Characteristics and tectonic setting of volcanic rocks of Baiyingaolao Formation in Hanwula of Xi Ujimqin Banner, Inner Mongolia
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摘要:
大兴安岭中生代火山岩的成因和构造背景一直存在争议。内蒙古西乌旗地区发育大面积的晚中生代火山岩，是中国东部巨型火山岩带的重要组成部分。本文对西乌旗罕乌拉地区白音高老组火山岩开展了野外地质、岩石学、锆石U-Pb同位素年代学、地球化学研究，以便对其岩石成因和构造背景给予制约。白音高老组火山岩主要由流纹岩及流纹质火山碎屑岩等一套中酸性火山岩组成。采集其中的球粒流纹岩和英安斑岩进行LA-ICP-MS锆石UPb测年，测年锆石的CL图和Th/U值(0.34~1.25)指示其为岩浆成因锆石，测年结果分别为(140±0.8)Ma和(133±0.7)Ma，表明这套火山岩的形成时代为早白垩世早期。岩石地球化学研究表明，白音高老组火山岩属高钾钙碱性系列，具高硅、富碱、贫镁、钙，高FeOT/MgO比值，低Mg#值、Nb/Ta比值的特征；相对富集轻稀土元素，亏损重稀土元素；大部分样品富集LILE，而亏损Ba、Sr和HFSE，具A型花岗岩地球化学特征，形成于伸展构造背景，为地壳部分熔融的结果。结合区域中生代火山岩的空间展布特征，认为该火山岩形成应与蒙古—鄂霍茨克洋闭合碰撞后伸展和古太平洋板块的俯冲作用有关。
Abstract:There exist different opinions concerning the petrogenesis and tectonic background of Mesozoic volcanic rocks developed in the Da Hinggan Mountains. The Late Mesozoic volcanic rocks in the Xi Ujimqin Banner of Inner Mongoliais a very important part of the huge volcanic rock belt in eastern China.The authors studied the volcanic rocks of Baiyingaolao Formation in Hanwula of Xi Ujimqin Banner in such aspects as field occurrence,petrology,zircon U-Pb isotopic geochronology and geochemisty in order to constrain their petrogenesis and tectonic background. The volcanic rocks of Baiyingaolao Formation are composed of rhyolite and volcanic clastic,which are a set of felsic volcanic rocks. The cathodoluminescence (CL) images of analyzed zircons of the pyromeride and dacite porphyry from Baiyingaolao Formation and their Th/U ratios(0.34-1.25) imply the igneous origin. LA-ICP-MS U-Pb dating shows that their ages are about(140±0.8) Ma and(133±0.7) Ma respectively,suggesting the early period of Early Cretaceous. Petrological and geochemical data reveal that the rocks belong to the high potassium calc-alkaline rock series characterized by rich Si and alkali,poor magnesium and calcium,high FeOT/MgO ratio and low Mg#,Nb/Ta ratio. LREE are richer than HREE.The trace element geochemistry is characterized evidently by enrichment of LILE,depletion of Ba,Sr and HFSE. All these geochemical characteristics of rocks show an affinity with the A-type granites,which were most probably formed in an extensional setting and originated from the partial melting of the crust. Combined with spacial distribution of the Mesozoic volcanic rocks,the authors hold that they were probably related to the post-orogenic extension following the closure of the Mongol-Okhotsk orogen,and were also affected by the subduction of the Paleo-Pacific plate.
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图 1 研究区大地构造位置图(a，据Xiao et al., 2003)及区域地质简图(b)
1—第四系；2—下白垩统白音高老组；3—上侏罗统玛尼吐组；4—上侏罗统满克头鄂博组；5—下二叠统大石寨组；6—下二叠统寿山沟组；7—中元古界锡林浩特岩群；8—早白垩世碱长花岗岩；9—早白垩世花岗斑岩；10—早白垩世英安斑岩；11—早中三叠世侵入岩；12—早二叠世侵入岩；13—不整合接触界线；14—实测断层；15—同位素年龄采样点及编号；16—剖面位置
Figure 1. Regional geological location of the study area (a, after Xiao et al., 2003) and geological sketch map of the study area (b)
1-Quaternary; 2−Lower Cretaceous Baiyingaolao Formation; 3−Upper Jurassic Manitu Formation; 4−Upper Jurassic Manketouebo Formation; 5−Lower Permian Dashizhai Formation; 6−Lower Permian Shoushangou Formation; 7−Middle Proterozoic Xilinhot Group; 8−Early Cretaceous alkali–feldspar granite; 9−Early Cretaceous granite porphyry; 10−Early Cretaceous dacite porphyry; 11−Early–Middle Triassic intrusive rock; 12− Early Permian intrusive rock; 13−Unconformity; 14−Measured fault; 15−Isotopic age sampling position and serial number; 16−Location of section
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图 2 罕乌拉地区白音高老组火山岩实测剖面
1—砾岩；2—砂砾岩；3—粉砂岩；4—凝灰质粉砂岩；5—流纹质凝灰角砾岩；6—流纹质含角砾岩屑晶屑凝灰岩；7—流纹质含角砾岩屑凝灰岩；8—流纹质岩屑晶屑凝灰岩；9—流纹质晶屑凝灰岩；10—流纹质含角砾岩屑晶屑熔结凝灰岩；11—流纹质含角砾熔结凝灰岩；12—流纹质晶屑熔结凝灰岩；13—流纹质熔结凝灰岩；14—流纹岩；15—流纹斑岩；16—英安斑岩；17—不整合界线；18—地质代号；19—同位素年龄采样点及编号；20—产状
Figure 2. Measured geological section of Baiyingaolao Formation in Hanwula
