Analyses of franklinite

 

 

Analyses of franklinite
 

1

2

3

4

5

6

7

8

Fe2O3

66.00

66.10

68.88

66.07

66.12

65.05

65.93

66.05

Mn2O3

16.00

14.96

 

12.24

11.98

14.77

11.34

12.23

ZnO

17.00

17.42

10.81

21.39

21.77

23.30

21.82

21.88

MnO    

16.32

          
Al2O3    

0.73

         
SiO2  

0.20

0.40

0.29

0.13

0.30

   
H2O  

0.56

           
 

89.00

99.24

97.14

99.99

100.00

103.42

99.09

100.16

1. Franklinite, Franklin. P. Berthier (3), analyst. (Original description.)
2. Franklinite, Sterling Hill. Thomas Thomson (23), analyst.
3. Franklinite. Hermann Abich (26), analyst.
4, 5. Franklinite. Dickerson, analyst, in C. T. Jackson (58).
6. Franklinite. G. J. Brush (76), analyst.
7. Franklinite crystals. C. F. Rammelsberg (93), analyst.
8. Average of three specimens of massive franklinite. C. F. Rammelsberg (93), analyst.
 

9

10

11

12

13

14

15

16

Fe2O3

63.40

67.42

60.52

56.57

67.38

66.34

66.20

66.58

Mn2O3

4.44

   

6.79

10.52

   

12.40

  
ZnO

23.11

6.78

19.44

15.91

16.28

20.26

21.00

20.77

MnO

10.46

9.53

12.81

16.37

16.38

12.31

 

9.96

FeO  

15.65

             
Al2O3  

0.65

           

0.80

None

SiO2

0.17

0.08

          

0.72

H2O               

0.71

CaO               

0.43

MgO               

0.34

 

101.58

100.11

99.56

99.37

100.04

98.91

100.40

99.51

9. Average of two feebly magnetic crystals, Franklin. G. H. Seyms (109), analyst.
10. Average of four strongly magnetic crystals, Sterling Hill. G. H. Seyms (109), analyst.
11. Granular ore, specific gravity 5.215, Franklin. G. C. Stone (131), analyst.
12. Massive ore, specific gravity 5.187, Franklin. G. C. Stone (131), analyst.
13. Crystals, specific gravity 5.136, Sterling Hill. G. C. Stone 1131), analyst.
14. Crystals, specific gravity 5.074. G. C. Stone (131), analyst.
15. Franklinite. Franz von Kobell (92), analyst. 16. Crystals, specific gravity 5.09. State of oxidation of iron and manganese not known. W. T. Schaller (Palache, 195), analyst.

 

 


 
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