Magnetic fabric evidences for the Late Paleoproterozoic mafic dyke swarm emplacement, southern margin of the North China craton
-
摘要: 华北克拉通南缘的中条山及邻区广泛发育元古宙放射状基性岩墙群,与五台山-恒山和大同地区的北北西向基性岩墙群以及熊耳中条拗拉谷的火山岩在时空分布和地球化学方面均具有密切的相关性。中条山及邻区放射状基性岩墙群的宏观和微观流动构造(包括捕虏体、冲痕构造、矿物线理和定向斑晶)指示岩墙群以一定的仰角向北西侵位。通过该区岩墙群磁化率各向异性(AMS)测量得到磁组构的最大磁化率长轴优势方位分布图和磁组构各向异性特征分析进一步指示华北南缘古元古代末岩墙群从熊耳中条拗拉谷的底部向北西侵位。岩墙群的流动构造和磁组构的统计成果夯实了华北克拉通古元古代末基性岩墙群与熊耳中条拗拉谷的成生联系。Abstract: In the time-space and geochemistry, the radiating Proterozoic mafic dyke swarms in the Mt. Zhongtiao are related to the mafic dyke swarms in the Mt. Wutai-Hengshan, and both of the mafic dyke swarms are related to the Xiong'er volcanic rocks in the Xiong'er-Zhongtiao aulacogen. The macro and micro flow structures (including xenolithes, scours, mineral lineations and orientation of phenocrystals) in the radiating mafic dyke swarms of the Mt. Zhongtiao indicate that the mafic dyke swarm emplaced from SE to NW at an angle. Based on measurement of the anisotropy of magnetic susceptibility (AMS), the dominant orientations of the maximum magnetic susceptilbility and analysis of susceptibility characteristics also indicate that the mafic dyke swarm emplaced from SE to NW from the bottom of the Xiong'er-Zhongtiao aulacogen, and further support that the Late Paleoproterozoic mafic dyke swarms in the North China craton are much related to the Xiong'er-Zhongtiao aulacogen.
-
Key words:
- North China craton /
- Mafic dyke swarms /
- Flow structures /
- Magnetic fabrics /
- Mechanism of emplacement
-
[1] Callot JP,Geoffroy L,Aubourg C,Magma flow directions of shallow dykes from the East Greenland volcanic margin inferred from magnetic fabric studies,Tectonophysics,2001.
[2] Callot JP,Guichet X,Rock texture and magnetic lineation in dykes:A simple analytical model,Tectonophysics,2003(3-4).
[3] Ernst RE,Baragar WRA,Evidence from magnetic fabric for the flow pattern of magma in the Mackenzie giant radiating dyke swarm,Nature,1992.
[4] Halls HC,Mafic dyke swarms and rifling.,Special Paper 34,Geological Association of Canada Special Paper,1987.
[5] Halls HC,Li JH,Davis D,A precisely dated Preterozoic palaeomagnetic pole from the NCC,and its relevance to palaeocontinental reconstruction,Geophysical Journal International,2000.
[6] Hou GT,Qian XL,The.magnetic fabric evidence of Late Prcambrian mafic dyke swarms emplacement,Shanxi,Shanai Geology,1992(4).
[7] Hou GT,Li JH,Qian XL,Geochemical characteristics and tectonic setting of Mesoproterozoic dyke swarms in northern Shanxi,Acta Petrologica Sinica,2001(3).
[8] Hou GT,Qian XL,Li JH,The simulation of Mesoproterozoic tectonic stress field forming mafic dyke swarms in the central North China craton,Acta Scientiarum Naturalium Universitatis Pekinensis,2002.
[9] Hou GT,Li JH,Halls HC,The flow structures and mechanics of Late Prccambrian mafic dyke swarms in North China raton,Acta Geclogica Sinica,2003(2).
[10] Hou GT,Li JH,Jin AW,Qian XL,Precambrian mafic dyke swarm in the western Shandong Province,Aca Geologica Sinica,2005(2).
[11] Hou GT,la JH,Qian XL,The Late Paleoproterozoic extension events:Aulacogens and dyke swarms,Progress in Natural Science,2006(2).
[12] Hou GT,Wang CC,Li JH,The Paleoproterosoic extension and reconstruction of paleostress field of the North China Craton,Tectonophysics,2006.
[13] Hou GT,Li JH,Yang MH,Geochemical constraints on the tectonic environment of the Late Paleoproterozoic mafic dyke swarms in the North China Craton,Gondwana Research,2008(1).
[14] Hou GT,Santosh M,Qian XL,Configuration of the Late Paleoproterozoic supercontinent Columbia:Insights from radiating mafic dyke swarms,Gondwana Research,2008.
[15] Hou GT,Santosh M,Qian XL,Tectonic constraints on 1.3~1.2Ga final breakup of Columbia supercontinent from a giant radiating dyke swarm,Gondwana Resarch,2008.
[16] Hu JL,Petrogenesis and tectonic setting of the ca.1.75 Ga mafic dyke swarms in the Mt.Zhongtiao and Mt.Songshan areas,北京:中国科学院研究生院,2007.
[17] Knsky TM,Li JH,Paleoproterozoic tectonic evolution of the North China Craton,Journal of Asian Earth Sciences,2003.
