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Tectonic implications of transitional eclogite from haiyangsuo, rushan county, eastern shandong peninsula

机译:山东半岛东部鲁山县海阳梭过渡榴辉岩的构造意义

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Transitional eclogite were found recently at Haiyangsuo, Rushan County, and eastern Shandong Peninsula. It shown metamorphic transformation from granulite to plagioclase-bearing transitional eclogite. The Granulite-facies assemblage (Grt-I + Cpx-I + Opx + P1-I + Ilm) is equilibrated at temperature of 78-830 deg. C and pressure of 8-9 kbar. Its granular textures are well preserved in the less deformed rock. With the development of the shearing deformation accompanied by fluid infiltration during the transitional Eclogite facies, the granulitic assemblage transformed to a transitional eclogitic paragenesis (Cpx-II (Omp/Di) + Grt-II + P1-II (Ab)+ Rut + Qtz + Ky + Zo + Tlc) with various degree.
机译:最近在海阳所,乳山县和山东半岛东部发现了过渡榴辉岩。它显示了从花岗石到斜长石过渡榴辉岩的变质转变。在78-830度的温度下平衡了花岗石相组合(Grt-1 + Cpx-1 + Opx + P1 + Ilm)。 C,压力为8-9 kbar。它的颗粒状纹理保存在变形较小的岩石中。随着过渡榴辉岩相中剪切变形的发展并伴有流体的渗透,花岗质组合转变为过渡渐次共生(Cpx-II(Omp / Di)+ Grt-II + P1-II(Ab)+ Rut + Qtz + Ky + Zo + Tlc)。

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