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Table 1 Table compiles the distance of each sample from the crater center; apparent crystallite size is (D); bulk magnetic susceptibility (χ); Curie temperature (TC); the ratios: remanence of coercivity to coercive force (Hcr/Hc) and the remanent magnetization to saturation remanence (Mrs/Ms)

From: Curie temperature of weakly shocked target basalts at the Lonar impact crater, India

Sample

Distance (km)

FWHM 2θ (°)

D (nm)

χ (10−3 SI)

TC (°C)

Hcr/Hc

Mrs/Ms

MDF (mT)

Coercivity

34

0.776

0.39

21.53

46.8

505.8

2.066

0.207

38

High

25

0.851

50.7

517.4

1.365

0.151

12

Medium

7

0.868

0.39

21.23

19.6

506.5

1.594

0.235

22

High

4

0.884

 

44.4

461.6

2.327

0.107

8

Low

1

0.888

0.29

28.47

26.5

479

1.414

0.178

25

High

33

0.891

0.35

23.74

32.5

504.8

2.156

0.19

44

High

23

0.893

0.29

28.85

37.4

548.6

1.702

0.302

28

High

26

0.925

31.1

513.1

2.124

0.207

50

High

31

0.96

53.1

537.8

2.352

0.202

9

Medium

21

0.984

39

532.5

2.523

0.133

30

High

32

1.011

30.4

510.6

2.106

0.221

31

High

14

1.321

61.7

498

1.241

0.146

8

Low

22

1.328

0.25

33.45

27.2

538.3

1.057

0.373

31

High

20

1.375

0.30

27.35

21.8

535.6

1.201

0.04

58

High

19

1.652

0.26

32.16

19.2

562

1.62

0.138

50

High

11

1.702

0.24

35.38

28.8

559

2.011

0.204

61

High

12

1.702

48.8

525.5

1.257

0.173

8

Low

10

1.818

75.3

552.5

0.174

0.17

9

Medium

8

2.019

0.43

19.60

35.5

475.6

1.293

0.171

28

High

16

2.413

73.1

536.6

0.388

0.259

8

Low

17

2.542

59.7

521.3

2.672

0.086

6

Low

  1. The median destructive field (MDF) and the coercivity estimates are taken from Agarwal et al. (2016)