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Table 1 A summary of discontinuities’ characterization in the study area

From: Application of paleostress analysis for the identification of potential instability precursors within the Benue Trough Nigeria

Site ID

Locality

Rock type

Fracture set

No. of fractures

Strike

Dip

Average fracture spacing (m)

Fracture infilling

002

Itigidi

Sandstone

JC-1

30

300–310

80–90

1.5

Ferruginized

006

Aboine River Akpoha

Shale

JT-1

38

340–355

80–90

0.1

None

JT-2

8

310–320

85–90

0.3

JT-4

3

260–270

80–90

2.0

008

Amaseri Ridge

Sandstone

JT-1

5

330–360

80–90

0.7

None

JS-1

9

045–060

45–60

1.5

012

Ohaozara

Sandstone

JT-1

40

330–350

85–90

0.15

None

013

Asu River Ohaozara

Shale

JT-1

156

330–360

70–90

0.1

None

JT-2

50

300–330

55–80

0.1

JT-3

3

290–300

85–90

0.1

JS-1

11

040–060

25–30

45–60

70–75

0.6

JS-2

10

060–080

60–65

80–85

0.55

014

Asu River Akpoha

Shale

JT-2

100

310–330

70–80

0.05

None

JS-1

13

40–50

30–35

55–60

2.0

JS-4

29

280–300

40–45

55–60

1.6

017

Aboine River Isinkoro

Shale

JT-1

18

355–050

90

0.2

None

JT-2

51

310–340

70–75

0.2

JT-3

1

290–300

75–80

0.5

021

Aba-Omega Ugep Road

Sandstone

JT-1

12

350–360

70–75

0.2

None

JT-2

9

320–330

80–85

0.2

026

Asu River

Shale

JT-2

28

330–340

70–80

0.2

None

JT-2

57

320–340

75–80

0.3

JS-6

55

340–350

45–50

0.3

JS-5

59

310–320

30–35

0.2

 

JT-1

35

330–340

60–65

0.2

027

Afikpo Road

Sandstone

JS-3

5

020–030

40–45

1.0

Ferruginized

JC-1

8

280–290

55–60

1.0