摘要
黑龙江杂岩主要出露在佳木斯地块西缘,沿牡丹江断裂分布,为佳木斯地块与松嫩地块拼合过程中形成的构造混杂岩.杂岩以强烈变形的长英质糜棱岩为主体,其中含有大量具洋壳性质的超基性岩、变基性熔岩(蓝片岩)及变硅质岩和大理岩等岩块或岩片.对出露于黑龙江省东部牡丹江地区的长英质糜棱岩进行了锆石LA-ICP-MS研究.获得两组^(206)Pb/^(238)U年龄数据,其加权平均年龄分别为509.4±7.1 Ma(n=9,MSWD=1.3)和269±1.9 Ma(n=22,MSWD=0.93).其中最老2420和2459 Ma锆石年龄的出现,表明杂岩中有来自古元古界古老物质;509 Ma左右是佳木斯地块中麻山群的高级变质和花岗质岩浆作用年龄;约269 Ma年龄说明黑龙江杂岩变形基质形成于晚二叠世之后,可能与晚古生代古亚洲洋闭合事件相关.
The Heilongjiang complex,mainly occurred in the western margin of Jiamusi massif along Mudanjiang fault,is a tectonic melange formed during the suturing of Jiamusi massif and Songnen massif.The complex is dominated by strongly deformed felsic mylonite,which contains a large number of ultrabasic rocks,metabasic lava(blueschist),meta-silicalite and marble blocks or slices with the nature of oceanic crust.The zircon LA-ICP-MS U-Pb dating of felsic mylonites in Mudanjiang area yields two groups of ^(206)Pb/^(238)U age data,with the weighted mean ages of 509.4±7.1 Ma(n=9,MSWD=1.3)and 269±1.9 Ma(n=22,MSWD=0.93).The zircons with the oldest ages of 2420 and 2459 Ma indicate that the complex contains ancient Paleoproterozoic materials.The age about 509 Ma is for advanced metamorphism and granitic magmatism of Mashan Group in Jiamusi massif.The age about 269 Ma suggests the deformed matrix of Heilongjiang complex be formed after Late Permian,which may be related to the closure of Paleo-Asian Ocean in Late Paleozoic.
作者
赵亮亮
徐福忠
张岩
倪斌
马晓辉
ZHAO Liang-liang;XU Fu-zhong;ZHANG Yan;NI Bin;MA Xiao-hui(Institute of Mineral Resources Research,China Metallurgical Geology Bureau,Beijing 100025,China;Geophysical Exploration Academy,China Metallurgical Geology Bureau,Baoding 071051,Hebei Province,China)
出处
《地质与资源》
CAS
2021年第4期405-413,共9页
Geology and Resources
基金
国家自然科学基金“黑龙江依兰地区黑龙江杂岩变质变形作用研究”(41602216)
“大兴安岭成矿带成果集成及成矿预测研究”(CMGB202002).
