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    吉林老虎山火山区中新世碱玄岩成因及其构造意义

    叶希青 徐智涛 孙立影 李忠伟 李萌萌 贾琳

    叶希青, 徐智涛, 孙立影, 李忠伟, 李萌萌, 贾琳, 2024. 吉林老虎山火山区中新世碱玄岩成因及其构造意义. 地球科学, 49(4): 1352-1366. doi: 10.3799/dqkx.2022.294
    引用本文: 叶希青, 徐智涛, 孙立影, 李忠伟, 李萌萌, 贾琳, 2024. 吉林老虎山火山区中新世碱玄岩成因及其构造意义. 地球科学, 49(4): 1352-1366. doi: 10.3799/dqkx.2022.294
    Ye Xiqing, Xu Zhitao, Sun Liying, Li Zhongwei, Li Mengmeng, Jia Lin, 2024. Genesis and Tectonic Significance of Miocene Tephrite in Laohushan Volcanic Area, Jilin Province. Earth Science, 49(4): 1352-1366. doi: 10.3799/dqkx.2022.294
    Citation: Ye Xiqing, Xu Zhitao, Sun Liying, Li Zhongwei, Li Mengmeng, Jia Lin, 2024. Genesis and Tectonic Significance of Miocene Tephrite in Laohushan Volcanic Area, Jilin Province. Earth Science, 49(4): 1352-1366. doi: 10.3799/dqkx.2022.294

    吉林老虎山火山区中新世碱玄岩成因及其构造意义

    doi: 10.3799/dqkx.2022.294
    基金项目: 

    中国地震局地质研究所国家野外科学观测研究站项目 NORSCBS22-06

    吉林省地震局青年科技发展课题 JZQ-202402

    中国地震局地震科技星火计划攻关项目 XH23013B

    详细信息
      作者简介:

      叶希青(1995-),女,硕士,主要从事地球化学研究.ORCID:0000-0002-7390-3708. E-mail:yxq0326@126.com

      通讯作者:

      徐智涛,E-mail:xuzhjtao@163.com

    • 中图分类号: P59

    Genesis and Tectonic Significance of Miocene Tephrite in Laohushan Volcanic Area, Jilin Province

    • 摘要: 老虎山单成因火山位于吉林省大口钦地区.为了探讨火山区中新世碱玄岩的地球化学特征、成因及其与区域断裂构造演化的耦合性,对其开展了全岩地球化学和Pb同位素研究.碱玄岩中Na2O/K2O=1.30~1.38,A/CNK值(0.97~1.09)偏低,Mg#值(58.05~61.11)偏高,富集Th、U、Nb等高场强元素(HFSEs),相对弱富集Rb、Ba、K等大离子亲石元素(LILEs),LREE/HREE=10.66~11.32,206Pb/204Pb、207Pb/204Pb和208Pb/204Pb值范围分别为17.661~17.675、15.451~15.457和37.652~37.692.成岩岩浆主要来源于软流圈地幔,混有少量俯冲洋壳物质,显示出OIB或板内交代富集型地幔源的属性,岩浆形成深度范围约在93~105 km,伊通-舒兰断裂的存在为火山深部岩浆的上升与裂隙式喷发提供了通道和空间,玄武质岩浆的形成及其对应的火山活动发生于伸展构造环境中.

       

    • 图  1  吉林省伊通-舒兰断裂带火山群位置简图(a)、中国东北部地区中-新生代地质构造简图(b)和大口钦老虎山火山区地质简图(c)

      图a据Sun et al.(2022)修改;图b据Sun et al.(2022)修改;图c据吉林省地质矿产局(1988)修改

      Fig.  1.  Overview of the location of volcanic groups in Yitong-Shulan fault zone, Jilin Province (a), Mesozoic-Cenozoic geotectonic map of Northeast China (b) and geological map of the Laohushan volcanic area in Dakouqin (c)

      图  2  老虎山火山野外图像(a)、碱玄岩的野外产状图像(b)、碱玄岩的手标本图像(c)、碱玄岩镜下矿物组成(d~e)

      Chal.玉髓;Pl.斜长石;Ol.橄榄石;Opx.斜方辉石

      Fig.  2.  Field occurrence image of the Laohushan volcano in the study area (a), field occurrence image of tephrite (b), hand specimen image of tephrite (c), main rock-forming minerals of tephrite under microscope (d-e)

      图  3  老虎山火山区碱玄岩TAS图解(a)、SiO2-Zr/TiO2图解(b)、K2O-Na2O图解(c)和A/NK-A/CNK图解(d)

      图a和图b底图据赵振华(2016)修改;图c和图d底图据Middlemost(1985)修改

      Fig.  3.  TAS diagram (a), SiO2 versus Zr/TiO2 diagrams (b), K2O versus Na2O diagrams (c) and A/NK versus A/CNK diagrams (d) of tephrites in the Laohushan volcanic area

