构造岩体积应变率与质量迁移率关系分析——以郯庐断裂长英质构造岩为例
Yunnan Geology(2006)
Abstract
构造岩质量迁移率与体积应变率关系的研究,是对经典构造岩石学领域的拓展和补充,具有广泛的理论和经济地质应用前景.利用质量等比线的原理、方法,对郯庐断裂浮槎山构造岩进行分析得知,在原岩变形变质为构造岩的过程中,化学组分的相对迁移由强到弱分别为:初糜棱岩中P2O5→total Fe→TiO2→MgO→H2O→MnO→SiO2→K2O→CaO→Na2O,糜棱岩中P2O5→MgO→TiO2→total Fe→H2O→MnO→K2O→CaO→Na2O→SiO2,超糜棱岩中P2O5→MgO→TiO2→CaO→total Fe→H2O→MnO→SiO2→K2O→Na2O.
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