Formation Age and Evolution Time Span of the Koktokay No. 3 Pegmatite, Altai, NW China: Evidence from U–Pb Zircon and 40Ar–39Ar Muscovite Ages. Issue 3 (July 2015)

• Record Type: Journal Article
• Authors: Zhou, Qifeng; Qin, Kezhang; Tang, Dongmei; Tian, Ye; Cao, Mingjian; Wang, Chunlong
• Is Part Of: Resource geology. Volume 65:Issue 3(2015:Jul.)
• Page Start: 210
• Page End: 231
• Publication Date: 2015-07
• Subjects: Mining geology -- Periodicals; Mining geology -- Pacific Area -- Periodicals; Mining geology -- Asia -- Periodicals; Geochemistry -- Periodicals; Environmental geology -- Periodicals; 553
• DOI: 10.1111/rge.12067
• Languages: English
• ISSNs: 1344-1698

Abstract

<abstract abstract-type="main"> <title>Abstract</title> <p>The Koktokay No. 3 pegmatite is the largest Li–Be–Nb–Ta–Cs pegmatitic rare‐metal deposit of the Chinese Altai orogenic belt, and is famous for its concentric ring zonation pattern (nine internal zones). However, the formation age and evolution time span have been controversial. Here, we present the results of LA‐ICP–MS zircon U–Pb dating and muscovite <sup>40</sup>Ar–<sup>39</sup>Ar dating. Four groups of zircon U–Pb ages (∼210 Ma, ∼193–198 Ma, ∼186–187 Ma and ∼172 Ma) for Zones II, V, VI, VII, and VIII, and a weighed mean <sup>206</sup>Pb/<sup>238</sup>U age of 965 ± 11 Ma for Zone IV are identified. Also, Zones II, IV, and VI have muscovite <sup>40</sup>Ar–<sup>39</sup>Ar plateau ages of 179.7 ± 1.1 Ma, 182.1 ± 1.0 Ma, and 181.8 ± 1.1 Ma, respectively. Considering previous U–Pb age studies (Zones I, V, and VII), the ages of emplacement, Li mineralization peak, hydrothermal stage of the No. 3 pegmatite are in ranges of 193–198 Ma, 184–187 Ma and 172–175 Ma, with weighted mean <sup>206</sup>Pb–<sup>238</sup>U ages of 194.8 ± 2.3 Ma, 186.6 ± 1.3 Ma and 173.1 ± 3.9 Ma, respectively. The No. 3 pegmatite formed in the early Jurassic. The results of xenocrysts suggest that there is another pegmatite forming event of around 210 Ma in the mining district and the old zircon U–Pb ages imply that Neoproterozoic crustal rocks pertain to sources of the No. 3 pegmatite. Including the previous muscovite <sup>40</sup>Ar–<sup>39</sup>Ar age studies (Zones I and V), a cooling age range of 177–182 Ma is considered as the time of hydrothermal stage and end of formation. The evolution process of the No. 3 pegmatite lasted 16 Ma. Therein, the magmatic stage continued for 9–11 Myr and the magmatic–hydrothermal transition and hydrothermal stages were sustained at 5–7 Ma. These time spans are long because of huge scale, cupola shape, large formation depth, and complex internal zoning patterns and formation processes. Considering some pegmatite dikes in the Chinese Altai, there is an early Jurassic pegmatite forming event.</p> </abstract>