Geochemical characteristics and intraplate extension of Late Devonian bimodal volcanic rocks in Chifeng area of Inner Mongolia
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摘要:
内蒙古赤峰敖汉旗一带的朝吐沟组火山岩由变玄武岩、变流纹岩组成，是一套典型的“双峰式”火山岩组合。采用LA-ICP-MS锆石U-Pb测年方法，获得了流纹岩的锆石206Pb/238U加权平均年龄分别为（359±1）Ma和（360±1）Ma，形成于晚泥盆世法门期。火山岩的SiO2含量分布在46.24%~56.6%和77.59%~85.75%，分别属于变玄武岩（玄武安山岩）和变流纹岩。变玄武岩（玄武安山岩）轻稀土元素弱富集而重稀土元素略亏损，（La/Yb）N=2.4~8.76，有弱Eu负异常，富集大离子亲石元素和高场强元素，Nb、Ta、Ti有明显负异常，87Sr/86Sr初始比值为0.705076~0.707770，具有高的正εNd（t）值（+0.51~+4.90）和年轻的模式年龄TDM（964~1090 Ma），推断其源于遭受地壳物质混染的亏损地幔；变流纹岩富硅、钾和钠，贫镁，具有轻稀土元素富集而重稀土元素略亏损，（La/Yb）N=7.07~11.07，有强烈的Eu负异常（δEu=0.12~0.43），Ti、P、Sr、Ba相对强烈亏损，Nb、Ta亏损，Rb、Th、U、K相对富集；其87Sr/86Sr初始比值为0.713757~0.739647，εNd（t）值为-1.75~+2.54），和年轻的模式年龄TDM（846~1156 Ma）；多数锆石的εHf（t）为-2.3~+6.9，年轻的模式年龄TDM（707~1074 Ma），具有A型花岗岩的特征，推测其来源为新元古代时新生的年轻陆壳。综合前人区域研究成果、地球化学特征，朝吐沟组“双峰式”火山岩形成于晚泥盆世板内伸展构造背景。
Abstract:The volcanic rocks of the Chaotugou Formation in Chifeng area of Inner Mongolia consist of meta-basalts and metarhyolites and exhibit typical "double peaks", with the SiO2 content being 46.24%-56.6% and 77.59%-85.75% respectively. Zircon LA-ICP-MS U-Pb dating of rhyolite yielded U-Pb ages of(359±1) Ma-(360±1) Ma, which represent the time of crystallization of the volcanic rocks. The volcanic rocks were formed in late Devonian Famennian age. Geochemically, meta-basalts (or basaltic andesites) are characterized by enriched LREE, depleted HREE, slightly negative Eu, Nb, Ta, Sr and Ti anomalies and high abundances of LILE and HFSE, with the (La/Yb)N ratios from 2.4 to 8.76, and the 87Sr/86Sr initial values from 0.705076 to 0.707770; in addition, they have relatively high positive εNd(t)values (+0.51 to +4.90) and relatively young TDM (964-1090 Ma) ages. The mafic rocks might have resulted from the mixture of depleted mantle with crustal source. Meta-rhyolites are generally characterized by rich silicon, alkali and poor magnesium. They are characterized by enriched LREE, depleted HREE, noticeable negative Eu (δEu 0.12-0.43), Nb, Ta, Sr, P and Ti anomalies, relatively high U, Th and rather low Ba, Sr, Ti and P; the (La/Yb)N ratios are from 7.07 to 11.07, 87Sr/86Sr initial values are high (0.713757-0.739647), negative εNd(t) values are low (-1.75 to +2.54), and TDM ages are relatively young (846-1156 Ma); besides, most zircons have the positive εHf(t) values (-2.3 to +6.9) and relatively young TDM ages (707-1074 Ma). The felsic rocks show an A-type affinity and might have come from a juvenile crustal source. According to their geochemistry and previous regional geological studies, the late Devonian volcanic rocks are basalts and rhyolites, suggesting a typical bimodal volcanic rock association and implying an extensional setting.
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Key words:
- Late Devonian /
- bimodal volcanic rocks /
- extensional setting /
- Chifeng area
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图 5 晚泥盆世朝吐沟组火山岩Nb/Y-Zr/TiO2分类图解（Winchester et al., 1977）
Figure 5.
图 8 朝吐沟组双峰式火山岩中玄武岩Zr-Zr/Y (a) (据Pearce et al., 1984, 1995)及流纹岩Nb-Y构造判别图解(b) (据Frster et al., 1997）
Figure 8.
表 1 朝吐沟组流纹岩(P1TW3, P2TW1) LA-ICP-MS锆石U-Pb同位素测定结果
Table 1. LA-ICP-MS zircon U-Pb dating results for the rhyolites (P1TW3, P2TW1) of the Chaotugou Formation
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表 2 赤峰敖汉旗晚泥盆世朝吐沟组火山岩地球化学分析结果
Table 2. Geochemical compositions of Late Dovianvolcanonic rocks in Aohanqi area of Chifeng
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表 3 赤峰敖汉旗晚泥盆世火山岩Sr-Nd同位素组成
Table 3. Sr-Nd isotopic compositions of Late Devonian volcanic rocks in Aohan Banner area of Chifeng
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表 4 赤峰敖汉旗晚泥盆世朝吐沟组流纹岩锆石Hf同位素组成
Table 4. Hf isotopic compositions of zircon from rhyolites samples in Aohan Banner area of Chifeng
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