淮南煤田潘三井田西部岩浆岩侵入年代确定与意义Magmatic Intrusive Age Determination and Its Significance in Western Panji No.3 Minefield,Huainan Coalfield
苗林,刘桂建,吴盾,吴斌,陈健
摘要(Abstract):
岩浆岩在淮南煤田潘谢矿区广泛发育,以潘三井田西翼岩浆岩为研究对象,对采集的岩浆岩样品经破碎、人工分选出锆石,采用激光剥蚀电感偶合等离子体质谱(LA-ICP-MS)对锆石进行元素和同位素测试,将测试结果用isoplot软件包投影到207Pb/235U-206Pb/238U图解上,并与标准锆石91500分析点所获得的同位素比值经线性拟合。结果表明,研究区内岩浆岩发生侵位的时期为距今大约118Ma,属于早白垩世四川期(135~52Ma)岩浆活动,晚于研究区内主要断层形成的年代。
关键词(KeyWords): 潘三井田;岩浆岩;同位素定年
基金项目(Foundation): 国家自然科学基金(NO.41173032);; 淮南矿业集团科技计划项目联合资助
作者(Author): 苗林,刘桂建,吴盾,吴斌,陈健
参考文献(References):
- [1]安徽省煤田地质局勘察研究院.淮南煤田潘北井田地质报告[R].安徽合肥:安徽省煤田地质局,2006.
- [2]Horn I,Rudnick R and McDonough WF.2000.Precise elemental andisotope ratio determination by simultaneous solution nebulization andlaser ablation-ICP-MS:application to U-Pb geochronology.ChemicalGeology,167:405-425.
- [3]Yuan H.-L.,Wu F.-Y.,Gao S.,et al.2003.Determination of U-Pband rare earth element concentrations of zircons from Cenozoicintrusions in northeastern China by laser ablation ICP-MS.Chinese Sci.Bull.,48,241 1-2421.
- [4]Rubatto D,Gebauer D.Use of cathodoluminescence for U-Pb zircondating by IOM Microprobe:Some examples from the western Alps.Cathodoluminescence in Geoscience,Springer-Verlag BerlinHeidelberg,Germany.2000,373-400.
- [5]M_ller A,O'Brien P J,Kennedy A,et al.Linking growth episodes ofzircon and metamorphic textures to zircon chemistry:An example fromthe ultrahigh-temperature granulites of Rogaland(SW Norway).EMUNotes in Mineralogy,2003,5:65-82.
- [6]徐德金,胡宝林,胡魏.淮北煤田卧龙煤矿岩浆侵入煤层的构造控制[J].煤田地质与勘探,2011,39(5):1-5.
- [9]Ames L,Zhou G Z,Xiong B C.Geochronology and geochemistry ofultrahigh-pressure metamorphism with implication for collision of Sino-Korean and Yangtze Cratons.Central China[J].Tectonics.1996,15(2):472-489.
- [8]索书田,钟增球,游振东.大别-苏鲁构造带三叠纪碰撞缝合线的位置[J].地球科学-中国地质大学学报,2000.25(2):111-116.
- [9]李锦轶.中朝地块和扬子地块碰撞的时限与方式[J].地质学报,2001,75(1):25-34.
- [10]宋传中,朱光,刘国生,等.淮南煤田的构造厘定及动力学控制[J].煤田地质与勘探,2005,33(1):11-15.