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Sa'ertielike intrusion, Fuyun Co. (Koktokay Co.), Aletai Prefecture (Altay Prefecture), Yili Hasake Autonomous Prefecture (Ili Kazakh Autonomous Prefecture), Xinjiang Autonomous Region, China

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Name(s) in local language(s): 萨尔铁列克岩体, 富蕴县, 阿勒泰地区 (ئالتاي ۋىلايىتى), 伊犁哈萨克自治州 (ئاپتونوم ئوبلاستىئىلى قازاق), 新疆维吾尔自治区, 中国
 
An alkaline granite intrusion, which forms part of the Ulungur river zone. This belt of alkaline granites in northern Xinjiang trends in southeastern direction along the southern bank of the Ulungur river and parallel to the suture zone between the Junggar plate and the Altay orogenic belt. The granites were formed within a short period of time during the latest stage of the Hercynian calc-alkaline magmatic cylcle (Rb-Sr isochron ages: 292-309 Ma), after the syn-collisional S-type and post-collisional uplift I-type granitoids of the Altay region. They compare to post-orogenic A-type alkali granites and mark the end of the Hercynian orogeny in this area.

Mineral List



7 entries listed. 7 valid minerals.

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References

Shiguang Wang, Baofu Han, Dawei Hong, Baoliang Xu, and Yayun Sun (1994): Geochemistry and tectonic significance of alkali granites along Ulungur river, Xinjiang. Scientia Geologica Sinica 29(4), 373-383 (in Chinese with English abstract).

 
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