[18] Liss D,Hutton DHW,Owens WH,Ropy flow structures:A neglected indicator of magma-flow direction in sills and dikes,Geology,2002(8).
[19] Peng P,Zhai MG,Zhang HF,Zhao TP and Ni ZY,Geochemistry and geological significance of the 1.8 Ga mafic dyke swarms in the North China craton:an example from the juncture of Shanxi,Hebei and Inner-Mongolia,Acta Petrologica Sinica,2004(3).
[20] Peng P,Zhai MG,Zhang HF,Guo JH,Geochronological constraints on the paleoproterozoic evolution of the North China craton:SHRIMP zircon age of different type of mafic dykes,International Geology Review,2005.
[21] Peng P,Zhai MG,Guo JH,Knsky Tand Zhao TP,Nature of mantle source contributions and crystal differentiation in the petrogenesis of the 1.78 Ga mafic dykes in the central North China craton,Gondwana Research,2007.
[22] Peng P,Zhai MG,Ernst R,Guo JH,Liu F and Hu B,A 1.78 Ga large igneous province in the North China craton:The Xiong\'er volcanic province and the North China dyke swarm,lathes,2008.
[23] Qian XL,Chen YP,Late Precambrian mafic dyke swarms of the North China Craton.Special Paper 34,Geological Association of Canada Special Paper,1987.
[24] Tarling DH,Principle and Application of Paleomagnetism,北京:科学出版社,1978.
[25] Wang Y,Fan W,Zhang Y,Geochemical,~(40)Ar/~(39) Ar geochronological and Sr-Nd isotopic constraints on the origin of Paleoproterozoic mafic dikes from the southern Taihang Mountains and implications for the ca.1800 Ma event of the North China Craton,Precambrian Research,2004.
[26] Zhang C,Hon GT,Qian XL,Magnetic gabbroic evidence of the style of emplacement of Late Precambrian mafic dyke swarms in the Luliang-northern Shanxi region,North China,Geologcial Review,1994.
[27] Zhao GC,Wilde SA,Cawood PA,Archean blocks and their boundaries in the North China Craton:Lithological,geochemical,structural and P-T path constraints and tectonic evolution,Precambrian Research,2001.
[28] Zhao TP,Zhou MF,Zhai MG,Paleoproterozoic rift-related volcanism of the Xiong\'er Group,North China Craton:Implications for the breakup of Columbia,International Geology Review,2002.
[29] Zhao TP,Jin CW,Zhai MG,Xia B Zhou MF,The geochemical characteristics and petrogenesis of Xiong\'er Group volcanic in the southern margin of the North China craton,Acta Petrologica Sinica,2002.
[30] Zhao TP,Zhai MG,Xia B,Zircon SHRIMP chronology of Xiong\'er Group volcanics:Constraint on the initial time of the North China craton cover layers,Chinese Science Bulletin,2004(22).
[31] Zhao TP,Xu YH,Zhai MG,Petrogenesis and tectonic setting of the Paleoproterozoic Xiong\'er Group in the southern part of the North China Craton:A review,Geological Journal of Chins Univemities,2007(2).
[32] 侯贵廷,钱祥麟,山西基性岩墙群侵位的磁组构证据,山西地质,1992(4).
[33] 侯贵廷.李江海.钱祥麟 晋北地区中元古代岩墙群的地球化学特征和大地构造背景 [J].-岩石学报2001(3)
[34] 侯贵廷,钱祥麟,李江海,华北克拉通中元古代岩墙群形成的构造应力场数值模拟,北京大学学报(自然科学版),2002.
[35] 侯贵廷.李江海.H C HALLS.钱祥麟 华北晚前寒武纪镁铁质岩墙群的流动构造及侵位机制 [J].-地质学报2003(2)
[36] 侯贵廷.李江海.金爱文.钱祥麟 鲁西前寒武纪基性岩墙群 [J].-地质学报2005(2)
[37] 胡俊良,中条山-嵩山地区ca.1.75 Ga基性岩墙群的成因与构造环境,北京:中国科学院研究生院,2007.
[38] 彭澎.翟明国.张华锋.赵太平.倪志耀 华北克拉通1.8Ga镁铁质岩墙群的地球化学特征及其地质意义:以晋冀蒙交界地区为例 [J].-岩石学报2004(3)
[39] 塔林,古地磁学原理和应用,北京:科学出版社,1978.
[40] 张臣.侯贵廷.钱祥麟 吕梁-晋北地区晚前寒武纪镁铁质岩墙群侵位方式的磁组构证据 [J].-地质论评1994(3)
[41] 赵太平.金成伟.翟明国.夏斌.周美夫 华北陆块南部熊耳群火山岩的地球化学特征与成因 [J].-岩石学报2002(1)
[42] 赵太平.翟明国.夏斌.李惠民.张毅星.万渝生 熊耳群火山岩锆石SHRIMP年代学研究:对华北克拉通盖层发育初始时间的制约 [J].-科学通报2004(22)
[43] 赵太平.徐勇航.翟明国 华北陆块南部元古宙熊耳群火山岩的成因与构造环境:事实与争议 [J].-高校地质学报2007(2)
计量
- 文章访问数: 7775
- PDF下载数: 5084
- 施引文献: 0