内蒙古北山地区标山一带早志留世花岗岩地球化学特征及构造意义
Geochemical Characteristics of Early Silurian Granite from Biaoshan Area in Beishan, Inner Mongolia and Their Tectonic Implications
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摘要: 通过内蒙古标山一带区域地质矿产调查,查明该区早志留世侵入岩由早到晚依次为花岗闪长岩、二长花岗岩和正长花岗岩。该期侵入体为钙碱性岩系,准铝质岩石,SiO2、K2O具正相关变化特征。三者球粒陨石标准化稀土配分曲线均具Eu负异常(δEu值分别为0.60~1.06,0.44~0.81,0.12~0.39)。原始地幔标准化蛛网图显示中等不相容元素La、Ce、Sm、Hf、Zr及强不相容元素Rb、Th、U相对富集,高场强元素Nb、Ta、P、Ti相对亏损。在花岗闪长岩、二长花岗岩、正长花岗岩中获得LA-ICP-MS锆石U-Pb同位素年龄值分别为(444±12)Ma、(441.2±1.8)Ma、(441.1±3.3)Ma,代表该期侵入体就位时代为早志留世。综合前人及本次项目研究成果可见,标山一带早志留世侵入岩就位于岛弧的构造环境。区域上早志留世古亚洲洋壳沿红柳河—月牙山—洗肠井一线向北强烈俯冲,导致本区早志留世深成岩侵位,形成石头井-化石山早古生代岩浆弧。Abstract: 1:50000 geological mapping (Regional geology and mineral resources survey project)indicate that the Early Silurian intrusion in Biaoshan area are dominated by granodiorite, adamellite and syenite granite from early to late in the order.This episode of intrusion is characterized by calc-alkalic rocks, which were interpreted as quasi aluminum rock with evidence of positive SiO2-K2O relationship.Rare earth chondrite standardized distribution of these three types of rocks are shown as europium negative anomaly (with δEu value of 0.60~1.06,0.44~0.81,0.12~0.39, respectively).Standardization of the primitive mantle spider diagram shows relatively enrichment of medium incompatible element (La, Ce, Sm, Hf, Zr)and strong incompatible element (Rb, Th, U), while they have relatively deficient of high field strength elements (Nb, Ta, P, Ti). Granodiorite, adamellite and syenite granite have yielded the zircon LA-ICP-MS ages of (444±12)Ma, (441.2±1.8)Ma and (441.1±3.3)Ma respectively, which represent Early Silurian emplacement.Combined with previous studies, the geochemical data suggests that these Early Silurian intrusions had emplaced in the island arc tectonic setting.Regionally, strong northward subduction has been occurred along the Hongliuhe-Yueyashan-Xichangjng area in the Early Silurian, leading to the emplacement of these intrusions, which formed the early Paleozoic magmatic arc.
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Key words:
- Early Silurian /
- intrusion /
- geochemistry /
- island arc /
- magmatic arc
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何世平,周会武,任秉琛,等.甘肃内蒙古北山地区构造单元划分[J].西北地质,2002,35(4):30-39.
HE Shiping,ZHOU Huiwu,REN Bingchen,et al.The division of tectonic units of Beishan area,Gansu and Inner Mongolia[J].Northwestern Geology,2002,35(4):30-39.
杨合群,赵国斌,李英,等.新疆-甘肃-内蒙古衔接区古生代构造背景与成矿的关系[J].地质通报,2012,31(2-3):413-421.
YANG Hequn,ZHAO Guobin,LI Ying,et al.The relationship between paleozoic tectonic setting and mineralization in Xinjiang-Gansu-Inner Mongolia juncture area[J]. Geoloical Bulletin of China,2012,31(2-3):413-421.
胡醒民,廖云峰,程海峰,等.内蒙古月牙山一带基性火山岩的地质特征、形成时代及归属[J].地质通报,2016,35(8):1234-1242.
HU Xingmin,LIAO Yunfeng,CHENG Haifeng,et al.A discussion on the geological characteristics,formation age and attribution of basic volcanic rocks in Yueyashan area,Inner Mongolia[J].Geoloical Bulletin of China,2016,35(8):1234-1242.
胡新茁,赵国春,胡新悦,等.内蒙古北山地区月牙山蛇绿质构造混杂岩带地质特征、形成时代及大地构造意义[J].地质通报,2015, 34(2-3):425-436.
HU Xinzhuo,ZHAO Guochun,HU Xinyue,et al.geological characteristics,formation epoch and geotectonic significance of the Yueyashan ophiolitic tectonic mélange in Beishan area,Inner Mongolia[J].Geoloical Bulletin of China,2015,34(2-3):425-436.
徐克勤,孙鼐,王德滋,等.华南花岗岩成因与成矿[D].南京:南京大学,1983:6-7.
XU Keqin,SUN Nai,WANG Dezi,et al.The genetic and metallogenic of granite in South of China[J].Nanjing:Nanjing University of Geology,1983:6-7.
刘英俊,曹励明,李兆麟,等.元素地球化学[M].北京:科技出版社,1984.
LIU Yingjun,CAO Liming,LI Zhaolin,et al.geochemistry of element[M].Beijing:A Science and Technology Publishing House,1984.
刘威,魏启荣,车越新.内蒙古石板井公婆泉组火山岩地球化学特征及构造意义[J].科学技术与工程,2015,15(17):18-22.
LIU Wei,WEI Qirong,CHE Yuexin.Geochemistry and Tectonic Significance of Gongpoquan Group in Shibanjing,Inner Mongolia[J].Science Technology and Engineering,2015,15(17):18-22.
WHRIGHT J B.A simple alkalinity Ratio and its application to question of non-orogenic granite genesis[J].Geol.Mag,1969,106(4):370-380.
MANIAR P D and PICCOLI P M.Tectonic discrimination of granitoids[J].GSA.Bull.,1989,101:635-643.
CORYELL,C.D.,J.W.Chase and J.W.Winchester.A procedure for geochemical interpretation of terrestrial rare-earth abundance patterns[J].Geophys.Res.,1963,68,559-566.
WOOD.D.A.A variably veined suboceanic upper mantle genetic significance for mid-ocean ridge basalts from geochemical evidence[J].Geologu,1979,v.7, 499-503.
GORTON,M.P.,SCHANDL,E.V.From Continents to Island Arcs;A Geochemical Index of Tectonic Setting for Arc-Related and Within-Plate Felsic to Intermediate Volcanic Rocks[J].Canadian Mineralogist,2000,38(5):1065-1073.
PEARCE J A,HARRIS B W, TINDLE A G.Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J].Journal of Petroleum Geology,1984,25(4):956-983.
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