1−Conglomerates; 2−Glutenites; 3−Siltstones; 4−Tuffaceous siltstones; 5−Rhyolitic tuff breccias; 6−Rhyolitic tuffs with breccia lithic and crystal clasts; 7−Rhyolitic tuffs with breccia and lithic clasts; 8−Rhyolitic tuffs with lithic and crystal clasts; 9−Rhyolitic tuffs with crystal clasts; 10−Rhyolitic welded tuffs with breccia lithic and crystal clasts; 11−Rhyolitic welded tuffs with breccia clasts; 12−Rhyolitic welded tuffs with crystal clasts; 13−Rhyolitic welded tuffs; 14−Rhyolite; 15−Rhyolite porphyry; 16−Dacite porphyry; 17−Unconformity; 18−Geological code; 19− Isotopic age sampling position and serial number; 20−Attitude
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图 3 白音高老组火山岩野外及显微照片
a, b—流纹岩; c, d—球粒流纹岩; e, f—流纹质晶屑熔结凝灰岩; g, h—英安斑岩; Q—石英; Pl—斜长石; Kf—钾长石; Bi—黑云母
Figure 3. Field outcrop and microscopic characteristics of Baiyingaolao Formation
a, b-Rhyolite; c, d-Pyromeride; e, f-Rhyolitic welded tuffs with crystal clasts; g, h-Dacite porphyry; Q−Quartz; Pl−Plagioclase; Kf−K-feldspar; Bi−Biotite
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图 4 罕乌拉地区白音高老组球粒流纹岩(Pm27−49)和英安斑岩(B1412)代表性单颗粒锆石阴极发光(CL)图像及其表面年龄(Ma)(a、b)；罕乌拉地区白音高老组球粒流纹岩(Pm27−49)和英安斑岩(B1412)LA−ICP−MS锆石U−Pb年龄谐和图(c、d)
Figure 4. Cathodoluminescence images of typical single−crystal zircons and their apparent ages (Ma) for the pyromeride(Pm27−49) and dacite porphyry (B1412)of Baiyingaolao Formation in Hanwula (a, b); LA−ICP−MS zircon U−Pb concordant age diagram for the pyromeride (Pm27−49) and dacite porphyry (B1412) of Baiyingaolao Formation in Hanwula (c, d)
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图 5 罕乌拉地区白音高老组火山岩SiO2−K2O图解(a)(转引自Rollinson，1993)和Nb/Y−Zr/TiO2分类命名图解(b)(转引自Wilson，1989)
Figure 5. SiO2−K2O diagrams (a, after Rollinson, 1993) and Nb/Y−Zr/TiO2 classifying−naming diagrams (b, after Wilson, 1989) for volcanic rocks of Baiyingaolao Formation in Hanwula
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图 6 罕乌拉地区白音高老组火山岩球粒陨石标准化稀土元素配分图(a)(球粒陨石标准化数据引自Boynton, 1984)和原始地幔标准化蛛网图(b)(原始地幔标准化数据引自Sun and MC Donough., 1989)
下地壳、中地壳据Rudnick et al., 2003；大兴安岭地区白音高老组火山岩数据据苟军等, 2010；Dong et al., 2014；Kong et al., 2014；秦涛等, 2014；聂立军等, 2015；王雄等, 2015；Yang et al., 2015；张乐彤等, 2015；张学斌等, 2015
Figure 6. Chondrite−normalized REE patterns(a)(normalization values after Boynton, 1984) and primitive mantle−normalized trace element spider diagrams (b)(normalization values after Sun and Mc Donough., 1989) for volcanic rocks of Baiyingaolao Formation in Hanwula lower crust, middle Crust(after Rudnick et al., 2003); data of Baiyingaolao Formation in the Da Hinggan Mountains
(after Gou Jun et al., 2010; Dong Yu et al., 2014; Kong Yuanming et al., 2014;Qin Tao et al., 2014; Nie Lijun et al., 2015;Wang Xiong et al., 2015; Yang Wubin et al., 2015;Zhang Letong et al., 2015;Zhang Xuebin et al., 2015)
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图 8 罕乌拉地区白音高老组火山岩10000×Ga/Al−Nb图解(a)和10000×Ga/Al−Zr图解(b)(a、b，据Whalen et al., 1987)
Figure 8. Diagrams of 10000×Ga/Al−Nb (a) and 10000×Ga/Al−Zr (b)(a, b, after Whalen et al., 1987) for volcanic rocks of Baiyingaolao Formation in Hanwula
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表 1 罕乌拉地区白音高老组火山岩球粒流纹岩(Pm27-49)和英安斑岩(B1412)LA-ICP-MS锆石U-Pb同位素分析结果
Table 1 LA-ICP-MS zircon U-Pb isotope analysis results for the pyromeride(Pm27-49) and dacite porphyry(B1412) of Baiyingaolao Formation in Hanwula
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表 2 罕乌拉地区白音高老组火山岩主量元素(%)和微量元素(10–6)分析结果
Table 2 Major(%) and trace element (10–6) analysis results of volcanic rocks of Baiyingaolao Formation in Hanwula
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表 3 大兴安岭地区白音高老组火山岩年龄测定结果
Table 3 The ages of volcanic rocks of Baiyingaolao Formation in Da Hinggan Mountains
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