Late Paleozoic crustal growth and tectonic evolution in Balkhash metallogenic belt(Kazakhstan), Central Asia | |
Liu, G (Liu Gang); Chen, XH (Chen XuanHua); Dong, SW (Dong ShuWen); Chen, ZL (Chen ZhengLe); Han, SQ (Han ShuQin); Yang, Y (Yang Yi); Ye, BY (Ye BaoYing); Shi, W (Shi Wei) | |
刊名 | ACTA PETROLOGICA SINICA |
2012 | |
卷号 | 28期号:7页码:1995-2008 |
关键词 | Crustal growth Tectonic setting Sr-Nd-Pb isotope Balkhash metallogenic belt |
ISSN号 | 1000-0569 |
英文摘要 | The Balkhash metallogenic belt in Kazakhstan is a famous porphyritic Cu-Mo metallogenic belt in the Central Asian metallogenic domain. The Late Paleozoic granitoids from Balkhash metallogenic belt are mainly of high-K calc-alkaline and I-type granites, with shoshonite in the late stage. Geochemistry analyses and tectonic discrimination show a change of tectonic setting from syn-collision and volcanic arc in Carboniferous to post-collision in Permian. The Late Paleozoic granitoids from Bony porphyry deposit formed in classical island-arc environment, though that from Kounrad, Aktogai and Sayak are adakitic. The epsilon(Nd)(t) values for the Late Paleozoic granitoids here are between -5.87 and +5.94, and epsilon(Sr)(t) values from -17.16 to +51.10. The continental crustal growth histories are different on the both sides of Central Balkhash fault. On the east side, epsilon(Nd)(t) values from Aktogai and Sayak are very high with character of depleted mantle, suggesting the crustal growth in the Lite Paleozoic. On the west side, epsilon(Nd)(t) values from Borly and Kounrad are slightly low, suggesting the existence of the New Proterozoic basement and the mixing of crust and mantle during magmatism. The granitoids have Pb-206/Pb-204, Pb-207/Pb-204, and Pb-208/Pb-204 values ranging in 18.3346 similar to 20.9929, 15.5213 similar to 15.7321 and 38.2874 similar to 40.0209, respectively, showing the affinity of the Late Paleozoic magmatism in Balkhash with that in Tianshan, Altai and Junggar areas. |
学科主题 | 构造地质学 |
WOS关键词 | PORPHYRY COPPER-DEPOSITS ; ISOTOPIC EVIDENCE ; CONTINENTAL GROWTH ; NORTHEASTERN CHINA ; FOLD BELT ; S-TYPE ; I-TYPE ; ND ; KAZAKSTAN ; GRANITES |
WOS研究方向 | Geology |
语种 | 中文 |
出版者 | SCIENCE PRESS |
WOS记录号 | WOS:000306631600004 |
内容类型 | 期刊论文 |
源URL | [http://119.78.100.197/handle/2HKVOGP0/39896] |
专题 | 中国地质调查局 |
作者单位 | China Univ Geosci, Beijing 100083, Peoples R China |
推荐引用方式 GB/T 7714 | Liu, G ,Chen, XH ,Dong, SW ,et al. Late Paleozoic crustal growth and tectonic evolution in Balkhash metallogenic belt(Kazakhstan), Central Asia[J]. ACTA PETROLOGICA SINICA,2012,28(7):1995-2008. |
APA | Liu, G .,Chen, XH .,Dong, SW .,Chen, ZL .,Han, SQ .,...&Shi, W .(2012).Late Paleozoic crustal growth and tectonic evolution in Balkhash metallogenic belt(Kazakhstan), Central Asia.ACTA PETROLOGICA SINICA,28(7),1995-2008. |
MLA | Liu, G ,et al."Late Paleozoic crustal growth and tectonic evolution in Balkhash metallogenic belt(Kazakhstan), Central Asia".ACTA PETROLOGICA SINICA 28.7(2012):1995-2008. |
个性服务 |
查看访问统计 |
相关权益政策 |
暂无数据 |
收藏/分享 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。
修改评论