Investigation on the metamorphic conditions and geochronology for the magnet garnet amphibole in the Tan-Lu Fault Zone (Anhui segment), and discussion of its tectonic attribution
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摘要: 通过对肥东群南缘特征性岩石——磁铁石榴角闪岩的构造地质学和岩相学研究表明，磁铁石榴角闪岩及其围岩以构造透镜体形式产出，该变质岩具有两个阶段变质矿物组合，热力学评价显示①阶段的温压范围为：T=616~700℃和P=0.66~0.85GPa，平均温压为T=653±35℃和P=0.75±0.09GPa。②阶段的温压范围为：T=597~643℃和P=0.51~0.94GPa，平均温压为T=620±15℃和P=0.73±0.15GPa，并表现出一个快速等压降温P-T演化特征。锆石U-Pb定年和拉曼光谱分析表明，该磁铁石榴角闪岩的变质年龄为2469±49Ma。结合地质背景和前人的研究，可以判定该类岩石可能源于华北板块。由于郯庐断裂的左旋走滑作用被构造并置与扬子板块中。从而进一步推测，郯庐断裂（安徽段）横向宽度可达到10~15km。Abstract: Based on the research of tectonic geology and lithology, The magnet garnet amphibole and its adjacent rock occurs as the tectonic lens in the south of Feidong terrane. This metamorphic rocks contain two metamorphic assemblages from different stages, and the P-T estimates show that the P-T condition of ① stage is T=616~700℃ and P=0.66~0.85GPa respectively and the average T and P are 653±35℃ and 0.75±0.09GPa; Differentially, the ② stage is T=616~700℃ and P=0.66~0.85GPa, and average P-T condition is 653±35℃ and 0.75±0.09GPa. A rapid and slight Isobaric cooling process is indicated by features from the first stage to the second stage. According to the Raman Spectral Analysis and the LA-ICPMS dating, the metamorphic age of the magnet garnet amphibole is 2469 ± 49Ma. Combined with geological background and current situation, The magnet garnet amphibole maybe come from north china plate because of the sinistral strike-slip of Tan-Lu Fault Zone, It could be further theorized that the width of Tan-Lu Fault Zone is up to 10~15km.
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Key words:
- Magnet garnet amphibole /
- Isobaric cooling /
- Zircon U-Pb age /
- Tan-Lu Fault Zone
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