Geochronology and geochemistry of volcanic rocks in Manketou'ebo Formation of Tulihe area, northern Da Hinggan Mountains
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摘要:
对大兴安岭北段图里河地区满克头鄂博组火山岩进行了锆石U-Pb年代学及岩石地球化学研究，以便对其岩石成因和构造背景给予制约。流纹岩LA-ICP-MS锆石U-Pb定年结果表明，该地区满克头鄂博组火山岩形成时代为晚侏罗世（157±1Ma）。该组火山岩具有高硅（SiO2=69.09%~75.92%）、富碱（K2O+Na2O=8.04%~9.23%），贫镁、铁、钙的特征，属高钾钙碱性、偏铝质-弱过铝质岩石；稀土元素配分曲线呈轻稀土富集的右倾形式，（La/Yb）N=5.85~13.53，无铕异常或具有较弱的铕负异常；火山岩样品富集Rb、Th、U、K等大离子亲石元素，亏损Nb、Ta、Ti等高场强元素。Mg#值为12.14~31.01，平均值22，Nb/Ta值（6.67~27.17，平均值12.23），Rb/Sr值（0.35~3.63，平均值1.58），显示火山岩岩浆源区为下地壳。依据岩石地球化学特征、构造判别图解，结合区域构造演化特征，认为满克头鄂博组火山岩形成于蒙古-鄂霍茨克洋闭合的造山后伸展背景。
Abstract:In this paper, the authors studied the chronology and geochemistry of volcanic rocks in Manketou'ebo Formation of Tulihe area within Da Hinggan Mountains to restrict the petrogenesis and the tectonic setting. Zircon U-Pb dating reveals that the volcanic rocks formed in (157±1) Ma, suggesting late Jurassic. The geochemical characteristics reveal that these rocks fall into the high-K calc-alkaline, metaluminous to slightly peraluminous rhyolite series, characterized by high SiO2 content (69.09%-75.92%), high alkali content (8.04%-9.23%) but low MgO, CaO and Fe2O3 content. The REE patterns reveal that the rocks are enriched in light rare earth elements with significant fractionation of HREE and LREE ((La/Yb)N=5.85-13.53), with no or lightly negative Eu anomaly. Rocks are enriched in LILE such as Rb, Th, U and K, relatively depleted in HFSE such as Nb, Ta and Ti. Mg# ratios vary from 12.14 to 31.01, 22 on average; Nb/Ta ratios vary from 6.67 to 27.17, 12.23 on average; Rb/Sr ratios vary from 0.35 to 3.36, 1.58 on average, implying that the magmatic source was the lower crust. According to the geochemical features, discrimination diagrams of tectonic setting and regional tectonic evolution, the authors hold that the volcanic rocks formed in the post-orogenic extension setting after the closure of Mongol-Okhotsk Ocean.
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Key words:
- Manketou'ebo /
- Mongol-Okhotsk Ocean /
- petrogenesis /
- northern Da Hinggan Mountains /
- Inner Mongolia
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图 3 岩石TAS分类图（据Le Maitre et al, 1989）
Figure 3.
图 4 岩石SiO2-K2O图解(据Peccerillo and Taylor, 1976)
Figure 4.
图 5 岩石稀土元素球粒陨石标准化配分图解（a，标准值据Boynton，1984）和微量元素原始地幔标准化蛛网图（b，标准值据Sun et al., 1989）
Figure 5.
图 8 岩石R1-R2图解（据Batchelor et al，1985）
Figure 8.
图 9 岩石(Y+Nb)-Rb图解（据Pearce等，1984）
Figure 9.
表 1 满克头鄂博组火山岩主量（%）与微量元素（10-6）分析结果
Table 1. Major and trace element compositions of Manketou'ebo volcanic rocks
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表 2 满克头鄂博组流纹岩锆石LA-ICP-MS U-Pb同位素分析结果
Table 2. Zircon isotopic LA-ICP-MS U-Pb analyses for Manketou'ebo rhyolites
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表 3 大兴安岭地区满克头鄂博组火山岩测年结果
Table 3. Ages of Manketou'ebo volcanic rocks of Da Hinggan Mountains
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