Locality type: | Complex |
Classification |
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Type: | Granite |
Age information |
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Maximum recorded age: | 308 ± 14 Ma |
Minimum recorded age: | 303 ± 26 Ma |
Sample ages: | | Recorded age | Geologic Time | Sample | Dating method |
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1 | 308 ± 14 to 303 ± 26 Ma | Pennsylvanian | - | Rb-Sr |
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Sample references: | |
1 | - | Han, B. F., Wang, S. G., Jahn, B. M., Hong, D. W., Kagami, H., & Sun, Y. L. (1997). Depleted-mantle source for the Ulungur River A-type granites from North Xinjiang, China: geochemistry and Nd |
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Confirmation |
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Validity: | Believed Valid |
Data |
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Mineral Data: | Click here to view Granite data |
Locality Data: | Click here to view Ulungur river peralkaline granites, Aletai Prefecture (Altay Prefecture), Yili Hasake Autonomous Prefecture (Ili Kazakh Autonomous Prefecture), Xinjiang, China |
Data Identifiers |
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Mindat Occurrence Record ID: | 1327686 |
Long-form Identifier: | 1:3:1327686:1 |
GUID (UUID V4): | b3fa42e2-68aa-4ebf-a422-7c828adeb38f |
Nearest other occurrences of Granite |
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63.0km (39.2 miles) | ⓘSuo'erkuduke Cu-(Mo) deposit (Suorkuduk Cu-(Mo) deposit; Sorkuduk Cu-(Mo) deposit; Xorkuduk Cu-(Mo) deposit), Fuyun Co. (Koktokay Co.), Aletai Prefecture (Altay Prefecture), Yili Hasake Autonomous Prefecture (Ili Kazakh Autonomous Prefecture), Xinjiang, China |
99.5km (61.8 miles) | ⓘKoktokay No. 3 pegmatite (Altay No. 3 pegmatite), Altay Mine, Koktokay pegmatite field (Keketuohai pegmatite field), Fuyun Co. (Koktokay Co.), Aletai Prefecture (Altay Prefecture), Yili Hasake Autonomous Prefecture (Ili Kazakh Autonomous Prefecture), Xinjiang, China |
References |
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Han, B. F., Wang, S. G., Jahn, B. M., Hong, D. W., Kagami, H., & Sun, Y. L. (1997). Depleted-mantle source for the Ulungur River A-type granites from North Xinjiang, China: geochemistry and Nd–Sr isotopic evidence, and implications for Phanerozoic crustal growth. Chemical Geology, 138(3-4), 135-159. |
Reference Search (possible matching items) |
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| Han, Bao-fu, Wang, Shi-guang, Jahn, Bor-ming, Hong, Da-wei, Kagami, Hiroo, Sun, Yuan-lin (1997) Depleted-mantle source for the Ulungur River A-type granites from North Xinjiang, China: geochemistry and Nd–Sr isotopic evidence, and implications for Phanerozoic crustal growth. Chemical Geology, 138 (3) 135-159 doi:10.1016/s0009-2541(97)00003-x | Journal (article/letter/editorial) | Depleted-mantle source for the Ulungur River A-type granites from North Xinjiang, China: geochemistry and Nd–Sr...of Geology, Peking UniÕersity, Beijing, 100871, China Geosciences Rennes, UniÕersite´ de Rennes I, AÕenue...Academy of Geological Sciences, Beijing, 100037, China Institute for Study of the Earth’s Interior, Okayama...December 1996 Abstract The Ulungur River granites from North Xinjiang, China, display two petrological...trends: Ž1. a peralkaline trend, composed of alkali amphibole- and alkali pyroxene-bearing granites and dykes |
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