LA-ICP-MS zircon U-Pb dating of syenite from Yushigou in Northern Qilian Mountain

WANG Guoqiang; LI Xiangmin; YU Jiyuan; TANG Zhuo; ZHU Tao; PAN Feng; ZHANG Yue; BU Tao

2018 Vol. 37, No. 4

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WANG Guoqiang, LI Xiangmin, YU Jiyuan, TANG Zhuo, ZHU Tao, PAN Feng, ZHANG Yue, BU Tao. LA-ICP-MS zircon U-Pb dating of syenite from Yushigou in Northern Qilian Mountain[J]. Geological Bulletin of China, 2018, 37(4): 532-537.

Citation:

WANG Guoqiang, LI Xiangmin, YU Jiyuan, TANG Zhuo, ZHU Tao, PAN Feng, ZHANG Yue, BU Tao. LA-ICP-MS zircon U-Pb dating of syenite from Yushigou in Northern Qilian Mountain[J]. Geological Bulletin of China, 2018, 37(4): 532-537.

LA-ICP-MS zircon U-Pb dating of syenite from Yushigou in Northern Qilian Mountain

1.
Research Center for Orogenic Geology/Xi'an Center of Geological Survey, Geological Survey of China, Xi'an 710054, Shaanxi, China
2.
MLR Key Laboratory of Magmatic Ore Deposits Genetic Models and Exploration/Xi'an Center of Geological Survey, Geological Survey of China, Xi'an 710054, Shaanxi, China

Received Date: 07 July 2017

Revised Date: 05 February 2018

Publish Date: 25 April 2018

Abstract

Abstract

The Yushigou ophiolite in Northern Qilian Mountain, which has developed relatively complete and typical ophiolite rock association, has received widespread attention. The authors conducted the chronological study of zircons from the syenite by means of LA-ICP-MS U-Pb. The weighted mean age of the zircons is 522.7±5.3Ma, which belongs to the Early Cambrian and confirms the earliest record of alkaline intrusive magmatic activity in Northern Qilian Mountain. At the same time, this age gives a constraint that the upper limit of the age of Yushigou ophiolite should be no later than 522.7Ma.
- Yushigou ophiolite /
- syenite /
- LA-ICP-MS zircon U-Pb dating /
- Northern Qilian Mountain

