The Fe-Zn Isotopic Characteristics and Fractionation Models: Implications for the Genesis of the Zhaxikang Sb-Pb-Zn-Ag Deposit in Southern Tibet

Table 1

EPMA data for Mn-Fe carbonate and quartz from the Zhaxikang deposit.

Sample number	SiO2 (%)	Na2O (%)	K2O (%)	TiO2 (%)	Al2O3 (%)	MgO (%)	CaO (%)	FeO (%)	MnO (%)	SrO (%)	BaO (%)	CO2 (%)	Total (%)	Mineral
9-3-4	0.015	0.005	0.007	0.011	0.003	1.231	2.061	28.598	29.840	0.007	0.057	38.164	99.999	Mcar
9-3-5	0.024	0.109	0.027	–	0.010	1.080	2.151	28.372	30.582	–	0.002	37.643	100.000	Mcar
9-8-8	0.002	0.031	0.007	–	–	1.276	1.978	27.341	31.338	0.010	0.022	37.993	99.998	Mcar
9-8-9	–	0.025	–	–	0.008	1.189	1.144	31.806	27.514	–	–	38.316	100.002	Mcar
ZXK-1-6	0.001	0.028	0.001	0.022	–	1.207	5.178	24.070	30.717	–	–	38.775	99.999	Mcar
ZXK-1-7	0.028	0.011	0.019	0.036	0.014	1.995	2.940	29.639	27.943	–	0.017	37.358	100.000	Mcar
ZXK-2-7	0.005	0.039	–	0.055	–	1.236	5.542	27.235	27.604	–	–	38.285	100.001	Mcar
ZXK-2-8	–	0.051	–	0.012	0.010	1.140	4.298	24.287	32.694	–	0.008	37.500	100.000	Mcar
ZXK-2-9	0.009	0.049	0.008	–	0.037	1.552	1.946	26.739	30.968	0.007	0.013	38.673	100.001	Mcar
ZXK-2-10	0.015	–	–	0.023	0.012	1.119	4.849	23.562	32.232	–	0.003	38.185	100.000	Mcar
ZXK-2-11	97.000	0.026	0.025	–	0.219	0.028	0.018	0.020	—	–	–	2.664	100.000	Qtz

Notes. (1) Mcar = Mn-Fe carbonate; Qtz = quartz; (2) for the sampling points, please see Figure 5.