本文選題：含石榴子石花崗片麻巖 + 溫度—壓力(P—T)評價　； 參考：《地質(zhì)論評》2017年02期

【摘要】：蚌埠隆起區(qū)是華北克拉通的重要組成部分,然而前人對于蚌埠隆起結(jié)晶基底形成的變質(zhì)環(huán)境和時限分析相對較為薄弱,制約了人們?nèi)胬斫庠撀∑鸬男纬珊脱莼^程。因此,本文在詳細(xì)的野外地質(zhì)調(diào)查基礎(chǔ)上,對在蚌埠隆起東部朱頂—石門山地區(qū)新發(fā)現(xiàn)的含石榴子石花崗片麻巖進(jìn)行了較為細(xì)致的巖相學(xué)、礦物化學(xué)測試分析以及LA-ICP-MS鋯石U-Pb定年,運(yùn)用不同的溫壓計方法進(jìn)行P—T條件估計,得出該樣品溫壓條件為736~788℃和0.76~0.89GPa,表明其形成于低壓麻粒巖相條件。鋯石定年分析記錄了巖漿結(jié)晶和變質(zhì)兩期事件,它們對應(yīng)的年齡分別為2562±34~2584±25Ma和2433±31~2436±24Ma。
[Abstract]:The Bengbu uplift is an important part of the North China Craton. However, the metamorphic environment and time limit analysis of the crystalline basement formation of Bengbu uplift is relatively weak, which restricts the overall understanding of the formation and evolution of the uplift. Therefore, on the basis of detailed field geological investigation, the new discovered granitic gneiss containing pomegranate in the eastern Zhuding-Shimenshan area of Bengbu uplift has been studied in detail. Mineral chemical analysis and LA-ICP-MS zircon U-Pb dating were used to estimate P-T conditions. The temperature and pressure conditions of the samples were 736 鈩，

本文編號：1850629