东天山黄山南镁铁-超镁铁质岩体锆石U-Pb年龄及岩浆演化过程探讨
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摘要
黄山南镁铁-超镁铁质岩体位于东天山造山带觉罗塔格构造带内,与构造带内一系列镁铁-超镁铁质岩体构成了东天山镁铁-超镁铁质岩带。黄山南岩体锆石U-Pb同位素定年得到293.7±3.1Ma的加权平均年龄,显示其形成年龄为早二叠世。岩石样品镁铁比值m/f比值介于4.45~6.37之间,属于铁质超基性岩;利用橄榄石最高Fo值计算得到黄山南岩体母岩浆的Mg~#值为0.70,表明其母岩浆成分与原生岩浆较为接近,具有高镁拉斑玄武岩质岩浆的性质,且演化程度较低或母岩浆有过剩橄榄石堆晶的加入。Ba/La、Ba/Nb、Ba/Th、Rb/Nb、Th/Nb和Sm/Yb等微量元素比值表明黄山南岩体的岩浆源区可能为一被俯冲板片沉积物和流体改造过的较富集的岩石圈地幔。主量元素变化特征显示了岩浆结晶分异作用的一般特征;较高的Ba/Nb比值,相对高的La/Nb和低La/Ba值以及Ni-Ta-(Ti)元素的负异常表明岩浆上升过程中可能经历了地壳物质的混染作用。黄山南岩体年龄及岩石地球化学特征综合表明其能够代表东天山地区地幔岩浆演化早期阶段的产物,具有较好的成矿潜力。
The Huangshannan mafic-ultramafic intrusion is located in the Jueluotage tectonic zone in East Tianshan Mountains,which is part of the large-scale mafic-ultramafic rock belt in this area. Zircon U-Pb isotopic dating of this intrusion yields a weighted average age of 293. 7 ± 3. 1Ma,indicating it was generated in the Early Permian. The m/f ratios of samples from the Huangshannan intrusion range from 4. 45 to 6. 37,implying ferric ultrabasic rock. Using the maximum Fo value of olivine,we estimate that the parental magma has a Mg#of 0. 70,showing a similar composition with primary magma and a characteristic of high-Mg tholeiitic basaltic magma. The parental magma has a low evolution degree,or it has been added by surplus olivine crystal. The ratios of Ba/La,Ba/Nb,Ba/Th,Rb/Nb,Th/Nb and Sm/Yb reveal that the source of the Huangshannan intrusion is relatively enriched lithospheric mantle which was reformed by slab-derived fluids and subducting sediment. The variation features of major elements show a crystallization differentiation process; relatively high Ba/Nb,La/Nb and low La/Ba ratios as well as the negative anomaly of Ni-Ta-( Ti) indicate that the magma of Huangshannan has likely suffered crustal contamination during its emplacement. Combining the age and the geochemical characteristics of the Huangshannan intrusion,we consider that this rock could represent the product of mantle magmatic evolution of early stage,having a good metallogenic potential.
The Huangshannan mafic-ultramafic intrusion is located in the Jueluotage tectonic zone in East Tianshan Mountains,which is part of the large-scale mafic-ultramafic rock belt in this area. Zircon U-Pb isotopic dating of this intrusion yields a weighted average age of 293. 7 ± 3. 1Ma,indicating it was generated in the Early Permian. The m/f ratios of samples from the Huangshannan intrusion range from 4. 45 to 6. 37,implying ferric ultrabasic rock. Using the maximum Fo value of olivine,we estimate that the parental magma has a Mg#of 0. 70,showing a similar composition with primary magma and a characteristic of high-Mg tholeiitic basaltic magma. The parental magma has a low evolution degree,or it has been added by surplus olivine crystal. The ratios of Ba/La,Ba/Nb,Ba/Th,Rb/Nb,Th/Nb and Sm/Yb reveal that the source of the Huangshannan intrusion is relatively enriched lithospheric mantle which was reformed by slab-derived fluids and subducting sediment. The variation features of major elements show a crystallization differentiation process; relatively high Ba/Nb,La/Nb and low La/Ba ratios as well as the negative anomaly of Ni-Ta-( Ti) indicate that the magma of Huangshannan has likely suffered crustal contamination during its emplacement. Combining the age and the geochemical characteristics of the Huangshannan intrusion,we consider that this rock could represent the product of mantle magmatic evolution of early stage,having a good metallogenic potential.
