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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Brecciated andesite from
Bailingshan Fe-(Cu) deposit, Shanshan Co., Turpan, Xinjiang, China


Locality type:Deposit
Classification
Type:Brecciated andesite
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Brecciated andesite data
Locality Data:Click here to view Bailingshan Fe-(Cu) deposit, Shanshan Co., Turpan, Xinjiang, China
Data Identifiers
Mindat Occurrence Record ID:1497217
Long-form Identifier:1:3:1497217:5
GUID (UUID V4):0
Nearest other occurrences of Brecciated andesite
23.1km (14.3 miles) ⓘHeijianshan Fe–Cu (–Au) deposit, Shanshan Co., Turpan, Xinjiang, China
References
Zheng, Jiahao (2020) A synthesis of iron deposits in the eastern Tianshan, NW China. Geoscience Frontiers, 11 (4) 1271-1287 doi:10.1016/j.gsf.2019.11.014
Zhang, Hui; Wang, Yin-Hong; Zhang, Fang-Fang; Liu, Jia-Jun; Sun, Min; Wang, Kang; Zhang, Wei; Zhang, Zhong-Yu; Huang, Yun-Ying (2022) Origin of the subduction-related Late Carboniferous dacitic tuffs associated with the Bailingshan Fe deposit in Eastern Tianshan, NW China: Geochronological, geochemical, and Sr-Nd-Hf-O isotopic constraints. Ore Geology Reviews, 142. 104725 doi:10.1016/j.oregeorev.2022.104725
Wang, Yin-Hong; Zhang, Hui; Seltmann, Reimar; Wang, Kang; Zhang, Fang-Fang; Liu, Jia-Jun; Zhou, Dao-Qing (2026) Arc magmatic evolution of submarine volcanic-hosted iron deposits: Insights from an economic deposit class in the southern Central Asian orogenic belt, Northwest China. Geoscience Frontiers, 17 (5). p.102361. doi:10.1016/j.gsf.2026.102361
Chai, Fengmei; Meng, Qingpeng; Xu, Mengjing; Qi, Dongmei; Zhao, Haitao (2026) Multiple-Stage Mineralization at the Bailingshan Volcanic-Hosted Iron Deposit, Xinjiang, NW China: Constraints from Garnet U-Pb and Amphibole Ar-Ar Geochronology and Garnet Geochemistry. Minerals, 16 (8). doi:10.3390/min16080831
 
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