Table 1 Oxygen isotope composition of impact-related materials from this study

From: Zhamanshin astrobleme provides evidence for carbonaceous chondrite and post-impact exchange between ejecta and Earth’s atmosphere

 

δ18O (‰)a

δ17O (‰)

Δ17O (‰)a

n

Tektites

 SBM-11

11.18

5.83

−0.088

1

 SBM-11 replicateb

9.62

5.02

−0.090

1

 SBM-23

10.98

5.72

−0.080

1

 SBM-35

12.46

6.50

−0.084

2

 SBM-44

10.95

5.71

−0.086

2

 SBM-88

12.57

6.55

−0.096

3

 SBM-192

11.79

6.15

−0.085

1

 MM-60

10.85

5.65

−0.092

2

 MM-67

10.84

5.66

−0.070

1

 CHBM-5

11.81

6.15

−0.086

2

 CHBM-6

9.44

4.92

−0.078

1

 CHBM-7b

10.13

5.30

−0.086

2

 MCB-2

12.14

6.33

−0.091

2

 LM-1

11.10

5.79

−0.085

2

 MOLD-SBb

11.08

5.30

−0.105

1

 MOLD-SB replicateb

10.45

5.79

−0.092

1

 MOLD-SB replicateb

11.12

5.47

−0.095

1

Irghizites

 IRG-IZ1

12.76

6.58

−0.170

2

 IRG-IZ3

11.85

6.12

−0.145

2

 IRG-IZ3 replicate

13.36

6.92

−0.141

1

 IRG-IZ3 replicate

13.05

6.76

−0.135

1

 IRG-IZ3 replicateb

12.98

6.76

−0.147

1

 IRG-IZ9

14.42

7.42

−0.198

2

 IRG-IZ9 replicateb

13.59

7.03

−0.201

1

 IRG-IZ9 replicateb

13.49

7.01

−0.173

1

 IR-2

14.24

7.33

−0.200

1

 IR-4

12.30

6.33

−0.175

1

 IR-8

12.49

6.44

−0.166

1

 IR-9

12.09

6.18

−0.219

1

 IR-11

12.90

6.63

−0.188

1

 IR-12

12.10

6.22

−0.178

1

Basic splash forms

 IRG-M4

8.01

4.17

−0.068

2

 IRG-M4 replicate

9.18

4.76

−0.104

1

 IR-10

8.47

4.42

−0.066

1

 IR-13

8.26

4.30

−0.075

1

 IR-14

8.56

4.45

−0.084

1

Composite splash forms

 IR-7

7.03

3.63

−0.094

1

  1. aEstimated measurement uncertainties are <0.3‰ and <0.008‰ for δ18O and Δ17O, respectively, based on the typical reproducibility (1 s.d.) of results for the standard reference material NBS 28 throughout the analytical sessions, except for samples denoted with superscript ‘b’
  2. bSamples analyzed with an improved extraction line (see text for details). Estimated measurement uncertainties are <0.15‰ and <0.007‰ for δ18O and Δ17O, respectively, based on the typical reproducibility (1 s.d.) of measurement results for San Carlos olivine