Diamond-barren kimberlite and lamproite pipes or dikes along a 70 x 30 km NW-trending K-rich ultramafic belt. The kimberlites and lamproites intruded Sinian-Ordovician carbonatites and shales.
Ref.:
- Zhang Hong-Fu, Min Sun, Lu Feng-Xiang, Zhou Xin-Hua, Zhou Mei-Fu, Liu Yong-Shun, and Zhang Guo-Hui (2001): Geochemical significance of a garnet lherzolite from the Dahongshan kimberlite, Yangtze Craton, southern China. Geochemical Journal 35(5), 315-331.
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Map Reference: 31°0'N , 113°0'E
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Mineral List:10 entries listed. 4 valid minerals.
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