Petrogenesis and Tectonic Setting of Intermediate-Felsic Volcanics in Ta'erqi Area, Central Great Xing'an Range
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摘要: 为探讨大兴安岭中段塔尔气地区中酸性火山岩成因及构造背景，深化大兴安岭中生代火山岩带的对比研究，对该地区满克头鄂博组、白音高老组火山岩开展了锆石U-Pb定年、岩石地球化学及Hf同位素分析.满克头鄂博组年龄为154±2 Ma和154±3 Ma，白音高老组年龄为132±2 Ma.样品富碱质，贫镁和钙，为弱过铝质.富K、Rb、Zr、Hf，贫Eu、Ba、Sr、P、Ti等元素，具有中等到较强的Eu负异常.锆石饱和温度平均值分别为915℃和841℃，表现出A型流纹岩的特点.样品εHf（t）值分别介于+6.9~+8.4和+6.7~+7.9，tDM2分别介于624~670 Ma和611~682 Ma，指示岩浆来源于新元古代亏损地幔增生年轻地壳物质.本地区满克头鄂博组形成于蒙古-鄂霍茨克洋闭合后伸展早期阶段，白音高老组则形成于蒙古-鄂霍茨克洋闭合后岩石圈伸展及拆沉作用，同时受到太平洋板块俯冲引发的弧后伸展作用叠加的影响.Abstract: In order to study the petrogenesis and tectonic setting of intermediate-felsic volcanics in Ta'erqi area, central Great Xing'an Range and promote the comparative study of Mesozoic volcanics in this region, in this paper it presents a synthesis study of zircon U-Pb chronology, geochemistry and Hf isotopes of volcanics from Manketouebo and Baiyingaolao formations. Zircon U-Pb dating yielded weighted mean ages of 154±2 Ma and 154±3 Ma of Manketouebo Formation and 132±2 Ma of Baiyingaolao Formation.The samples are weak peraluminous with high alkali, low Mg and Ca contents, while existing the enrichment of Rb, K, Zr, Hf and depletion of Eu, Sr, Ba, P, Ti with moderate to strong negative Eu anomalies. The average zirconium saturation temperature are 915 ℃ and 841 ℃, respectively, showing the characteristics of A-type rhyolite. The εHf(t) values range from +6.9 to +8.4 and +6.7 to +7.9, while the tDM2 values range from 624 Ma to 670 Ma and 611 Ma to 682 Ma, indicating that the magma originated from the the partial melting of Neoproterozoic young crust accreted from the depleted mantle. Manketouebo Formation in Ta'erqi area formed in the early stage of extensional tectonic setting after the closure of Mongolia-Okhotsk ocean, while Baiyingaolao Formation was caused by the lithosphere extension and delamination after the closure of the Mongolia-Okhotsk Ocean and the back-arc extension induced by the subduction of the paleo-Pacific plate to Eurasia.
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Key words:
- central Great Xing'an Range /
- zircon U-Pb dating /
- Hf isotope /
- A-type rhyolites /
- lithosphere extension /
- deposits
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图 1 工作区构造位置图(a)及工作区区域地质简图(b)
a图中，I.兴蒙造山带; I-1.额尔古纳地块; I-2.兴安地块; I-3.松辽地块; I-4.佳木斯地块; II.华北地块.①新林-喜桂图断裂; ②二连-贺根山断裂; ③西拉沐伦断裂; ④牡丹江断裂
Fig. 1. Tectonic location of study area (a) and simplified geological map of study area (b)
图 2 塔尔气地区满克头鄂博组(J3mk)地质剖面
1.浅灰色流纹质晶屑岩屑凝灰岩；2.紫红色流纹质晶屑岩屑凝灰熔岩；3.浅紫色流纹岩；4.紫灰色流纹质晶屑岩屑角砾凝灰熔岩；5.灰色英安质晶屑凝灰熔岩；6.灰色英安质晶屑熔岩
Fig. 2. Geological section map of Manketouebo Formation (J3mk) in Ta'erqi area
图 3 满克头鄂博组岩石手标本及显微照片
a.浅紫色流纹岩；b.紫红色流纹质晶屑凝灰熔岩；c.紫灰色流纹质晶屑凝灰岩，d.斑状结构；e.晶屑凝灰熔岩结构；f.晶屑凝灰结构；Bt.黑云母；Pl.斜长石；Q.石英；Sa.透长石
Fig. 3. Hand specimen photographs and micro photographs of Manketouebo Formation rock samples
图 4 塔尔气地区白音高老组(J3b)地质剖面
1.灰白色流纹质岩屑晶屑凝灰岩；2灰色流纹质岩屑晶屑角砾凝灰岩；3.灰白色流纹岩；4.浅灰色流纹质晶屑岩屑角砾凝灰熔岩；5.浅灰色流纹质晶屑熔岩；6.灰白色流纹质晶屑凝灰熔岩；7.紫红色流纹质岩屑晶屑角砾凝灰熔岩；8.灰白色流纹岩；9.灰白色流纹质晶屑凝灰岩；10.灰白色球粒流纹岩；11.灰白色流纹岩
Fig. 4. Geological section map of Baiyingaolao Formation (J3b) in Ta'erqi area
图 5 白音高老组岩石手标本及显微照片
a.灰白色流纹岩；b.灰色流纹质岩屑晶屑角砾凝灰岩；c.紫红色流纹质晶屑岩屑角砾凝灰熔岩；d.流纹构造；e.晶屑凝灰结构；f.流纹质岩屑；Bt.黑云母；Pl.斜长石；Q.石英；Sa.透长石
Fig. 5. Hand specimen photographs and micro photographs of Baiyingaolao Formation rock samples
图 6 满克头鄂博组流纹岩锆石阴极发光图像
Fig. 6. CL images of the zircons of rhyolite of Manketouebo Formation
图 7 满克头鄂博组流纹岩锆石U-Pb年龄
a.J3mk-1；b.J3mk-6
Fig. 7. Zircon U-Pb ages of rhyolite of Manketouebo Formation
图 8 白音高老组锆石阴极发光图像(a)及U-Pb谐和曲线图(b)
Fig. 8. CL images of the zircons (a) and zircon U-Pb ages of rhyolite of Baiyingaolao Formation (b)
图 9 样品主量元素图解
a.火山岩TAS图解(据Le Bas and LeMaitre，1986)；b.K2O-SiO2图解(据Peccerillo and Taylor, 1976)；c.Na2O-K2O图解(据Rollinson，1993)；d.A/CNK-A/NK图解(据Maniar and Piccoli, 1989)
Fig. 9. Diagrams of major elements
图 10 满克头鄂博组火山岩稀土元素球粒陨石标准化配分曲线图(a)及微量元素原始地幔标准化蛛网(b)
阴影部分数据张超(2014)
Fig. 10. Chondrite-normalized REE patterns (a) and primitive mantle-normalized trace element spider diagram (b) for the samples of Manketouebo Formation
图 16 蒙古-鄂霍茨克洋俯冲-闭合构造演化
SIB.西伯利亚板块；KAZ.哈萨克斯坦板块；Tar.塔里木板块；NCB.华北板块；XMOB.兴蒙造山带；MOS.蒙古-鄂霍茨克构造带；据Ren et al.(2018)修改
Fig. 16. Mesozoic tectonic evolution of Mongolia-Okhotsk ocean
图 17 蒙古-鄂霍茨克构造域与古太平洋构造域晚中生代演化模式(据许文良等，2019修改)
Fig. 17. Mesozoic tectonic evolution of Mongolia-Okhotsk and paleo-Pacific ocean (modified after Xu et al., 2019)
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