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Table 3 Outcrops where fault-slip analysis yielded indications of shortening (compare Figs. 12, 13)

From: Outcrop-scale fracture systems in the Alpine foreland of central northern Switzerland: kinematics and tectonic context

Outcrop signature

N

n

Right-Dihedra fault-slip analysis

Tectonic regime

Age constraint

σ1

σ2

σ3

Azi.

Pl.

Azi.

Pl.

Azi.

Pl.

1

27

1

337

7

86

68

244

21

Strike-slip

Pre- to post folding

1

21

1

336

9

82

62

242

27

Transpression

Post-folding

1

6

0

340

2

81

82

250

8

Strike-slip

Pre-folding

2

33

3

170

2

53

86

260

3

Strike-slip

Pre-folding

3

16

4

340

9

71

7

198

79

Compression

Pre- to post folding

4

18

0

157

4

49

77

248

13

Transpression

Pre- to post folding

4

6

0

161

6

69

11

278

77

Compression

Post-folding

4

12

0

156

3

37

84

246

5

Strike-slip

Pre-folding

5

21

5

341

0

246

86

71

4

Strike-slip

Pre- to post folding

6

32

3

341

5

217

81

72

8

Transpression

Pre-folding

7

21

2

174

7

35

81

256

6

Transpression

 

8

29

4

157

2

48

85

247

5

Strike-slip

 

9

41

1

175

3

346

87

85

0

Transpression

 

10

32

0

162

3

29

86

252

3

Transpression

 

11

10

2

166

0

72

82

256

8

Strike-slip

Pre-folding

13

9

2

347

6

83

48

252

42

Transpression

Pre-folding

14

6

1

210

23

301

3

37

67

Compression

Post-folding

14

22

4

150

0

57

84

240

6

Strike-slip

Pre-folding

15

23

4

344

5

238

73

75

16

Transpression

 

16

14

2

20

5

139

81

289

8

Strike-slip

Pre-folding

17

19

6

339

9

69

1

166

81

Compression

Post-folding

18

34

3

337

8

81

62

243

27

Transpression

 

19

37

0

339

10

96

68

246

19

Transpression

 

20

23

6

332

1

282

87

62

3

Transpression

 

21

11

0

311

5

193

80

41

9

Strike-slip

 

22

17

1

138

3

348

87

229

1

Strike-slip

 

23

21

1

320

1

101

89

230

1

Strike-slip

 

24

15

3

145

2

259

85

55

4

Strike-slip

Pre- to post-folding

25

6

0

129

15

302

75

38

2

Strike-slip

Pre-folding

25

9

3

185

4

21

86

275

1

Strike-slip

Pre-folding

26

10

1

181

2

360

88

91

0

Strike-slip

 

27

39

5

344

5

129

84

254

3

Strike-slip

 

28

14

3

351

2

133

88

261

1

Strike-slip

Post-folding

29

17

2

337

6

212

79

68

9

Strike-slip

 

30

30

0

171

2

68

81

261

9

Strike-slip

 

31

9

1

329

4

188

85

59

3

Strike-slip

Pre-folding

32

41

1

170

2

284

86

80

3

Strike-slip

 

33

8

3

197

5

104

32

295

58

Compression

Post-folding

34

26

4

6

4

274

26

104

64

Transpression

Pre-folding

34

20

3

42

3

154

30

311

6

Transpression

Pre-folding

35

30

2

192

3

78

83

282

7

Transpression

 

36

12

1

2

3

272

2

143

86

Compression

Post-folding

36

22

4

342

2

119

88

252

2

Strike-slip

Pre-folding

37

41

5

2

7

98

40

263

49

Transpression

Post-folding

38

26

2

349

4

249

66

81

23

Transpression

Post-folding

39

20

1

143

2

245

79

53

11

Transpression

 

39

14

0

16

7

248

79

107

8

Strike-slip

 

41

22

10

11

5

264

73

103

16

Transpression

Pre-folding

42

25

6

331

10

86

68

238

20

Transpression

Pre- to post folding

42

6

1

325

12

62

26

213

60

Compression

Post-folding

42

19

5

333

7

120

82

243

4

Strike-slip

Pre-folding

43

34

0

342

2

181

88

72

1

Strike-slip

 

44

8

0

326

6

143

84

236

0

Strike-slip

 

45

28

3

168

0

261

83

78

7

Strike-slip

 

46

23

1

351

1

237

88

81

2

Strike-slip

 

47

12

2

155

4

278

83

64

6

Strike-slip

 

48

19

4

6

1

226

89

96

1

Strike-slip

Post-tilting

49

13

0

335

5

199

84

65

4

Strike-slip

 

50

9

2

202

2

318

86

112

4

Strike-slip

 

51

13

1

13

3

157

86

283

3

Strike-slip

 

52

23

1

161

1

257

77

70

13

Strike-slip

Post-tilting

57

20

4

2

5

110

74

271

15

Strike-slip

Post-tilting

  1. Italic letters show faul-slip analyses for fracture subsets representing pre- and post folding states of deformations that yielded identical results (compare Fig. 13)
  2. N number of relevant fracture measurements, n number of fracture measurements with no shear sense information. σ1 > σ2 > σ3 maximum, intermediate and minimum principal stress axes, Azi Azimuth, Pl. Plunge