Quartzo-feldspar vein Found In Nassarawa State

The location is located along Akwanga – Lafia road. The location is an outcrop of older granite compare to the one we saw at the other outcrop (location 3). The granite occurs in schist i.e. they are foliated (pan-African) with alignment of some minerals. 

#There is also a horizontal joint that is cementing them together and the horizontal joint helps in terms of breaking them to aggregates for construction work and there are also vertical joint in the formation and quartz veins is also there. 

        Measurement of features taken here are as follows;

Thickness of the quartz vein;

(1)    5cm (2) 4cm (3) 2.5cm (4) 3cm

Trend:

Strike                       N34 – N214

Dip direction            124 SE

Dip amount             540

The G.P.S Reading

Latitude – 80, 44′ 08″N

Longitude- 80, 32′ 46″E

Elevation    27M

Table 1:   Showing the trend joint were measured in terms

               of their dimension

S/NO

    TREND OF JOINT

1

N275O     

N95O

2

N102O       

N283O

3

N347O       

N168O

4

N355O       

N175O

5

N348O     

N167O

6

N357O       

N177O

7

N54O           

N234O

8

N285O       

N105O

9

N346O       

N168O

10

N13O          

N193O

11

N140O                

N160O

12

N339O         

N159O

13

N269O      

N91O

14

N345O      

N165O

15

N78O         

N257O

16

N93O         

N183O

17

N262O

N82O

18

N248O     

N67O

19

N293O    

N112O

20

N255O    

N75O

            

Table 2:   Showing the cumulative frequency of different

on trend of joint

S/N

Class interval

Frequency

Total frequency

1

0 – 30

0

0

2

31 – 60

0

0

3

61 – 90

3

15

4

91 – 120

4

20

5

121 – 150

0

0

6

151 – 180

8

40

7

181 – 210

2

10

8

211 – 240

1

5

9

241 – 270

1

5

10

271 – 300

1

5

Related Posts: NASSARAWA STATE, ROCKS

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