿物质岩石的天然系统的研究，该系统出现了高达1.2 GPA的压力。通过应用热力学模型，可以确定在这些岩石的变质演化期间实现的P和T条件可用于重建多造或多孔状复合物的相关构造环境。

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《AIRAPT International Conference on High Pressure Science and Technology》|2007年||共13页
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G Angi; R Cirrincione; E Fazio; G Ortolano; A Pezzino; R Punturo;
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机译：天然高压制度的石榴石生长：解开山腰orgeny岩石压力温度路径的关键工具
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Garnet growth in natural high pressure regime: a key tool in unravelling the pressure-temperature path of rocks involved in mountain belt orogeny

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