引文
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Mao Ya-jing,Qin Ke-zhang,Li Chu-si,Tang Dong-mei.2015.A modified genetic model for the Huangshandong magmatic sulfide deposit in the central Asian Orogenic belt,Xinjiang,western China[J].Miner Deposita,50:65-82
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Qian Zhuang-zhi,Sun Tao,Tang Zhong-li,Jiang Chang-yi,He Ke,Xia Ming-zhe,Wang Jian-zhong.2009.Platinum-group elements geochemistry and its significances of the Huangshandong Ni-Cu sulfide deposit,east Tianshan,China[J].Geological Review,55(6):873-884(in Chinese with English abstract)
Qin Ke-zhang,Ding Kui-shou,Xu Ying-xia,Sun He,Xu Xing-wang,Tang Dong-mei,Mao Qian.2007.Ore potential of protoliths and modes of Co-Ni occurrence in Tulargen and Baishiquan Cu-Ni-Co deposits,east Tianshan,Xinjiang[J].Mineral Deposit,6(1):1-14(in Chinese with English abstract)
Qin Ke-zhang,Su Ben-xun,Sakyi P A,Tang Dong-mei,Li Xian-hua,Sun He,Xiao Qing-hua,Liu Ping-ping.2011.SIMS Zircon U-Pb geochronology and Sr-Nd isotopes of Ni-Cu-bearing mafic-ultramafic intrusions in eastern Tianshan and Beishan in correlation with flood basalts in Tarimbasin(MW China):Constraints on a ca.280Ma mantle plume[J].American Journal of Science,311:1-23
Qin Qie,Guo Rui-qing,Zhang Xiao-fan,Zhan Xin-zhong,Guo Yin.2012.Zircon U-Pb geochronology and geological implications of the Xingdi No.Ⅳgabbro-dioritic pluton in Quruatagh,Xinjiang[J].Journal of Xinjiang University(Natural Science Edition),29(2):240-248(in Chinese with English abstract)
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San Jin-zhu,Qin Ke-zhang,Tang Zhong-li,Tang Dong-mei,Su Ben-xun,Sun He,Xiao Qing-hua,Liu Ping-ping.2010.Precise zircon U-Pb age dating of two mafic-ultramafic complexs at Tulaergen large Cu-Ni district and its geological implications[J].Acta Petrologica Sinics,026(10):3027-3035(in Chinese with English abstract)
Sun He,Qin Ke-zhang,Xu Xing-wang,Ding Kui-shou,Xu Ying-xia,San Jin-zhu.2007.Petrological characteristics and copper-nickel oreforming processes of early Permian mafic-ultramafic intrusion belts in east Tianshan[J].Mineral Deposits,26(1):98-108(in Chinese with English abstract)
Sun Tao,Qian Zhuang-zhi,Jiao Jian-gang,He Ke,Zhao Xiao-jian,Zhang Rui.2011.The deep progress of magma Cu-Ni sulfide ore-forming in east Tianshan region[J].Acta Mineralogica Sinca,(s1):170-171(in Chinese)
Sun Tao,Qian Zhuang-zhi,Tang Zhong-li,Jiang Chang-yi,He Ke,Sun Ya-li,Wang Jian-zhong,Xia Ming-zhe.2010.Zircon U-Pb chronology,platinum group element geochemistry characteristics of Hulu Cu-Ni deposit,east Xinjiang,and its geological significance[J].Acta Petrologica Sinca,26(11):333-3349(in Chinese with English abstract)
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