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    新疆北山二叠纪镁铁-超镁铁质岩成因、成矿作用和找矿信息

    阮班晓 吕新彪 俞颖敏 刘月高 柳潇 魏巍 王鹏 王恒

    阮班晓, 吕新彪, 俞颖敏, 刘月高, 柳潇, 魏巍, 王鹏, 王恒, 2020. 新疆北山二叠纪镁铁-超镁铁质岩成因、成矿作用和找矿信息. 地球科学, 45(12): 4481-4497. doi: 10.3799/dqkx.2020.245
    引用本文: 阮班晓, 吕新彪, 俞颖敏, 刘月高, 柳潇, 魏巍, 王鹏, 王恒, 2020. 新疆北山二叠纪镁铁-超镁铁质岩成因、成矿作用和找矿信息. 地球科学, 45(12): 4481-4497. doi: 10.3799/dqkx.2020.245
    Ruan Banxiao, Lü Xinbiao, Yu Yingmin, Liu Yuegao, Liu Xiao, Wei Wei, Wang Peng, Wang Heng, 2020. Petrogenesis, Mineralization and Prospecting Information of Permian Mafic-Ultramafic Rocks, Beishan, Xinjiang. Earth Science, 45(12): 4481-4497. doi: 10.3799/dqkx.2020.245
    Citation: Ruan Banxiao, Lü Xinbiao, Yu Yingmin, Liu Yuegao, Liu Xiao, Wei Wei, Wang Peng, Wang Heng, 2020. Petrogenesis, Mineralization and Prospecting Information of Permian Mafic-Ultramafic Rocks, Beishan, Xinjiang. Earth Science, 45(12): 4481-4497. doi: 10.3799/dqkx.2020.245

    新疆北山二叠纪镁铁-超镁铁质岩成因、成矿作用和找矿信息

    doi: 10.3799/dqkx.2020.245
    基金项目: 

    国家自然科学基金项目 41802101

    新疆358项目 XGMB2012012

    中国地质调查项目 DD20179607

    教育部中央高校基本科研基金项目 G1323541879

    教育部中央高校基本科研基金项目 G1323541839

    详细信息
      作者简介:

      阮班晓(1988-), 男, 讲师, 博士, 主要从事镁铁-超镁铁质岩成岩成矿作用研究.ORCID:0000-0003-0077-3313.E-mail:bxruan@foxmail.com

      通讯作者:

      吕新彪, ORCID:0000-0003-0588-7934.E-mail:luxb@cug.edu.cn

    • 中图分类号: P612

    Petrogenesis, Mineralization and Prospecting Information of Permian Mafic-Ultramafic Rocks, Beishan, Xinjiang

    • 摘要: 为认识新疆北山二叠纪镁铁-超镁铁质岩石成岩成矿作用,基于地质调查获得的新资料,对这套岩石存在争议或认识模糊的年代学、岩浆起源与性质、动力学背景、硫化物熔离机制等进行了重新梳理.区内幔源岩浆除了早二叠世大规模侵入,中二叠世还有一期小规模侵入(261~266 Ma).母岩浆起源于受俯冲流体交代改造的亏损地幔在相对浅的深度发生高程度部分熔融,其具高温、高镁、含水、氧化特征.这些岩石并非地幔柱成因,亦非产于岛弧环境,而是造山后伸展背景下板片断裂引起的软流圈地幔上涌形成镁铁质侵入岩.坡北亚带和红石山亚带具有类似的岩石矿物组合和地球化学特征,但是矿化方式有明显差异.不同类型矿化是硫化物多期次熔离的产物,来自邻近VMS型铜矿床的外源硫混染触发硫化物在橄榄石结晶分异之前熔离,高品位脉状矿化是硫化物矿浆晚期贯入苏长岩的产物.超镁铁质岩相橄榄石中较低的Ni含量,岩体低Ti、高Mg、高m/s和m/f比值、母岩浆MgO含量大于11.5%、部分熔融程度不低于10%、固结指数SI大于50,均是有利的找矿指标,红十井深大断裂一带可能具有找矿潜力.

