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摘要
以大兴安岭呼中地区满克头鄂博组火山岩为研究对象,采用地质勘查、岩石地球化学和 LA-ICP-MS 锆石 SiO2 年代学方法,分析火山岩的岩石学、主量元素、微量元素和年代学特征,探讨火山岩岩浆来源、岩石成因及构造环境。结果表明:满克头鄂博组火山岩 76.82%∼77.82%,Al2O3 的质量分数为 11.83%∼12.55%, K2O 质量分数为 1.50%∼4.72%,Na2O的质量分数为 3.10%∼5.24% 的质量分数为 10-6 ,属于铝质高钾钙碱性岩系;稀土元素总量的质量分数为(102.54~141.50)× (95.75∼132.66)×10-6 ,轻稀土元素富集,质量分数为 10-6 ,重稀土元素亏损,质量分数为 (6.79~9.87)× Rb、 K、Th、La、Ce、Nd、Hf ,其中, Ba、Sr、Nb、P、Ti 等元素富集, (164.6±1.8)Ma 等元素亏损, Eu 元素具有明显的负异常特征。火山岩岩浆来源于沉积物熔体加入的地壳物质部分熔融,满克头鄂博组酸性火山岩获得锆石 U-Pb 年龄为 U-Pb ,形成时代为晚侏罗世。研究区满克头鄂博组的构造环境为与古太平洋板块俯冲作用相关的活动陆缘环境。该结果为研究大兴安岭火山岩带年代学和构造背景提供依据。
Abstract
This study investigates the volcanic rocks of the Manketouebo Formation in the Huzhong Area of the Great Xing'an Range using geological survey methods, petrological and geochemical analyses, and zircon U-Pb dating via LA-ICP-MS. The research systematically examines the petrology, major and trace element geochemistry, and geochronological characteristics of the volcanic rocks, with the aim of elucidating their magmatic source, petrogenesis, and tectonic setting. The results indicate that the Manketoúebo Formation volcanic rocks have 76.82% contents ranging from 77.82%,Al2O3 to 11.83% contents ranging from 12.55%, K2O to 1.50% contents ranging from 4.72% to Na2O, and 3.10% contents ranging from 5.24% to (102.54-141.50)×10-6, classifying them as high-potassium calcalkaline aluminosilicate rocks. The total rare earth element(REE) content is (95.75-132.66)×10-6, which is enrichment of light rare earth elements, mass fraction of LREEs is (6.79-9.87)×10-6 and heavy rare earth element deficit, mass fraction of HREEs is 164.6±1.8. The rocks show enrichment in elements such as Rb, K, Th, La, Ce, Nd, and Hf, while Ba, Sr, Nb, P, and Ti are depleted. A pronounced negative Eu anomaly is also observed. Geochemical evidence suggests that the volcanic magma originated from partial melting of crustal material with sedimentary input. The zircon U-Pb age of ( Sr-Nd、 Pb-Hf ) Ma was obtained from the acidic volcanic rocks of the Manketou'ebo Formation, which was formed in the Late Jurassic. The tectonic environment of the Manketou'ebo Formation is interpreted as an active continental margin related to the subduction of the Paleo-Pacific Plate. These findings provide critical insights into the chronology and tectonic framework of the volcanic belt in the Great Xing'an Range.
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于跃江,李慧,李新鹏,江峰,梁景龙,李金明,卜程丹.
大兴安岭呼中地区满克头鄂博组火山岩地球化学特征、锆石 U-Pb 年龄及构造环境[J].
东北石油大学学报, 2025, 49(3): 29-40 DOI:10.3969/j.issn.2095-4107.2025.03.003
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基金资助
黑龙江省1 :5万区域地质矿产调查项目(HLJKD2015-07)