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Syenite from
Baima V-Ti-Fe deposit, Miyi County, Panzhihua, Sichuan, China


Locality type:Deposit
Classification
Type:Syenite
Age information
Maximum recorded age:259 ± 5 Ma
Minimum recorded age:258 ± 4 Ma
Sample ages:
Recorded ageGeologic TimeSampleDating method
1259 ± 5 to 258 ± 4 MaLopingian - U-Pb
Sample references:
1 -
Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Syenite data
Locality Data:Click here to view Baima V-Ti-Fe deposit, Miyi County, Panzhihua, Sichuan, China
Data Identifiers
Mindat Occurrence Record ID:1329267
Long-form Identifier:1:3:1329267:4
GUID (UUID V4):bca0e9e0-23d1-49a8-8965-b02ea0ca8c82
Nearest other occurrences of Syenite
23.7km (14.8 miles) ⓘDalucao REE deposit, Dechang County, Liangshan Yi, Sichuan, China
26.8km (16.6 miles) ⓘMaomaogou Complex, Miyi County, Panzhihua, Sichuan, China
31.7km (19.7 miles) ⓘXiaoheiqing Nb-Ta deposit, Huili County, Liangshan Yi, Sichuan, China
33.7km (21.0 miles) ⓘHongge V-Ti-Fe deposit, Yanbian County, Panzhihua, Sichuan, China
37.1km (23.1 miles) ⓘBaicao Nb-Ta deposit, Huili County, Liangshan Yi, Sichuan, China
39.5km (24.5 miles) ⓘLuku Complex, Yanbian County, Panzhihua, Sichuan, China
51.5km (32.0 miles) ⓘPanzhihua Fe-V-Ti-(PGE) deposit, Dong District, Panzhihua, Sichuan, China
51.5km (32.0 miles) ⓘLiushaxiang, Puge County, Liangshan Yi, Sichuan, China
References
Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133.
Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217.
Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55.
Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
Zhong, H., Campbell, I. H., Zhu, W. G., Allen, C. M., Hu, R. Z., Xie, L. W., & He, D. F. (2011). Timing and source constraints on the relationship between mafic and felsic intrusions in the Emeishan large igneous province. Geochimica et Cosmochimica Acta, 75(5), 1374-1395.
 
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