Vote for your favorite mineral in #MinCup26! - Quartz vs. Asagiite
It's a classic vs a newbie as the most common named mineral in the crust Quartz is up against an exceedingly-rare sea foam-green mineral discovered just a few years ago Asagiite.
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Calcite from
Daolinshan, Xiaoshan District, Hangzhou, Zhejiang, China


Locality type:Complex
Classification
Species:Calcite
Formula:CaCO3
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Calcite data
Locality Data:Click here to view Daolinshan, Xiaoshan District, Hangzhou, Zhejiang, China
Data Identifiers
Mindat Occurrence Record ID:1331635
Long-form Identifier:1:3:1331635:4
GUID (UUID V4):0
Nearest other occurrences of Calcite
17.7km (11.0 miles) ⓘJianglong P deposit, Zhuji Co., Shaoxing, Zhejiang, China
26.6km (16.5 miles) ⓘShixiang P-U deposit, Zhuji Co., Shaoxing, Zhejiang, China
30.6km (19.0 miles) ⓘXiqiu Cu-Zn deposit (Zigiu Cu-Zn deposit), Shaoxing Co., Shaoxing, Zhejiang, China
39.8km (24.7 miles) ⓘHuangshan Mine, Huangshan complex, Zhuji Co., Shaoxing, Zhejiang, China
43.5km (27.0 miles) ⓘZhupu'ao Au-Ag deposit, Pingshui, Shaoxing Co., Shaoxing, Zhejiang, China
43.7km (27.2 miles) ⓘXianlin deposit, Xihu District, Hangzhou, Zhejiang, China
68.4km (42.5 miles) ⓘDongxi P deposit, Tonglu County, Hangzhou, Zhejiang, China
87.9km (54.6 miles) ⓘWujinshan ore deposit, Lin'an District, Hangzhou, Zhejiang, China
90.1km (56.0 miles) ⓘLangcun W-Mo deposit, Anji Co., Huzhou, Zhejiang, China
References
Li, X-H., Li, W-X., Li, Z.X., Ying, L. (2008) 850–790 Ma bimodal volcanic and intrusive rocks in northern Zhejiang, South China: A major episode of continental rift magmatism during the breakup of Rodinia. Lithos, 102 (1-2), 341-357.
Wang, Q., Wyman, D.A., Li, Z.X., Bao, Z.W., Zhao, Z.H., Wang, Y.X., Jian, P., Yang, Y.H., Chen, L.L. (2010) Petrology, geochronology and geochemistry of ca. 780 Ma A-type granites in South China: Petrogenesis and implications for crustal growth during the breakup of the supercontinent Rodinia. Precambrian Research, 178(1-4), 185-208.
 
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