[1]温淑女.2013.海南岛乐东地区志仲岩体锆石U-Pb年代学、Hf同位素研究及其构造意义.大地构造与成矿学,37(2):294-307.
 WEN Shunv,LIANG Xinquan.2013.Zircon U-Pb Ages, Hf Isotopic Composition of Zhizhong Granitic Intrusion in Ledong Area of Hainan Island and Their Tectonic Implications.Geotectonica et Metallogenia,37(2):294-307.
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海南岛乐东地区志仲岩体锆石U-Pb年代学、Hf同位素研究及其构造意义
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《大地构造与成矿学》[ISSN:ISSN 1001-1552/CN:CN 44-1595/P]

卷:
期数:
2013年37卷02期
页码:
294-307
栏目:
岩石大地构造与地球化学
出版日期:
2013-04-30

文章信息/Info

Title:
Zircon U-Pb Ages, Hf Isotopic Composition of Zhizhong Granitic Intrusion in Ledong Area of Hainan Island and Their Tectonic Implications
作者:
温淑女12梁新权1范蔚茗1王岳军1池国祥3梁细荣1周云1蒋英1
1.中国科学院 广州地球化学研究所,同位素地球化学国家重点实验室,广东 广州 510640;2.中国科学院大学,北京 100049;3.Department of Geology, University of Regina, Regina, Saskatchewan, Canada S4S 0A2
Author(s):
WEN Shunv12 LIANG Xinquan1 FAN Weiming1 WANG Yuejun1CHI Guoxiang3 LIANG Xirong1 ZHOU Yun1 and JIANG Ying1
1.State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, Guangdong, China; 2.University of Chinese Academy of Sciences, Beijing 100049, China; 3.Department of Geology, University o
关键词:
LA-ICP-MS锆石U-Pb定年Hf同位素志仲岩体海南岛
分类号:
P597
文献标志码:
A
摘要:
海南岛分布大量的海西-印支期的花岗岩,关于这些花岗岩的成因及其成岩背景,特别是海西期花岗岩,一直是争论的焦点。本文采用LA-ICP-MS对海南岛乐东地区志仲花岗岩体进行了高精度的锆石U-Pb同位素年代学及锆石Hf同位素组成特征的研究。结果显示,两个花岗岩样品获得接近的272 Ma的结晶年龄,表明该花岗岩体形成于早二叠世晚期。锆石原位Hf同位素组成εHf(t)值变化于-3.7至+2.8之间,对应的两阶段模式年龄tDM2集中在1.12~1.53 Ga,表现出壳幔混合源区特征。据此,推测志仲花岗岩的形成岩浆很可能来源于海南中元古代火成岩的重熔,同时可能有新生地幔物质的加入。其两阶段模式年龄tDM2与前人研究的Nd二阶段模式年龄计算的结果(1.3~1.6 Ga)相近,表明中元古代是该区一期重要的地壳分异的时间,即海南岛在中元古代发生过重要的地壳增生事件。结合区域构造-岩浆活动-沉积记录及古地磁资料,我们趋向于认为海南岛内海西期岩浆作用应该是古特提斯演化过程中构造-岩浆作用的产物,并非古太平洋西向俯冲-碰撞的结果。

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备注/Memo

备注/Memo:
收稿日期: 2012-10-04; 改回日期: 2012-10-30 项目资助: 中国科学院重大项目(编号: KZCX-YW-15-1)、国家973项目(编号:2010CB808900)、国家科技重大专项(2011ZX5023-004-011)和国家自然科学基金项目(批准号: 40872080, 41072081)联合资助。第一作者简介: 温淑女(1985-),女,博士研究生,主要从事岩石大地构造研究。Email: wenshunv@gig.ac.cn
更新日期/Last Update: 2013-04-30