早侏罗世粗中粒黑云母二长花岗岩岩石地球化学、 LA-ICP-MS 锆石 U-Pb 年代学特征及成因——以大兴安岭北段潮满林场地区为例

Geochemistry and LA-ICP-MS zircon U-Pb chronology and genetic mechanism of the Early Jurassic coarse to medium grained biotite monzogranite: a case study of the Chaoman Forest Farm area in the Northern Great Xingan Range

摘要

以大兴安岭北段额尔古纳地块北缘潮满林场地区粗中粒黑云母二长花岗岩为研究对象，采用地质调查、岩石地球化学和 LA-ICP-MS 锆石 U-Pb 年代学方法，分析粗中粒黑云母二长花岗岩岩石学、主量元素、微量元素和年代学等特征，探讨成因及构造环境。结果表明：潮满林场地区粗中粒黑云母二长花岗岩具有 I 型花岗岩特征，属于弱过铝质高钾钙碱性花岗岩；粗中粒黑云母二长花岗岩中 68.92 \mathrm{\%} \sim 72.44 \mathrm{\%} , {\mathrm{N}\mathrm{a}}_2 \mathrm{O} 的质量分数为 4.65 \mathrm{\%} \sim 4.85 \mathrm{\%} , {\mathrm{K}}_2 \mathrm{O} 的质量分数为 3.33 \mathrm{\%} \sim 4 . 41 \mathrm{\%} , {\mathrm{A}\mathrm{l}}_2 {\mathrm{O}}_3 的质量分数为 15.25 \mathrm{\%} \sim 16.75 \mathrm{\%} 的质量分数为 0.95 \sim 2.84 ，里特曼指数为 10^-6 ；稀土元素总量的质量分数为（101.24~152.40）× Rb、Th、Ce、Zr ，轻、重稀土元素分馏明显，轻稀土元素富集，重稀土元素亏损，其中富集 Ta、Nb、P、Ti 等元素，相对亏损 w(SiO₂) 等元素。粗中粒黑云母二长花岗岩岩浆来源于新增生下地壳物质的部分熔融，形成于早侏罗世（192.1 ± 1.6）Ma。研究区早侏罗世粗中粒黑云母二长花岗岩的形成环境为与蒙古-鄂霍茨克洋南向俯冲一碰撞作用相关的活动大陆边缘火山弧环境。该结果为研究大兴安岭北段潮满林场地区粗中粒黑云母二长花岗岩岩体构造背景和年代学提供依据。

Abstract

Farm on the northern edge of the Erguna Block in North Great Xing'an Range. Adopting geological surveys, rock geochemistry, and LA-ICP-MS zircon U-Pb geochronology research methods is to analyze the petrological, major element, trace element, and chronological characteristics of the coarse to medium grained biotite monzogranite and to discuss its genesis mechanism and tectonic environment. The results show that the coarse to medium grained biotite monzogranite in the Chaoman Forest Farm area has Itype granite characteristics and belongs to weakly peraluminous and high potassium-cala-alkaline granite, the 68.92 \mathrm{\%} - 72.44 \mathrm{\%} , w \left({\mathrm{N}\mathrm{a}}_2\mathrm{O}\right) of monzogranite is 4.65 \mathrm{\%} - 4.85 \mathrm{\%} , w \left({\mathrm{K}}_2\mathrm{O}\right) is 3.33 \mathrm{\%} 4.41 \mathrm{\%} is w(Al₂O₃), and 15.25 \mathrm{\%} - 16.75 \mathrm{\%} is \left( \sigma \right), rittman index 0.95-2.84 is (101.24-152.40)×10^-6. Total rare earth content is Rb,Th,Ce,Zr. There are significant fractionation of light and heavy rare earths, enrichment of light rare earths, loss of heavy rare earths, enriched in elements such as Ta,Nb,P and relatively depleted in elements such as U-Pb, and Ti. The magma of the coarse to medium grained biotite monzogranite originates from the partial melting of newly accreted lower crustal materialand was formed in the Early Jurassic (192.1 ± 1.6) Ma. The tectonic environment of the Early Jurassic coarse to medium grained biotite monzogranite in the study area is an active continental margin volcanic arc environment related to the south ward subduction collision of the Mongolian-Okhotsk Ocean. This result provides evidence for the study of the tectonic background and chronology of the coarse to medium grained biotite monzogranite in the Chaoman Forest Farm area of the northern section of the Great Xing'an Range.

关键词

LA-ICP-MS 锆石 U-Pb 年代学 / 地球化学 / 粗中粒黑云母二长花岗岩 / 早侏罗世 / 潮满林场地区 / 大兴安岭北段

Key words

LA-ICP-MS zircon U-Pb chronology / geochemistry / coarse to medium grained biotite monzogranite / Early Jurassic / Chaoman Forest Farm / North Great Xing'an Range

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基金资助

黑龙江省 SiO₂ 万区域地质矿产调查项目(HLJKD2015-04)