       

    • 图  1  研究区区域地质简图

      a.中亚造山带分布;b.新疆镁铁质岩分布(据陈继平等,2013Zhang et al., 2015修改);c.东天山-北山镁铁-超镁铁质岩分布(据Su et al., 2012修改);d.新疆北山镁铁-超镁铁质岩分布(据Ruan et al., 2020修改).①大南湖-头苏泉岛弧,②小热泉子-梧桐窝子弧内盆地,③康古尔-黄山韧性剪切带,④雅满苏弧后盆地;I.阿齐库都克-沙泉子断裂,Ⅱ.红柳河-依格孜塔格断裂,Ⅲ.白地洼-淤泥河断裂,Ⅳ.红十井断裂

      Fig.  1.  Regional geological map of the studied area

      图  2  新疆北山镁铁-超镁铁质岩岩相期次及矿化

      Fig.  2.  Lithofacies sequence and mineralization of mafic-ultramafic rocks in the Beishan area, Xinjiang

      图  3  新疆北山二叠纪镁铁-超镁铁质岩带岩体侵位年龄

      各岩体年龄见附表 3;东天山-北山镁铁质岩年龄范围据Qin et al.(2011)

      Fig.  3.  Ages of the Permian mafic-ultramafic complexes in the Beishan area, Xinjiang

      图  4  新疆北山镁铁-超镁铁质岩及同时期中酸性岩石的Sr-Nd同位素组成

      早二叠世岩石数据参考Su et al.(2012)Xue et al.(2016a, 2016b)和Zhang et al.(2015),中二叠世岩石数据参考苏本勋等(2010)Xue et al. (2016b);MORB.大洋中脊玄武岩;OIB.洋岛玄武岩;EMⅠ.Ⅰ型富集地幔;EMⅡ.Ⅱ型富集地幔

      Fig.  4.  Sr-Nd isotopic compositions of mafic-ultramafic rocks and contemporaneous felsic rocks in Beishan area

      图  5  新疆北山镁铁质岩石中铬铁矿内部固相包裹物

      a.角闪石(Amp)和金云母(Phl)包裹体;b.钠金云母(Na-Phl)和角闪石包裹体;c.镍黄铁矿(Pn)和黄铜矿(Ccp)包裹体;d.角闪石和希兹硫镍矿(Hwd)包裹体

      Fig.  5.  Solid inclusions in chromite from the mafic rocks in the Beishan area

      图  6  坡北亚带浸染状矿化和脉状团块状矿化(a~e)和红石山亚带的浸染状矿化(f)

      Fig.  6.  Disseminated and vein-type sulfide mineralization in the Pobei sub-belt (a-e) and disseminated sulfide in the Hongshishan sub-belt(f)

      图  7  新疆北山地区不同类型矿石的Pd-Cu/Pd散点图

      坡一和红石山数据分别参考Xue et al.(2016a)Ruan et al.(2020);红星代表原始地幔成分,演化线中斜体数字代表早期熔离硫化物的量(据Wang et al., 2018b)

      Fig.  7.  Plot of Pd vs. Cu/Pd for various sulfide ores in the Beishan area

      图  8  新疆北山“岩浆多期次侵入+硫化物多期次熔离”的镍成矿模式(据Ruan et al., 2020修改)

      Fig.  8.  Model of "multi-stages of magma emplacement and sulfide segregation" for the Ni mineralization in the Beishan area, Xinjiang (modified from Ruan et al., 2020)

      图  9  红石山镁铁-超镁铁质亚带成矿相关元素变化

      Fig.  9.  Plots of mineralized elements in the Hongshishan sub-belt

      图  10  固结指数SI-Al2O3关系图,区分含矿岩体和不含矿岩体

      Fig.  10.  Diagram of Solidification index SI-Al2O3 to discriminate ore bearing and non-bearing intrusions

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    • 收稿日期:  2020-07-30
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