[1]陈公正,武 广,李英雷.2022.大兴安岭南段前进场岩体锆石U-Pb年龄、地球化学及其地质意义.大地构造与成矿学,46(2):356-379.doi:10.16539/j.ddgzyckx.2022.02.011
　CHEN Gongzheng,WU Guang,LI Yinglei.2022.Zircon U-Pb Age and Geochemistry of the Qianjinchang Intrusion in the Southern Great Xing’an Range and its Geological Implications.Geotectonica et Metallogenia,46(2):356-379.doi:10.16539/j.ddgzyckx.2022.02.011
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大兴安岭南段前进场岩体锆石U-Pb年龄、地球化学及其地质意义
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《大地构造与成矿学》[ISSN:ISSN 1001-1552/CN:CN 44-1595/P]

卷:
期数:
2022年46卷02期
页码:
356-379
栏目:
岩石大地构造与地球化学
出版日期:
2022-04-25

文章信息/Info

Title:
Zircon U-Pb Age and Geochemistry of the Qianjinchang Intrusion in the Southern Great Xing’an Range and its Geological Implications
文章编号:
1001-1552(2022)02-0356-024
作者:
陈公正1;  武 广1*;  李英雷1、2;  李铁刚1;  刘瑞麟1、2;  李睿华1、2;  杨 飞1、2
1. 中国地质科学院 矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室, 北京 100037; 2. 北京大学 造山带与地壳演化教育部重点实验室, 北京 100871
Author(s):
CHEN Gongzheng1;  WU Guang1*;  LI Yinglei1、2;  LI Tiegang1;  LIU Ruilin 1、2;  LI Ruihua1、2;  YANG Fei1、2
1. MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China; 2. MOE Key Laboratory of Orogen and Crust Evolution, Peking University, Beijing 100871, China
关键词:
锆石U-Pb年龄;  岩石地球化学;  矿物地球化学;  黑云母二长花岗岩;  前进场岩体;  大兴安岭南段
Keywords:
zircon U-Pb dating;  petrogeochemistry;  mineral geochemistry;  biotite monzogranite;  Qianjinchang intrusion;  the southern Great Xing’an Range
分类号:
P595; P597
DOI:
10.16539/j.ddgzyckx.2022.02.011
文献标志码:
A
摘要:
前进场岩体位于大兴安岭南段, 主要岩石类型为黑云母二长花岗岩, 是道伦达坝铜钨锡银矿床的赋矿围岩之一。本文对前进场岩体开展了岩石地球化学、LA-ICP-MS锆石U-Pb定年、锆石Lu-Hf同位素及矿物地球化学研究。锆石U-Pb定年结果表明前进场岩体形成于278~279 Ma, 为早二叠世岩浆活动产物。岩石地球化学特征显示其SiO2含量为66.18%~68.71%, 具有较高的全碱含量(Na2O+K2O=7.14%~8.05%)和A/CNK值(1.10~1.21), 富集轻稀土元素、亏损重稀土元素, 稀土元素配分曲线呈右倾式, 具中等Eu负异常(δEu=0.40~0.56); 岩石富集大离子亲石元素(Rb、Th和K等)和轻稀土元素(La和Ce等), 强烈亏损高场强元素(Nb、Ta、Zr、Hf、P和Ti等)和Sr。样品的锆石εHf(t)值在2.5~9.7之间, Hf同位素单阶段模式年龄(tDM1)在552~747 Ma之间, 两阶段模式年龄(tDM2)在696~1023 Ma之间, 表明其源区主要为起源于亏损地幔的新元古代新生地壳物质。电子探针分析结果显示岩体中的云母为富铁黑云母, 斜长石为更长石, 表明岩浆分异程度较低。磷灰石具有富F(2.73%~5.09%, 平均为3.75%)、贫Cl(0.02%~0.07%, 平均为0.05%)特征, 稀土元素总量较低, 其配分曲线呈海鸥式, 轻重稀土元素分馏不明显, 具有明显的Eu负异常和弱的Ce正异常, 表明岩浆氧逸度较低。前进场岩体形成于贺根山洋闭合后的后碰撞环境, 是黑云斜长角闪岩部分熔融形成的过铝质花岗岩, 不是道伦达坝矿床的成矿岩体。
Abstract:
The Qianjinchang intrusion, located in the southern Great Xing’an Range and mainly composed of biotite monzogranite, is the main host rock of the Daolundaba Cu-W-Sn-Ag deposit. In this paper, we report the geochemistry, zircon U-Pb age, Lu-Hf isotopes, and mineral geochemistry of the Qianjinchang intrusion. U-Pb dating of zircon from the biotite monzogranite yielded crystallization ages of 278 Ma and 279 Ma. The geochemical characteristics of the biotite monzogranite show high contents of SiO2 (66.18% - 68.71%) and Na2O+K2O (7.14% - 8.05%), with high values of A/CNK (1.10 - 1.21). The biotite monzogranites show right-inclined chondrite-normalized REE patterns, rich in LREE and LILE (such as Ba, Rb, and K) and deplete in HREE and HFSE (Nb, Ta, Zr, Hf, P, and Ti), with medium negative Eu anomalies (0.4 - 0.56). The Qianjinchang intrusion has high εHf(t) values (2.5 - 9.7), young single-stage and two-stage model ages (552 - 747 Ma; 696 - 1023 Ma), suggesting that the Qianjinchang intrusion originated from partial melting of juvenile crust material that originally derived from depleted mantle. The mica and plagioclase in the Qianjinchang intrusion are haughtonite and andesine, respectively, implying a slight magma differentiation. Apatite from the Qianjinchang intrusion is enrich in F (2.73% - 5.09%, averaging 3.74%) and poor in Cl (0.02% - 0.09%, averaging 0.05%), with low REE contents, negative Eu anomalies, and positive Ce anomalies, implying a low fO2 for the magma of the Qianjinchang intrusion. The apatite has seagull forms rare earth element distribution patterns. Our results show that the Qianjinchang intrusion consisting of peraluminous granite that formed by partial melting of a source dominated by biotite-bearing plagioclase amphibolite, under a post-collisional environment after the closure of the Hegenshan Ocean, which is a branch ocean of the Paleo-Asian Ocean. The Qianjinchnag intrusion is not the ore-forming rock body of the Daolundaba deposit.

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备注/Memo

备注/Memo:
收稿日期: 2020-12-04; 改回日期: 2021-01-25
项目资助: 国家重点研发计划项目(2017YFC0601303)、战略性矿产重点远景区矿产地质调查二级项目(DD20221684)、国家自然科学基金项目(41772086)和河北地质大学青年科技基金项目(QN202218)联合资助。
第一作者简介: 陈公正(1993-), 男, 博士研究生, 矿物学、岩石学、矿床学专业。E-mail: 86793604@qq.com
通信作者: 武广(1965-), 男, 研究员, 从事矿床学和地球化学研究。E-mail: wuguang65@163.com
更新日期/Last Update: 2022-04-10