Zircon U-Pb dating and petrogenesis of the Early Jurassic rhyolite in Badaguan area, northern Da Hinggan Mountains
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摘要:
大兴安岭北段八大关地区首次发现早侏罗世火山岩，该类岩石主要由流纹岩组成，含少量英安岩和流纹质凝灰岩，LA-ICPMS锆石U-Pb定年结果显示其形成于185~190 Ma，岩石地球化学研究表明，流纹岩具有高硅富碱，贫镁钙和高FeOT/MgO比值的特征，属于高钾钙碱性系列；稀土总量不高（ΣREE=103.80×10-6~194.31×10-6），轻重稀土分馏较明显（（La/Yb）N=7.12~10.22），中等负Eu异常（δEu=0.34~0.74），微量元素以富集Rb、Ba、Th、U、K和LREE，强烈亏损Sr、P、Ti，相对亏损Nb、Ta为特征，显示地壳来源，结合较低的Ga/Al比值，该区流纹岩具有Ⅰ型花岗岩特点，在（Y+Nb）-Rb和（Yb+Ta）-Rb判别图解上显示其形成于活动大陆边缘环境。综合研究表明，八大关地区早侏罗世之前为活动陆缘环境，蒙古—鄂霍茨克大洋板块向额尔古纳地块之下俯冲。
Abstract:The newly-discovered Early Jurassic rhyolite in Badaguan area of Da Hinggan Mountains is of great significance in investigating the tectonic evolution history of Northeast China. The rocks are mainly composed of rhyolites, with a small amount of dacitic and rhyolitic tuffs. LA-ICPMS shows the rhyolites were formed in Early Jurassic, and their formation ages range from 185 Ma to 190 Ma. Geochemical studies show that the rhyolites are characterized by rich silicon and alkalis, poor calcium and magnesium and high FeOT/MgO ratios. Hence the rhyolites belong to high-potassium calc-alkaline rocks. All samples have the similar characteristics of REE patterns, which are characterized by relatively poor total REE content (∑REE=103.80×10-6-194.31×10-6), significant fractionation of HREE and REE[(La/Yb)]N=7.12-10.22) and moderate Eu negative anomalies (δEu=0.34-0.74). The rhyolites are characterized by enrichment of Rb, Th, U, K and LREE, strong depletion of Ba, Sr and HFSE (e.g., Nb, Ta, P and Ti), and relative loss of Nb, Ta. The relatively low Ga/Al ratios indicate that the rhyolites are Ⅰ-type granites of high differentiation. The discrimination diagrams of (Y+Nb)-Rb and (Yb+Ta)-Rb show that the rhyolites were formed on the active continental margin. The comprehensive studies show that the Badaguan area was located on an active continental margin before Early Jurassic, which was affected by the subduction of Mongol-Okhotsk plate towards metamorphic rocks in the Erguna Block.
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Keywords:
- Early Jurassic /
- rhyolite /
- zircon U-Pb dating /
- petrogenesis /
- tectonic setting /
- Badaguan area
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致谢: 衷心感谢核工业二四〇研究所、审稿专家及编辑老师在论文撰写和修改的过程中给予的大力支持与帮助。注释❶核工业二四〇研究所.2015.1:5万八大关牧场等六幅区域地质调查报告[R].
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图 1 八大关地区早侏罗世流纹岩地质简图❶
Figure 1. Sketch geological map of Early Jurassic rhyolite in Badaguan❶
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图 2 八大关地区流纹岩野外和显微照片
a, b—流纹岩野外露头; c—硅化流纹岩; d—球粒流纹岩Kfs—钾长石; Qtz—石英
Figure 2. Field and microstructure photographs of the rhyolite e in Badagua
a, b-Rhyolite outcrop; c-Silicified rhyolite; d-Pyromeride Kfs-Orchoclase; Qtz-Quartz
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图 3 八大关地区流纹岩中部分锆石CL图像和年龄值
Figure 3. Representative CL images and ages of zircons from rhyolite in Badaguan
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图 4 八大关地区流纹岩石锆石U-Pb年龄谐和图
Figure 4. Zircon U-Pb concordia diagrams for the rhyolite in Badaguan
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图 5 八大关地区早侏罗世流纹岩K2O-SiO2与A/CNK-A/NK图解
Figure 5. SiO2-K2O and A/CNK-A/NK diagrams of the Early Jurassic rhyolite of Badaguan
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图 6 八大关地区流纹岩TAS分类图
Pc—苦橄玄武岩; B—玄武岩; O1—玄武安山岩; O2—安山岩; O3—英安岩; R—流纹岩; S1—粗面玄武岩; S2—玄武质粗面安山岩; S3—粗面安山岩; T—粗面岩、粗面英安岩; F—副长石岩; U1—碱玄岩、碧玄岩; U2—响岩质碱玄岩; U3—碱玄岩
Figure 6. TAS diagram of rhyolite in Badaguan
Pc-Picrite; B-Basalt; O1-Basaltic andesite; O2-Andesite; O3-Dacite; O3-Rhyolite; S1-Trachybasalt; S2-Basaltic trachyandesite; S3-Trachyandesite; T-Trachyte、Trachydacite; F-Secondary feldspar; U1-Tephrite, asanite; U2-Phonolitic basalt; U3-Basanite
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图 7 八大关地区花岗岩稀土元素配分模式图和微量元素蛛网图
Figure 7. Chondrite-normalized REE pattern and primitive mantle-normalized spidergram of Early Jurassic rhyolite from Badaguan
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图 8 八大关地区流纹岩SiO2-P2O5相关关系图
Figure 8. P2O5 versus SiO2 variation diagrams showing that the rhyolite follows the trend of Ⅰ-type
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图 9 八大关地区早侏罗世流纹岩成因判别图解
Figure 9. Discrimination diagram of genetic types for Early Jurassic rhyolite from Badaguan
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图 10 八大关地区早侏罗世流纹岩构造环境判别图解(据Pearce et al., 1984)
Figure 10. Tectonic setting for Early Jurassic rhyolite of Badaguan (after Pearce et al., 1984)
表 2 八大关地区流纹岩主量、微量元素分析结果(主量元素%; 微量元素10-6)
Table 2 Abundances of major and trace elements for the granites in Badaguan area (major elements: %; trace elements: 10-6)
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