| 广东从化佛冈（主体）黑云母花岗岩定年和成因 |
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| 引用本文： | 陈小明,王汝成,刘昌实,胡欢,张文兰,高剑锋.广东从化佛冈（主体）黑云母花岗岩定年和成因[J].高校地质学报,2002,8(3):293-307. |
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| 作者姓名： | 陈小明 王汝成 刘昌实 胡欢 张文兰 高剑锋 |
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| 作者单位： | 南京大学地球科学系内生金属矿床成矿机制研究国家重点实验室，江苏南京210093 |
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| 基金项目： | 国家自然科学基金项目40132010,40073009,40025209资助。 |
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| 摘 要： | 佛冈黑云母花岗岩是大型东西走向的佛冈花岗质杂岩体的主体部分、占杂岩体面积的85％。粗等粒或巨晶斑状结构。由黑云母（2－6％），石英（35－41％），斜长石（An10-23,10-18%)和微纹长石（36－48％）组成，系黑云母花岗岩。黑云母具有低的Mg/(Mg+Fe)值（0.17-0.21)。据全岩－矿物Rb-Sr等时线定年其定位年龄为167.5±7.5Ma，MSWD为2.4(中侏罗世晚期）。在岩石化学成分上为富硅（SiO2在71.74-77.64%)，中等过铝质（A／NKC平均为1.056)，钼碱性－弱亚碱性（NK／A平均为0.797)，相对富K2O（K2O／Na2O为1.66)。在微量元素和稀土元素组成方面，显示Nb亏损，具有低Nb/Ta值（平均5.94)，高Rb/Sr(1.98-41.71)，Rb/Nb(11-23)和K／Nb(1498－2976值）；中－强Eu亏损（Eu/Eu在0.12-0.46)；高的（La/Sm)N值（1.67-5.39)等。在Sr,Nd,Pb,O同位素组成上，具有高的Isr值（0.7116±0.0023)和εSr(t)值（96－103）；低的εNd(t)值（－6.19--8.93)。据模拟计算，其源区岩石中华南上壳端元约占66－69％，高的^207Pb/^204Pb(15.734)和^206Pb/^204Pb值（18．962－19．049）位于铅构造模式图的上壳演化线域内，高δ^18O‰（＋9.3-+12.5)等。以上数据表明佛冈黑云母花岗岩系该区中－下地壳层次的源岩部分熔融而成，与华南S型花岗岩有相似之处。古太平洋板块（向西）与欧亚板块和菲律宾地块（向北）与南中国－印支地块的岩石圈消减作用导致的玄武岩底侵，对黑云母花岗岩的形成有一定的贡献。
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| 关 键 词： | 黑云母 成因 花岗岩 广东 铷－锶等时线定年 |
| 文章编号： | 1006-7493(2002)03-293-08 |
| 修稿时间： | 2002年5月10日 |
Isotopic Dating and Genesis for Fogang Biotite Granites of Conghua Area, Guangdong Province |
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| CHEN Xiao-ming,WANG Ru-cheng,LIU Chang-shi,HU Huan,ZHANG Wen-Ian,GAO Jian-feng.Isotopic Dating and Genesis for Fogang Biotite Granites of Conghua Area, Guangdong Province[J].Geological Journal of China Universities,2002,8(3):293-307. |
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| Authors: | CHEN Xiao-ming WANG Ru-cheng LIU Chang-shi HU Huan ZHANG Wen-Ian GAO Jian-feng |
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| Institution: | Department of Earh Sciences, State Key Laboratary for Mineral Deposits Research, Nanjing University, 210093 |
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| Abstract: | Fogang(main body)biotite granites are a part of large-scaled Fogang granitic complex of east-west trending.They occupy about 85％ of the complex in area.They are composed of about 2～ 6％ biotite,35～ 41％ quartz,10～ 18％ plagioclase (An10—23)and 36～ 48％perthite,corresponding to biotite syenogranite(3a)on the basis of mineral contents by lUGS classification.The biotite has lower Mg／(Mg+Fe )values(0.17-0.21)and the K-feldspar is usually microcline perthite.Fogang biotite granites have an age of 167.5± 7.5Ma(MSWD =2.4),determineted by Rb-Sr whole rock-minera1 isochron method (emplaced during Middle
Jurassic period).Similar to S type granites in south China,Fogang granites are markedly rich in silica(Si02：71.74～77.64％)and K20 relative to Na20 (averaging K2O／Na20=1.66),and are moderately peraluminous (averaging A／NKC = 1.056) and calcic-alkaline to weakly subalkaline series(NK／A=0.797 in average).Based on the trace element and rare earth element data,the granites commonly have higher Rb／Sr(1.98～ 41.71),Rb／Nb(11～23),K/Nb(1498-2976)ratios,lower Nb／Ta ratio(5.94 in average),strong to moderate Eu depletion(Eu／Eu* =0.12～0.46),and higher(La／Sm)N values(1.67～5.39).In Sr,Nd,Pb,O,isotopic composition field,Fogang granites have higher Isr (0.7116±0.0023)and εsr (t)values(96～ 103),showing that South China Upper Crust end member occupies about 66～69％ in their source materials in terms of the model calculation. The granites possess higher δ18O‰(+9.3～ +12.5)and 207Pb／204Pb(15.734)and 206Pb／204Pb(18.968～19.049) indicating that they are consistent with Upper Crust Evolution Line in the Pb-tetonic model diagram.The above mentioned data wholely indicate that Fogang biotite granites were formed by partial melting of source materials consisting of mid to lower crust rocks.Some of dark enclaves of dioritic or granodioritic compositions are found in Fogang biotite granites. This suggests that basalt underplating resulted from lithosphere westward subduction of the Palaeo Pacific plate and northward subduction of the Philippine Block,effected upon the formation of Fogang granites. |
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| Keywords: | granite Rb-Sr isochron Fogang area of Guangdong province |
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