Geochronology, geochemistry and petrogenesis of early Cretaceous Yaocun A-type granite in the Lower Yangtze region
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摘要:
姚村岩体位于下扬子江南造山带东北端,主要由中心相的中粗粒正长花岗岩和边缘相的细粒似斑状正长花岗岩组成。本文对该岩体进行了详细的锆石U-Pb年代学、主量元素、微量元素以及Nd-Hf同位素研究。LA-ICP-MS锆石U-Pb定年表明姚村岩体的形成年龄为(127.6±1.4)Ma,为燕山晚期岩浆活动的产物。岩石地球化学研究表明姚村岩体属于A型花岗岩,具高硅、富铁,锆饱和温度高、轻重稀土分馏明显、富集Rb、Th、U、K、Pb等元素而亏损Ba、Nb、Sr和Ti等元素、铕负异常显著(Eu/Eu*=0.22~0.46)的特点。姚村岩体的全岩εNd(t)值与锆石εHf(t)值分别变化于-6.2~-5.7和-13.9~-5.0,两阶段Nd和Hf同位素模式年龄分别为TDM2(Nd)=1439~1532 Ma和TDM2(Hf)=1508~2062 Ma,Nd同位素的模式年龄重叠于Hf同位素模式年龄。结合区域地质研究成果认为,姚村岩体可能于早白垩世古太平洋板块俯冲作用之后伸展-拉伸环境下,由中元古代地壳重熔而成。
Abstract:The Yaocun pluton in Southern Anhui Province, lithologically consisting mainly of medium-to coarse-grained syenogranite in its centre and fine-grained porphyritic syenogranite on its margin, is outcropped around the northeastern Jiangnan orogeny of the Lower Yangtze region. This paper reports detailed study results of its the LA-ICP-MS zircon U-Pb dating, major elements, trace elements, whole-rock Nd isotopic compositions and zircon Hf isotopic compositions. LA-ICP-MS zircon U-Pb ages show that the Yaocun pluton, as the product of magmatic activity in the late Yanshanian period, was emplaced at 127.6±1.4Ma. The studies of petrography and geochemistry of this rock indicate that it is A-type granite, and is characterized by rich silica, high iron, high zircon saturation temperatures, enrichment of Rb, Th, U, K and Pb, depletion of Ba, Nb, Sr and Ti, and significant negative Eu anomalies (Eu/Eu*=0.22-0.46). Its εNd(t) and εHf(t) values range from -6.2 to -5.7 and from -13.9 to -5.0 respectively, and the calculated two-stage model ages (TDM2) of Nd and Hf isotopes from 1439 Ma to 1532 Ma and from 1508 Ma to 2062 Ma respectively. Combined with the results of regional geological research, it is suggested that the Yaocun pluton might be formed by the Mesoproterozoic crust remelting under extension-tension environment after the subduction of the Paleo-Pacific plate during the Early Cretaceous.
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图 1 大地构造位置图(a)、区域构造略图(b,据陈芳等,2014修改)及岩体地质简图(c)
Figure 1.
图 4 姚村岩体TAS分类图解(a)(据Middlemost, 1994)和K2O-SiO2图解(b)(据Peccerillo et al., 1976)(圆形为中粗粒正长花岗岩,正方形为细粒似斑状正长花岗岩)
Figure 4.
图 6 姚村A型花岗岩判别图解(底图a据Collins et al., 1982;底图b据Frost and Frost, 2011; 底图c和d据Whalen et al., 1987)(图例同图 4)
Figure 6.
图 7 姚村岩体岩浆过程判别图解(a)La-La/Sm图解; (b) Zr-Zr/Nb图解(图例同图 4)
Figure 7.
图 8 姚村岩体源岩判别图解:(a)摩尔Al2O3/(MgO+FeOT)-摩尔CaO/(MgO+FeOT)图解(据Altherr et al., 2000); (b)Al2O3/TiO2-CaO/Na2O图解(据Sylvester., 1998)(图例同图 4)
Figure 8.
图 9 姚村岩体全岩εNd(t)-t图解(a, 双桥山群和溪口岩群全岩Nd同位素据Chen & Jahn, 1998)和锆石εHf(t)-t图解(b,新元古代花岗岩锆石Hf同位素据Zhang & Zheng, 2013; Wang et al., 2013)
Figure 9.
表 1 姚村岩体中粗粒正长花岗岩(8849-1-1)LA-ICP-MS锆石U-Th-Pb同位素分析结果
Table 1. Zircon LA-ICP-MS U–Pb geochronology results in the Yaocun coarse-grained syenogranite
表 2 姚村岩体全岩主量元素(%)、稀土元素和微量元素含量(10-6)
Table 2. The content of main elements (%), rare earth elements and trace elements(10-6) of the Yaocun pluton
表 3 姚村岩体全岩Sr-Nd同位素测试结果
Table 3. Sr-Nd isotope compositions of representative samples from the Yaocun pluton
表 4 姚村岩体(8849-1-1)锆石Hf同位素组成
Table 4. Hf isotopic compositions of zircon grains from the Yaocun pluton determined by LA-MC-ICP-MS
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