[1]刘贻灿,侯克斌,杨 阳.2018.大别山北淮阳带奥陶纪花岗岩的厘定及其对北秦岭东延的启示.大地构造与成矿学,优先出版:001-13.doi:10.16539/j.ddgzyckx.2020.02.017
 LIU Yican,HOU Kebin,YANG Yang.2018.Confirmation of the Ordovician Granite from the Beihuaiyang Zone in the Dabie Orogen: Insight into Eastern Extension of the Northern Qinling Orogen.Geotectonica et Metallogenia,优先出版:001-13.doi:10.16539/j.ddgzyckx.2020.02.017
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大别山北淮阳带奥陶纪花岗岩的厘定及其对北秦岭东延的启示
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《大地构造与成矿学》[ISSN:ISSN 1001-1552/CN:CN 44-1595/P]

卷:
期数:
2018年优先出版
页码:
001-13
栏目:
出版日期:
2020-12-30

文章信息/Info

Title:
Confirmation of the Ordovician Granite from the Beihuaiyang Zone in the Dabie Orogen: Insight into Eastern Extension of the Northern Qinling Orogen
作者:
刘贻灿1 侯克斌12 杨 阳1 李 洋1 宋 彪3
1.中国科学院壳幔物质与环境重点实验室, 中国科学技术大学 地球和空间科学学院, 安徽 合肥 230026; 2.安徽省地质调查院, 安徽 合肥 230001; 3.北京离子探针中心, 中国地质科学院 地质研究所, 北京 100037
Author(s):
LIU Yican1 HOU Kebin12 YANG Yang1 LI Yang1 and SONG Biao3
1. CAS Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, Anhui, China; 2. Anhui
关键词:
花岗岩 早古生代 SHRIMP U-Pb定年 俯冲增生 北淮阳带
Keywords:
granite the early Paleozoic SHRIMP U-Pb dating subduction-accretion the Beihuaiyang zone
分类号:
P597
DOI:
10.16539/j.ddgzyckx.2020.02.017
文献标志码:
A
摘要:
详细的野外地质调查以及锆石SHRIMP U-Pb定年和初步的岩石学研究表明, 大别山北淮阳带东段发育早古生代奥陶纪花岗岩。而且, 这些花岗岩经过了强烈的构造变形、局部发育片麻理和绿帘角闪岩相变质作用, 它们的形成时代为457±2 Ma, 并且与北淮阳带西段马畈闪长岩的形成时代以及北秦岭?桐柏造山带一期与大洋俯冲相关的早古生代岛弧岩浆作用时代一致。结合区域地质背景和盆地沉积分析, 证明北秦岭古生代俯冲增生造山带至少向东延伸到大别山北淮阳带的金寨及相邻地区。因此, 研究区古生代花岗岩及相关岩石的进一步研究, 将为大别山碰撞造山带的古生代构造演化以及华南与华北板块之间的汇聚?拼贴过程提供新的制约。
Abstract:
Academy of Geological Survey, Hefei 230001, Anhui, China; 3. Beijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, ChinaThe detailed field investigation, zircon SHRIMP U-Pb dating and preliminary petrographic observation suggest that the Early Paleozoic Ordovician granite is for the first time documented to occur in the eastern Beihuaiyang zone of the Dabie orogen. In addition, the granite experienced a strong deformation associated with local foliation and epidote-amphiboilite facies metamorphism, and its formation time is 457±2 Ma. The age is similar to those of the Mafan diorites from the western segment of the Beihuaiyang zone and the early Paleozoic arc rocks related to oceanic subduction in the northern Qinling?Tongbo orogen. Combined with regional geological background and the related basin sediments, it is indicated that the northern Qinling orogen easterly extends to the Jinzhai and adjacent area in the eastern segment of Beihuaiyang zone, the Dabie orogen. As a result, the further integrated researches on the Paleozoic granites and related rocks in the studied region will provide new constraints on the Paleozoic tectonic evolution of the Dabie collisional orogen, and the convergent-amalgamate processes between the North and South China Blocks.

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备注/Memo

备注/Memo:
收稿日期: 2019-07-06; 改回日期: 2019-07-29
项目资助: 国家重点基础研究发展计划(“973”计划)项目(2015CB856104)和国家自然科学基金项目(41773020)联合资助。
第一作者简介: 刘贻灿(1962-), 男, 教授, 博士生导师, 主要从事变质地球化学与岩石大地构造学研究。Email: liuyc@ustc.edu.cn
更新日期/Last Update: 2020-04-03