新疆卡鲁安矿区伟晶岩锆石U-Pb 定年、铪同位素组成及其与哈龙花岗岩成因关系研究
Zircon U-Pb geochronology and Hf isotopes of pegmatites from the Kaluan mining area in the Altay, Xinjiang and their genetic relationship with the Halong granite
查看参考文献65篇
|
文摘
|
利用LA-ICPMS 和LA-MC-ICPMS 技术, 对卡鲁安-阿祖拜伟晶岩田中4条伟晶岩脉以及哈龙岩体中锆石U-Pb 定年、铪同位素组成进行了研究。研究显示, 卡鲁安矿区805、806、807号脉的形成时代分别为(216.0±2.6) Ma、(223.7±1.8) Ma 和(221±15) Ma, 属三叠纪岩浆活动的产物。对于库卡拉盖650号脉, 锆石U-Pb定年结果显示, 它由形成时代为(227.9±2.6) Ma 的早期钠长石伟晶岩与形成时代为(211.3±2.4) Ma 的晚期锂辉石-钠长石-锂云母伟晶岩2期伟晶岩构成。哈龙岩体形成时代为400.9 ~ 403.3 Ma, 由于伟晶岩与哈龙岩体之间存在形成时代上的差异(170 Ma 以上), 预示着它们之间不具成因上的联系。卡鲁安矿区伟晶岩脉中锆石显示较小的正ε_(Hf)(t)值(+0.65~+2.50)和较大的模式年龄T_(DM2)(1090~1213 Ma), 相似于可可托海3号脉、柯鲁木特112号脉中锆石的铪同位素组成, 指示伟晶岩由陆-陆碰撞体制伸展背景下的加厚地壳物质减压熔融所形成。 |
|
其他语种文摘
|
Zircon U-Pb dating and Hf isotopes of four pegmaites from the Kaluan-Azubai pegmatite mining area were carried out by LA-ICPMS and LA-MC-ICPMS in this paper. The formation ages of pegmatites, numbered 805, 806 and 807 in the Kaluan mining area, were determined to be (216.0±2.6) Ma, (223.7±1.8) Ma and (221±15) Ma, respectively, i.e. products of Triassic magmatic activities. For the Kukalagai No.650 pegmatite, zircon U-Pb dating shows that it made up of two stages of pegmatites, that is, the early albite pegmatite (227.9±2.6) Ma and the late spodumene-albite-lepidolite pegmatite (211.3±2.4) Ma. The intrusive age of Halong granite is in the range of 400.9–403.3 Ma, as the products of Devonian magmatic activities. As large gaps in their formation age (>170 Ma) between pegmatites and Halong granites, it indicates that pegmatites from the Kaluan mining area have no genetic relationship with the Halong granite. Zircons from the pegmatites of Kaluan mining area have lower positive ε_(Hf)(t) values (+0.65 – +2.50), with T_(DM2) model ages of 1090–1213 Ma, similar to zircon Hf isotopes of the Keketuohai No.3 pegmatite and the Kelumute No.112 pegmatite, indicating that the pegmatites were created by crust thickening and decompression melting in a post-collision tectonic setting. |
|
来源
|
地球化学
,2015,44(1):9-26 【核心库】
|
|
关键词
|
锆石U-Pb 定年
;
锆石铪同位素
;
花岗岩
;
伟晶岩
;
阿尔泰
|
|
地址
|
中国科学院地球化学研究所, 贵州, 贵阳, 550002
|
|
语种
|
中文 |
|
文献类型
|
研究性论文 |
|
ISSN
|
0379-1726 |
|
学科
|
地质学 |
|
基金
|
国家自然科学基金
;
新疆有色金属工业(集团)有限责任公司科研项目
;
中国科学院地球化学研究所矿床地球化学国家重点实验室开放课题资助基金
|
|
文献收藏号
|
CSCD:5334596
|
参考文献 共
65
共4页
|
|
1.
Windley B F. Neoproterozoic to Paleozoic geology of the Altai orogen, NW China: New zircon age data and tectonic evolution.
J Geol,2002,110(6):719-737
|
被引
279
次
|
|
|
|
|
2.
邹天仁. 新疆阿尔泰造山带花岗岩和非造山花岗岩及其判别标志.
地质学报,1988(3):229-243
|
被引
1
次
|
|
|
|
|
3.
