[1]李 亮,孙景贵*,郭 维.2016.鹤岗北部地区黑龙江岩群的构造属性: 来自岩石地球化学、锆石U-Pb定年和Hf同位素的制约.大地构造与成矿学,4(5):1014-1030.doi:10.16539/j.ddgzyckx.2016.05.010
 LI Liang,SUN Jinggui*,GUO Wei and HAN Jilong.2016.Tectonic Attribute of Heilongjiang Metamorphic Rocks in the Northern Part of Hegang Area, NE China: Constrains from Geochemistry, Zircon U-Pb Dating and Hf Isotopic Composition.Geotectonica et Metallogenia,4(5):1014-1030.doi:10.16539/j.ddgzyckx.2016.05.010
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鹤岗北部地区黑龙江岩群的构造属性: 来自岩石地球化学、锆石U-Pb定年和Hf同位素的制约
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《大地构造与成矿学》[ISSN:ISSN 1001-1552/CN:CN 44-1595/P]

卷:
期数:
2016年40卷05期
页码:
1014-1030
栏目:
岩石大地构造与地球化学
出版日期:
2016-10-15

文章信息/Info

Title:
Tectonic Attribute of Heilongjiang Metamorphic Rocks in the Northern Part of Hegang Area, NE China: Constrains from Geochemistry, Zircon U-Pb Dating and Hf Isotopic Composition
文章编号:
1001-1552(2016)05-1014-017
作者:
李 亮1 孙景贵1* 郭 维2 韩吉龙1
1.吉林大学 地球科学学院, 吉林 长春 130061; 2.天津华北地质勘查局地质研究所, 天津 300170
Author(s):
LI Liang1 SUN Jinggui1* GUO Wei 2 and HAN Jilong1
1. School of Earth Sciences, Jilin University, Changchun 130061, Jilin, China; 2. Geological Institute of North China Geological Exploration Bureau of Tianjin, Tianjin 300170, China
关键词:
黑龙江岩群 岩石地球化学 锆石U-Pb定年 Hf同位素 形成环境 构造属性
Keywords:
Heilongjiang metamorphic rocks geochemistry zircon U-Pb dating Hf isotopic composition formation environment tectonic setting
分类号:
P595; P597
DOI:
10.16539/j.ddgzyckx.2016.05.010
文献标志码:
A
摘要:
产于鹤岗北部地区的黑龙江岩群是由绿帘绿泥钠长片岩、绿帘蓝闪片岩(下部)和二云母片岩、石榴白云钠长片岩、方解白云钠长片岩、石榴白云钠长石英片岩(上部)等岩系组成。本文通过岩石地球化学、锆石U-Pb年代学和Hf同位素组成研究, 厘定下岩组原岩为幔源碱性玄武岩(SiO2=47.44%~48.38%)及岛弧钙碱性玄武岩(SiO2=46.84%~49.22%), 有3组锆石U-Pb年龄(526±44 Ma, n=3; 249±11 Ma, n=6; 207±4 Ma, n=8); 上岩组原岩为海陆交互相碎屑岩(SiO2=66.70%~93.00%), 有4组锆石U-Pb年龄(484±13 Ma, n=3; 429±24 Ma, n=3; 277±4 Ma, n=11; 262±3 Ma, n=6)。结合锆石的内部结构、Hf同位素和区域构造演化特征, 幔源火山喷发和沉积作用发生在277±4 Ma, 碰撞造山作用发生在262~249 Ma, 构造折返发生在207±4 Ma。这项研究对于深入认识黑龙江岩群性质和构造属性具有重要的意义。
Abstract:
The Heilongjiang metamorphic rocks located in the northern part of the Hegang area, NE China, consist of epidote-chlorite-albite schist, epidote-glaucophane schist (the lower group), and two-mica schist, garnet-muscovite -albite schist, calcite-muscovite-albite schist, garnet-muscovite-quartz schist (the upper group), etc. Detailed research on geochemistry, zircon U-Pb dating and Hf isotopic composition showed that the protoliths of the lower group are alkali basalt derived from mantle (SiO2=47.44% ? 48.38%), and island arc calc alkali basalt (SiO2=46.84% ? 49.22%). The lower group contains three groups of zircon U-Pb age (526±44 Ma, n=3; 249±11 Ma, n=6; 207±4 Ma, n=8), whereas the protolith of the upper group is alternative continent-marine facies clastic rock (SiO2=66.70% ? 93.00%), and contains four groups of detrital zircon U-Pb age (484±13 Ma, n=3; 429±24 Ma, n=3; 277±4 Ma, n=11; 262±3 Ma, n=6). Combined with zircon internal texture, Hf isotopic composition and regional tectonic evolution features, we suggest that the volcanic eruption and sedimentation occurred at 277±4 Ma, and collision orogeny was during 262 Ma to 249 Ma. Tectonic exhumation occurred at 207±4 Ma. The research is significant to identify the nature and tectonic affinity of Heilongjiang metamorphic rocks.

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备注/Memo

备注/Memo:
收稿日期: 2014-05-27; 改回日期: 2014-10-13 项目资助: 国家自然科学基金项目(41172072和40772052)联合资助。 第一作者简介: 李亮(1985–), 男, 博士研究生, 地球化学专业。Email: liliang850729@163.com 通信作者: 孙景贵(1961–), 男, 教授, 博导, 从事岩浆、热液矿床研究工作。Email: sunjinggui@jlu.edu.cn
更新日期/Last Update: 1900-01-01