LA-ICP-MS zircon U-Pb dating and tectonic setting of the monzogranites in the Fengleishan area of Beishan orogenic belt, Inner Mongolia
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摘要:
风雷山二长花岗岩位于北山北部的红石山—百合山—蓬勃山与芨芨台子—小黄山两条蛇绿混杂岩带之间，构造位置特殊。二长花岗岩LA-ICP-MS锆石U-Pb年龄加权平均值为（320±1）Ma，代表了其成岩年龄。岩石具有富SiO2、Al2O3的特征，里特曼指数（σ）为1.58~2.74（< 3.3），碱度率（AR）为2.35~4.05，属于钙碱性花岗岩类，A/NCK=0.92~1.15，显示出偏铝质、过铝质岩浆的特征。稀土元素总量（ΣREE）较高，稀土配分模式呈轻稀土富集的右倾型[（La/Yb）N=4.60~8.83]，轻稀土分异程度大于重稀土，所有样品均具有Eu负异常（δEu=0.56~0.88，平均为0.72）；强烈富集强不相容元素Th、U和大离子亲石元素Rb、K，亏损高场强元素Nb、Ta、Ti、P。曲线形态与上地壳的相似，表明岩浆作用过程有上地壳物质的参与。高的Th含量（8.58~21.62 μg/g）及低的Nb/Ta值（8.75~15.72）指示岩浆源区主要为地壳。在Rb-（Nb+Y）及R1-R2等构造判别图解中样品大多数落入板块碰撞前火山弧花岗岩区，根据岩石共生组合特征，认为风雷山地区二长花岗岩为碰撞前陆缘弧岩浆作用的产物，与红石山—百合山—蓬勃山有限洋的洋壳俯冲作用有关。结合区域地质背景，推测红石山—百合山—蓬勃山有限大洋的闭合时间应晚于晚石炭世早期。
Abstract:Monzogranites in Fengleishan are located in northern Beishan and situated between two ophiolitic mélange belts of Hongshishan-Baiheshan-Pengboshan and Jijitaizi-Xiaohuangshan, having a special tectonic affinity. Zircons from the monzogranites yielded a weighted mean LA-ICP-MS U-Pb age of (320±1) Ma, representing the intrusion age. The samples are characterized by high content of SiO2 and Al2O3 with Rittmann indexes of 1.58-2.74 (< 3.3) and alkaline ratios of 2.35-4.05, belonging to calc-alkaline granitoids. Their A/NCK values range from 0.92 to 1.15 and display metaaluminous to peraalmuinous affinities. They have relatively high content of total REE and are characterized by LREE-enriched patterns ((La/Yb)N=4.60-8.83)and negative Eu anomalies (δEu=0.56-0.88, 0.72 in average). They also show strong enrichment of incompatible elements (e.g., Th and U) and large ion lithophile elements (e.g., Rb and K) but depletion of high field strength elements (e.g., Nb, Ta, Ti and P). Their normalized patterns are similar to those of upper continental crust (UPC), indicating participation of materials from the UPC in their magma source. High values of Th (8.58-21.62 μg/g) and low ratios of Nb/Ta (8.75-15.72) point to a crust-dominated magma source. On the tectonic discriminant diagrams of Rb-(Nb+Y) and R1-R2, most of the samples are plotted in the pre-collisional volcanic arc granite area. Based on associated lithological characteristics, it is proposed that monzogranites in the Fengleishan were formed by pre-collisional volcanic arc magmatism, which was related to oceanic crust subduction in the Hongshishan-Baiheshan-Pengboshan belt. Combined with regional geological background, it is inferred that the closure of the small ocean in the Hongshishan-Baiheshan-Pengboshan belt should postdate the early period of late Carboniferous.
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图 5 AFM图解和A/CNK-A/NK图解(据Irvine and Barage, 1971; Peccerillo and Taylor, 1976; Maniar and Piccoli, 1989)
Figure 5.
图 6 北山风雷山二长花岗岩的稀土元素球粒陨石标准化配分型式(a)和微量元素原始地幔蛛标准化蛛网图(b)(据Sun and McDonough, 1989)
Figure 6.
图 7 (Na2O+K2O)/CaO-(Zr+Nb+Ce)+Y图(据Whalen et al., 1987)及SiO2-P2O5图解(据Chappell and White, 1992)
Figure 7.
图 8 北山风雷山二长花岗岩的构造环境判别图解(据Pearce et al., 1984; Batchelor and Bowden, 1985)
Figure 8.
表 1 北山风雷山二长花岗岩LA-ICP-MS锆石U-Pb同位素测年数据
Table 1. LA-ICP-MS zircon U-Pb isotopic data of monzogranites in Fengleishan, Beishan
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表 2 北山风雷山二长花岗岩主量元素(%)和微量元素(10-6)组成
Table 2. Major(%) and trace elements(10-6) content of monzogranites in Fengleishan, Beishan
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