The Structure of the Kuenlunkuan Granodiorite and its Relation to the Formation of the Ore-bearing Quartz Veins
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Abstract:
The Kuenlunknan Granodiorite, whick occurs slightly to the west of the apex of the Kuangi are, is exposed at the southern end of the Tamingshan anticline. The mass is injeated into the Lower Devonian and Pre-Devonian rocks. This pluton is
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Y. C. HSU.1943. The Structure of the Kuenlunkuan Granodiorite and its Relation to the Formation of the Ore-bearing Quartz Veins[J]. Acta Geologica Sinica(),23(Z1):77-85,87,88
