内蒙古集宁三岔口夕线堇青石榴二长片麻岩变质作用及年代学研究  

Metamorphic P-T conditions and U-Pb dating of the sillimanite-cordierite-garnet paragneisses in Sanchakou,Jining area,Inner Mongolia

作　　者：蔡佳[1] 刘福来[1] 刘平华[1] 施建荣[1] 

机构地区：[1]中国地质科学院地质研究所,北京100037

出　　处：《岩石学报》2014年第2期472-490,共19页Acta Petrologica Sinica

基　　金：科技部973项目(2012CB416603);国家杰出青年科学基金项目(40725007);中国地质调查局地质大调查项目(1212010811065;1212011120150)联合资助

摘　　要：三岔口夕线堇青石榴二长片麻岩出露于华北克拉通孔兹岩带东部的集宁变质杂岩中,该岩石保留了典型的减压反应结构。系统的岩相学观察和矿物化学研究结果表明,三岔口地区夕线堇青石榴二长片麻岩保存了两个阶段变质作用的矿物组合及相应的变质反应结构,其中峰期变质阶段M1的矿物组合为石榴石＋夕线石＋黑云母＋石英＋斜长石＋钾长石＋钛铁矿±磁铁矿;峰后减压的M2-1变质阶段矿物组合为石榴石＋堇青石＋夕线石＋石英＋斜长石＋钾长石＋钛铁矿±尖晶石,M2-2阶段的矿物组合为石榴石＋堇青石＋黑云母＋石英＋斜长石＋钾长石＋钛铁矿＋磁铁矿±尖晶石。自峰期变质阶段到峰后减压阶段,典型的转变（减压）反应包括：Grt＋Sil＋Melt→Crd＋Bt＋Fe-oxide和Grt＋Sil→Crd＋Spl。相平衡模拟结合传统地质温压计限定峰期变质阶段的温压条件为T=852-862℃,P=9.3-10.2kbar;峰期后近等温减压的M2-1和M2-2阶段的温压条件分别为854-880℃和7.0-7.4kbar,820-848℃和5.3-6.4kbar。三岔口夕线堇青石榴二长片麻岩记录了典型的近等温减压型的顺时针P-T轨迹。阴极发光图像特征显示夕线堇青石榴二长片麻岩存在大量变质锆石,LA-ICP-MS U-Pb定年结果表明,所有变质锆石记录了十分一致的207Pb/206Pb年龄,其变质时代为1912±11Ma。变质作用历史说明内蒙古孔兹岩带东段的集宁地体卷入了华北克拉通西部的阴山陆块和鄂尔多斯陆块之间的俯冲-碰撞,并经历了古元古代（-1912Ma）的麻粒岩相变质作用后快速折返至地表的过程。Sanchakou sillimanite-cordierite-garnet paragneisses,showing distinct decompressional textures,crop out in Jining Complex in the eastern segment of the Khondalite Belt,the North China Craton（ NCC）. The mineral assemblages and microtextures of the Sanchakou sillimanite-cordierite-garnet paragneisses allow a reconstruction of the metamorphic history of the area. The rocks contain two distinct metamorphic assemblages according to the systematic petrographic observations and mineral chemistry,namely the peak（ M 1） and the post-peak（ M 2） stages. The peak（ M 1） assemblage consists of garnet（ mantle） ＋ sillimanite ＋ biotite ＋ quartz ＋ plagioclase ＋ K-feldspar ＋ ilmenite ± magnetite. Post-peak near-isothermal decompressional（ M 2） stage following the peak stage could be subdivided into two stages M 2-1 and M 2-2. The M 2-1 stage is characterized by garnet and the development of cordierite ＋ sillimanite ＋ quartz ＋ plagioclase ＋ K-feldspar ＋ ilmenite ± spinel corona,and the M 2-2 stage is represented by garnet ＋ cordierite ＋ biotite ＋ quartz ＋ plagioclase ＋ K-feldspar ＋ ilmenite ＋ magnetite ± spinel,involving the reactions of garnet ＋ sillimanite ＋ melt→ cordierite ＋ biotite ＋ Fe-oxide and garnet ＋ sillimanite → cordierite ＋ spinel. Quantitative phase equilibria modeling in the system Na2 O-CaO-K 2 O-FeOMgO-Al 2 O 3-SiO 2-H 2 O-TiO 2-Fe 2 O 3,in combination with traditional thermobarometry,was applied to obtain P-T conditions of 852~862℃ and 9. 3~10. 2kbar for M 1,854~880℃ and 7. 0~7. 4kbar for M 2-1,820~848℃ and 5. 3~6. 4kbar for M 2-2. The combination of the mineral assemblages,mineral compositions,and metamorphic reaction histories in the Sanchakou sillimanitecordierite-garnet paragneisses defines a clockwise P-T path that involves near-isothermal decompression that followed the peak granulitefacies metamorphism. Cathodoluminescent images show that zircons contained in the Sanchakou sillimanite-cordierite-garnet paragneisses mostly are

关 键 词：变泥质岩 相平衡模拟 U-PB年代学 古元古代 三岔口 集宁地区 

分 类 号：P588.3[天文地球—岩石学]