Physiochemical Restrictions of Mineral Zoning of Sediment-Hosted Stratiform Copper Deposit in SW China

Table 1

Homogeneous temperature of fluid inclusions of minerals in the Dayao deposit.

Mineral	Metallogenesis	Sample numbers	Gas-liquid ratio (%)	Homogeneous temperature (°C)		Source of date
				Range	Average
Calcite	Diagenesis	13	5~15	116~145	133	(1)
Quartz	Reformation	2	5~15	158~205	182
		2	25~45	302~332	317
Quartz	Diagenesis	14	2~30	96~137	120, 260~300	(2)
	Main reformation	15	2~25	123~209	149
	Minor reformation	6	2~25	97~129	113

Note. Source of data: (1) Ran and Zhuang [49], tested by the center analysis room of Zhongnan University; (2) Wu [62], tested by Nanjing University.