      图  4  老虎山碱玄岩原始地幔标准化微量元素蜘网图(a)和稀土元素球粒陨石标准化配分模式图(b)

      图a元素标准化值据Sun and McDonough(1989);图b元素标准化值据赵振华(2016);洋岛玄武岩(OIB)和洋中脊玄武岩(MORB)值赵振华(2016)

      Fig.  4.  Primitive mantle-normalized trace element spider diagram (a) and chondrite-normalized REE patterns (b) from tephrites in the Laohushan volcanic area

      图  5  老虎山碱玄岩全岩中207Pb/204Pb与206Pb/204Pb铅同位素图解(a)和206Pb/204Pb与208Pb/204Pb铅同位素图解(b)

      底图据Zartman and Doe(1981)修改

      Fig.  5.  207Pb / 204Pb and 206Pb / 204Pb isotopic diagram (a) and 206Pb / 204Pb and 208Pb / 204Pb isotopic diagram (b) in the whole rock of tephrites in the Laohushan volcanic area

      图  6  长白山火山区及邻区晚新生代火山岩年龄频次

      年龄为汇总的长白山火山区及邻区晚新生代火山岩的K-Ar、40Ar-39Ar、14C和锆石U-Pb测年结果,阴影区域为不同年龄的分布数量,曲线为频次趋势线.底图据Li et al.(2021)修改

      Fig.  6.  Age frequency of Late Cenozoic volcanic rocks in Changbai Mountain volcanic area and its adjacent areas

      图  7  Na2O+K2O-δEu图解(a)、Ba/La-Ba/Nb图解(b)、La/Ba-La/Nb图解(c)、Ba/Th-La/Sm图解(d)、Th/Hf -Ta/Hf图解(e)、Th/Yb-Ta/Yb图解(f)

      图e中:I.板块发散边缘N-MORB区; II.板块汇聚边缘; III.大洋板内洋岛及大洋中脊玄武岩区; IV1.陆内裂谷及陆缘裂谷拉斑玄武岩区; IV2.陆内裂谷碱性玄武岩区; IV3.大陆拉张带玄武岩区; V.地幔热柱玄武岩区; 图f:中ICA.岛弧钙碱性系列; SHO.橄榄玄武粗面质; TH.拉斑系列; E-MORB.富集大洋玄武岩; N-MORB.正常大洋玄武岩; OIB.洋岛玄武岩.底图据赵振华(2016)修改

      Fig.  7.  Na2O+K2O versus δEu diagram (a), Ba/La versus Ba/Nb diagram (b), La/Ba versus La/Nb diagram (c), Ba/Th versus La/Sm diagram (d), Th/Hf versus Ta/Hf diagram (e), Th/Yb versus Ta/Yb diagram (f)

      图  8  Ni-Cr图解

      底图据Tsuchiya et al.(2005)修改

      Fig.  8.  Cr versus Ni diagram

      图  9  伊通-舒兰断裂带31~9 Ma岩石圈深部壳幔结构图(a)和(b)Na/Ti-Sm/Yb图解(b)

      图a底图据张辉煌等(2006)修改;图b底图据赵振华(2016)修改

      Fig.  9.  Deep crust mantle structure of 31-9 Ma lithosphere of Yitong-Shulan fault (a) and Na/Ti versus Sm/Yb diagram (b)

      表  1  老虎山碱玄岩全岩Pb同位素组成

      Table  1.   Lead isotopic composition of tephrite in the Laohushan volcano

      样品编号 岩性 206Pb/204Pb 208Pb/204Pb 207Pb/204Pb Δβ Δγ
      Jhly05a 碱玄岩 17.675 0.003 37.692 0.007 15.457 0.003 8.1 6.5
      Jhly05b 碱玄岩 17.661 0.004 37.654 0.010 15.454 0.004 7.9 5.5
      Jhly05c 碱玄岩 17.665 0.005 37.652 0.011 15.451 0.004 7.7 5.4
      注:Δβ和Δγ的具体含义和计算方法据朱炳泉(1998),分别表示样品的207Pb/204Pb和208Pb/204Pb相对于同时代地幔的偏差值.Δβ= [βs(t)/βm(t)-1]×1 000,Δγ= [γs(t)/γm(t)-1]×1 000,β= 207Pb/204Pb,γ= 208Pb/204Pb,s表示样品,m表示地幔,t为样品形成时代.关于不同时代地幔Pb同位素组成计算采用地幔增长线公式,即取地幔μ值为7.8,232Th/238U = 4.04,地球年龄取4.57 Ga,原始Pb同位素组成取206Pb/204Pb = 9.307,207Pb/204Pb = 10.294,208Pb/204Pb = 29.476.
      下载: 导出CSV
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