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References

[1]	王荃, 刘雪亚.我国西部祁连山区的古海洋地壳及其大地构造意义[J].地质科学, 1976, 1:42-55. Google Scholar
[2]	肖序常, 陈国铭, 朱志直.祁连山古蛇绿岩带的地质构造意义[J].地质学报, 1978, 52(4):281-95. Google Scholar
[3]	冯益民, 何世平.祁连山大地构造与造山作用[M].北京:地质出版社, 1996. Google Scholar
[4]	冯益民, 何世平.北祁连蛇绿岩的地质地球化学研究[J].岩石学报, 1995, S1:125-140. Google Scholar
[5]	张旗, 周国庆, 王焰.中国蛇绿岩的分布、时代及其形成环境[J].岩石学报, 2003, 19(1):1-8. Google Scholar
[6]	张旗, 周国庆.中国蛇绿岩[M].北京:科学出版社, 2001. Google Scholar
[7]	张旗, 孙晓猛, 周德进, 等.北祁连蛇绿岩的特征、形成环境及其构造意义[J].地球科学进展, 1997, 12(4):366-393. Google Scholar
[8]	张旗, 贾秀琴.北祁连大岔大坂蛇绿岩的地球化学特征及其成因[J].中国科学:地球科学, 1998, 19(1):30-34. Google Scholar
[9]	张招崇, 毛景文, 杨建民, 等.北祁连西段中元古代蛇绿岩的发现及地质意义[J].矿物岩石地球化学通报, 1998, 17(2):114-118. Google Scholar
[10]	宋述光, 张贵宾, 张聪, 等.大洋俯冲和大陆碰撞的动力学过程:北祁连-柴北缘高压-超高压变质带的岩石学制约[J].科学通报, 2013, 58(23):2240-2245. Google Scholar
[11]	Song S G, Niu Y L, Su L, et al. Tectonics of the North Qilian orogen, NW China[J]. Gondwana Research, 2013, 23(4):1378-1401. doi: 10.1016/j.gr.2012.02.004 CrossRef Google Scholar
[12]	Tseng C Y, Yang H J, Yang H Y, et al. The Dongcaohe ophiolite from the North Qilian Moun-tains:A fossil oceanic crust of the Paleo-Qilian ocean[J]. Science Bulletin, 2007, 52(17):2390-2401. doi: 10.1007/s11434-007-0300-3 CrossRef Google Scholar
[13]	Xia X H, Song S G, Niu Y L. Tholeiite-Boninite terrane in the North Qilian suture zone:Implications for subduction initiation and back-arc basin development[J]. Chemical Geology, 2012, 328(11):259-277. Google Scholar
[14]	Xia X H, Song S G. Forming age and tectono-petrogenises of the Jiugequan ophiolite in the North Qilian Mountain, NW China[J]. Science Bulletin, 2010, 55(18):1899-1907. doi: 10.1007/s11434-010-3207-3 CrossRef Google Scholar
[15]	孟繁聪, 张建新, 郭春满, 等.大岔大坂MOR型和SSZ型蛇绿岩对北祁连洋演化的制约[J].岩石矿物学杂志, 2010, 29(5):453-466. Google Scholar
[16]	夏小洪, 孙楠, 宋述光, 等.北祁连西段熬油沟二只哈拉达坂蛇绿岩的形成环境和时代[J].北京大学学报(自然科学版), 2012, 48(5):757-769. Google Scholar
[17]	相振群, 陆松年, 李怀坤, 等.北祁连西段熬油沟辉长岩的锆石SHRIMP U-Pb年龄及地质意义[J].地质通报, 2007, 26(12):1686-1691. Google Scholar
[18]	史仁灯, 杨经绥, 吴才来, 等.北祁连玉石沟蛇绿岩形成于晚震旦世的SHRIMP年龄证据[J].地质学报, 2004, 78(5):649-657. Google Scholar
[19]	武鹏, 李向民, 徐学义, 等.北祁连山扎麻什地区东沟蛇绿岩LA-ICP-MS锆石U-Pb测年及其地球化学特征[J].地质通报, 2012, 31(6):896-906. Google Scholar
[20]	夏林圻, 夏祖春, 徐学义.北祁连山海相火山岩岩石成因[M].北京:地质出版社, 1996. Google Scholar
[21]	夏林圻.祁连山及邻区火山作用与成矿[M].北京:地质出版社, 1998. Google Scholar
[22]	宋述光.北祁连山俯冲杂岩带的构造演化[J].地球科学进展, 1997, 12(4):351-365. Google Scholar
[23]	侯青叶, 赵志丹, 张宏飞, 等.北祁连玉石沟蛇绿岩印度洋MORB型同位素组成特征及其地质意义[J].中国科学:地球科学, 2005, 35(8):710-719. Google Scholar
[24]	夏林圻.北祁连山构造-火山岩浆-成矿动力学[M].北京:中国大地出版社, 2001. Google Scholar
[25]	Xia L Q, Xia Z C, Xu X Y. Magmagenesis in the Ordovician backarc basins of the Northern Qilian Mountains, China[J]. Geological Society of America Bulletin, 2003, 115(12):1510-1522. doi: 10.1130/B25269.1 CrossRef Google Scholar
[26]	Xia L Q, Xia Z C, Zhao J T, et al. Determination of properties of Proterozoic continental flood basalts of western part from North Qilian Mountains[J]. Science China Earth Sciences, 1999, 42(5):506-514. doi: 10.1007/BF02875244 CrossRef Google Scholar
[27]	Xia L Q, Li X M, Yu J Y, et al. Mid-late neoproterozoic to early paleozoic volcanism and tectonic evolution of the Qilianshan, NW China[J]. Geo. Res. J., 2016, 9/12:1-41. Google Scholar
[28]	许志琴, 杨经缓, 吴才来, 等.柴达木北缘超高压变质带形成与折返的时限及机制[J]. Acta Geologica Sinica, 2003, 77(2):163-176. Google Scholar
[29]	Zhiqin X, Jianxin Z, Haibin L. Architecture and orogeny of the northern Qilian orogenic belt, northwestern China[J]. Journal of the Geological Society of China (Taibei), 2000, 34(1):125-141. Google Scholar
[30]	柳小明, 高山, 袁洪林, 等. 193nm LA-ICP-MS对国际地质标准参考物质中42种主元素和微量元素的分析[J].岩石学报, 2002, 18(3):408-418. Google Scholar
[31]	Claesson S, Vetrin V, Bayanova T, et al. U-Pb zircon ages from a Devonian carbonatite dyke, Kola peninsula, Russia:a record of geological evolution from the Archaean to the Palaeozoic[J]. Lithos, 2000, 51(1/2):95-108. Google Scholar
[32]	Belousova E, Griffin W, O'reilly S Y, et al. Igneous zircon:trace element composition as an indicator of source rock type[J]. Contributions to Mineralogy and Petrology, 2002, 143(5):602-22. doi: 10.1007/s00410-002-0364-7 CrossRef Google Scholar
[33]	夏林圻, 李向民, 余吉远, 等.祁连山新元古代中-晚期至早古生代火山作用与构造演化[J].中国地质, 2016, 43(4):1087-1138. Google Scholar
[34]	夏林圻, 夏祖春, 徐学义.北祁连山构造-火山岩浆演化动力学[J].西北地质科学, 1995, 16(1):1-28 Google Scholar
[35]	Upadhyay D, Raith M M, Mezger K, et al. Mesoproterozoic riftrelated alkaline magmatism at Elchuru, Prakasam Alkaline Province, SE India[J]. Lithos, 2006, 89(3/4):447-477. Google Scholar
[36]	Shaw C S J. The petrology of the layered gabbro intrusion, eastern gabbro, Coldwell alkaline complex, Northwestern Ontario, Canada:evidence for multiple phases of intrusion in a ring dyke[J]. Lithos, 1997, 40(2/4):243-259. Google Scholar