滁州地区金牛侵入体的岩石成因:拆沉下地壳熔融还是壳幔混合
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摘要
滁州冶山地区研究程度较低,前人研究认为金牛岩体属于冶山岩体的边缘相,本次对金牛岩体开展独立研究。金牛侵入岩锆石U-Pb定年结果为(129±2)Ma,属于早白垩世早期。锆石原位Hf同位素分析显示,具有较均一的负εHf(t)值(-2.82~-6.52)和较古老的地壳模式年龄tDMC(1360~1600 Ma)。金牛岩体为碱性(σ:5.08~5.74)、准铝质(A/CNK:0.803~0.844)岩石,具有较强的轻重稀土元素分异、无明显-弱负Eu异常、相对富集轻稀土元素、大离子亲石元素,明显亏损重稀土元素和高强场元素的特点,综合对比冶山岩体,认为金牛岩体与冶山岩体同期不同源。结合区域构造演化特征及岩石地球化学、Hf同位素特征,金牛岩体很可能为来源于富集岩石圈地幔的富水底侵基性岩浆与古老下地壳部分熔融形成的岩浆混合的产物,其源动力与太平洋板块的俯冲有关。
The research on Lower Yangtze block in Yeshan area of Chuzhou is very insufficient. Previous researchers held that Jinniu rock mass belongs to marginal facies of Yeshan pluton. In this paper, the authors studied Jinniu pluton. Zircon U-Pb dating indicates that The Jinniu pluton of Yeshan area of Lower Yangtze block was formed at 129±2 Ma, suggesting a product of Early Cretaceous.Zircon Hf isotopic composition has relatively uniform negative εHf(t)values(-2.82--6.52)and old Hf isotopic crustal model ages(1360-1600 Ma). The Jinniu pluton is alkaline(σ:5.08-5.74)),metaluminous rock body(A/CNK:0.803-0.844),which is characterized by relatively strong differentiation between light and heavy rare earth elements,indistinct negative Eu anomalies,enrichment of LREE and LILE, and depletion of HREE and HFSE. Comprehensive comparative study of the Yeshan rock mas shows that the Jinniu rock mass and Yeshan rock mass belong to two different sources of the same period. Regional tectonicevolution characteristics and geochemistry of rocks and Hf isotope characteristics indicate that the source of the Jinniu rock mass seems to have been a mixed product of underplating water-rich basic magma from enriched lithospheric mantle and partially melted ancient lower crust due to the subduction of Paleo-Pacific Plate.
The research on Lower Yangtze block in Yeshan area of Chuzhou is very insufficient. Previous researchers held that Jinniu rock mass belongs to marginal facies of Yeshan pluton. In this paper, the authors studied Jinniu pluton. Zircon U-Pb dating indicates that The Jinniu pluton of Yeshan area of Lower Yangtze block was formed at 129±2 Ma, suggesting a product of Early Cretaceous.Zircon Hf isotopic composition has relatively uniform negative εHf(t)values(-2.82--6.52)and old Hf isotopic crustal model ages(1360-1600 Ma). The Jinniu pluton is alkaline(σ:5.08-5.74)),metaluminous rock body(A/CNK:0.803-0.844),which is characterized by relatively strong differentiation between light and heavy rare earth elements,indistinct negative Eu anomalies,enrichment of LREE and LILE, and depletion of HREE and HFSE. Comprehensive comparative study of the Yeshan rock mas shows that the Jinniu rock mass and Yeshan rock mass belong to two different sources of the same period. Regional tectonicevolution characteristics and geochemistry of rocks and Hf isotope characteristics indicate that the source of the Jinniu rock mass seems to have been a mixed product of underplating water-rich basic magma from enriched lithospheric mantle and partially melted ancient lower crust due to the subduction of Paleo-Pacific Plate.
引文
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