吴柏青. 试论新疆阿尔泰花岗伟晶岩的成因.
新疆矿产地质,1989(1):60-70
|
被引
9
次
|
|
|
|
|
4.
王涛. 阿尔泰造山带花岗岩时空演变、构造环境及地壳生长意义------以中国阿尔泰为例.
岩石矿物学杂志,2010,29(6):595-618
|
被引
121
次
|
|
|
|
|
5.
曾乔松. 阿尔泰冲乎尔盆地花岗质岩类的锆石SHRIMP U-Pb定年及其构造意义.
岩石学报,2007,23(8):1921-1932
|
被引
73
次
|
|
|
|
|
6.
王登红. 新疆阿尔泰印支期伟晶岩的成矿年代学研究.
矿物岩石地球化学通报,2003,22(1):14-17
|
被引
31
次
|
|
|
|
|
7.
任宝琴. 阿尔泰造山带伟晶岩年代学及其地质意义.
矿物学报,2011,31(3):587-596
|
被引
50
次
|
|
|
|
|
8.
Lu Zhenghang. Petrogenesis and magmatic-hydrothermal evolution time limitation of Kelumute No.112 pegmatite in Altay, Northwestern China: Evidence from zircon U-Pb and Hf isotopes.
Lithos,2012,154:374-391
|
被引
32
次
|
|
|
|
|
9.
Zhu Yongfeng. Geochemistry of the rare metal-bearing pegmatite No.3 vein and related granites in the Keketuohai region, Altay Mountains, northwest China.
J Asian Earth Sci,2006,27(1):61-77
|
被引
123
次
|
|
|
|
|
10.
Wang Tao. SHRIMP U-Pb Zircon geochronology of the Altai No.3 Pegmatite, NW China, and its implications for the origin and tectonic setting of the pegmatite.
Ore Geol Rev,2007,32(1):325-336
|
被引
78
次
|
|
|
|
|
11.
Xiao Wenjiao. Palaeozoic accretionary and convergent tectonics of the southern Altaids: Implications for the growth of Central Asia.
J Geol Soc,2004,161(3):339-342
|
被引
286
次
|
|
|
|
|
12.
Mossakovsky A A. Central Asian fold belt: Geodynamic evolution and formation history.
Geotectonics,1994,27(6):445-474
|
被引
12
次
|
|
|
|
|
13.
Xiao Wenjiao. Accretion leading to collision and the Permian Solonker suture, Inner Mongolia, China: Termination of the central Asian orogenic belt.
Tectonics,2003,22(6):1069-1089
|
被引
513
次
|
|
|
|
|
14.
Xiao Wenjiao. Paleozoic accretionary and collisional tectonics of the Eastern Tianshan (China): Implications for the continental growth of central Asia.
Am J Sci,2004,304(4):370-395
|
被引
436
次
|
|
|
|
|
15.
Yuan Chao. Accretionary orogenesis of the Chinese Altai: Insights from Paleozoic granitoids.
Chem Geol,2007,242(1):22-39
|
被引
22
次
|
|
|
|
|
16.
Xiao Wenjiao. Middle Cambrian to Permian subductionrelated accretionary orogenesis of Northern Xinjiang, NW China: Implications for the tectonic evolution of central Asia.
J Asian Earth Sci,2008,32(2):102-117
|
被引
457
次
|
|
|
|
|
17.
Long Xiaoping. Early Paleozoic sedimentary record of the Chinese Altai: Implications for its tectonic evolution.
Sediment Geol,2008,208(3/4):88-100
|
被引
34
次
|
|
|
|
|
18.
Sengor A. Evolution of the Altaid tectonic collage and Palaeozoic crustal growth in Eurasia.
Nature,1993,364(6435):299-307
|
被引
1143
次
|
|
|
|
|
19.
Wang Tao. Timing, petrogenesis, and setting of Paleozoic synorogenic intrusions from the Altai Mountains, Northwest China: Implications for the tectonic evolution of an accretionary orogen.
J Geol,2006,114(6):735-751
|
被引
195
次
|
|
|
|
|
20.
Xiao Wenjiao. Geodynamic evolution of Central Asia in the Paleozoic and Mesozoic.
Int J Earth Sci,2009,98(6):1185-1188
|
被引
80
次
|
|
|
|
|
了解气象卫星更多信息，请访问