| 再论塔里木北缘阿克苏蓝片岩的时代和成因环境:来自锆石U-Pb年龄、Hf同位素的新证据 |
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| 引用本文： | 张健,张传林,李怀坤,叶现韬,耿建珍,周红英.再论塔里木北缘阿克苏蓝片岩的时代和成因环境:来自锆石U-Pb年龄、Hf同位素的新证据[J].岩石学报,2014,30(11):3357-3365. |
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| 作者姓名： | 张健 张传林 李怀坤 叶现韬 耿建珍 周红英 |
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| 作者单位： | 天津地质矿产研究所, 天津 300170;南京地质矿产研究所, 南京 210016;天津地质矿产研究所, 天津 300170;南京地质矿产研究所, 南京 210016;天津地质矿产研究所, 天津 300170;天津地质矿产研究所, 天津 300170 |
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| 基金项目： | 本文受大陆构造与动力学国家重点实验室开放基金(201306)、国家自然科学基金项目(41172175)和中国地质调查局项目(12120113013900)联合资助. |
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| 摘 要： | 阿克苏蓝片岩和基性岩墙形成时代和构造背景对认识塔里木地块前寒武纪构造演化以及新元古代超大陆重建具有重要意义.本文通过对含蓝片岩的阿克苏群中变质碎屑岩和侵入阿克苏群的基性岩墙的锆石U-Pb定年及Hf同位素分析表明,(长石)石英片岩中碎屑锆石出现2个明显的统计峰值,较老一组锆石207Pb/206Pb的表面年龄集中在~1.9Ga,并有少量太古代的年龄信息;另一组较年轻锆石206Pb/238U表面年龄峰值为~820Ma,代表阿克苏群的最大沉积年龄.侵入阿克苏群的基性岩墙锆石U-Pb年龄为~760Ma.阿克苏蓝片岩相变质的时间被严格限定在820~760Ma区间内.碎屑锆石Hf同位素地壳模式年龄峰值出现在2.2~2.3Ga,2.6Ga和3.2~3.3Ga.综合本次工作及前人研究成果,表明阿克苏蓝片岩地体是塔里木早前寒武纪基底之上发育起来的大陆边缘岩浆弧.
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| 关 键 词： | 阿克苏蓝片岩 U-Pb年龄 Lu-Hf同位素 成因环境 塔里木 |
| 收稿时间： | 2014/3/27 0:00:00 |
| 修稿时间： | 6/8/2014 12:00:00 AM |
Revisit to time and tectonic environment of the Aksu blueschist terrane in northern Tarim, NW China: New evidence from zircon U-Pb age and Hf isotope |
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| ZHANG Jian,ZHANG ChuanLin,LI HuaiKun,YE XianTao,GENG JianZhen and ZHOU HongYing.Revisit to time and tectonic environment of the Aksu blueschist terrane in northern Tarim, NW China: New evidence from zircon U-Pb age and Hf isotope[J].Acta Petrologica Sinica,2014,30(11):3357-3365. |
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| Authors: | ZHANG Jian ZHANG ChuanLin LI HuaiKun YE XianTao GENG JianZhen and ZHOU HongYing |
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| Institution: | Tianjin institute of Geology and Mineral Resources, Tianjin 300170, China;Nanjing institute of Geology and Mineral Resources, Nanjing 210016, China;Tianjin institute of Geology and Mineral Resources, Tianjin 300170, China;Nanjing institute of Geology and Mineral Resources, Nanjing 210016, China;Tianjin institute of Geology and Mineral Resources, Tianjin 300170, China;Tianjin institute of Geology and Mineral Resources, Tianjin 300170, China |
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| Abstract: | It is of significant importance to understand the Precambrian tectonic evolution and reconstruction of the Neoproterozoic supercontinent of Tarim block in northwestern China by the study of the timing and tectonic background of the Aksu blueschist and the mafic dyke swarms intruding it. In this study, we carry out U-Pb dating and Hf isotope analysis on zircons from both the meta-clastic rocks of the Aksu blueschist and the mafic dyke swarms. There are two significant age peaks in the U-Pb age spectra of the detrital zircons from the schist, i.e., the older zircon group concentrates at ~1.9Ga, with minor Archaean component; another group peaking at ~820Ma and representing the oldest deposit time of the Aksu blueschist. The mafic dyke swarms intruding the Aksu blueschist yields a zircon U-Pb age of ~760Ma. Hence, the time of the Aksu blueschist facies metamorphism can be quite precisely defined in the range of 820~760Ma. The peaks of the detrital zircon Hf crust-model age spectra appears at 2.2~2.3Ga, 2.6Ga and 3.2~3.3Ga respectively, implying that Aksu blueschist terrane may be continental margin magmatic arc developed on the Early Precambrian Tarim basement. |
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| Keywords: | Aksu blueschist U-Pb age Lu-Hf isotope Tectonic environment Tarim |
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