Table 1 Copper isotopic compositions of the measured samples and geological reference materials

From: Martian differentiation history inferred from copper isotopes

Group

Subtype

Name

δ65Cu (‰)

2 SD (‰)g

Nh

Shergottite

Basaltic

NWA 12269

−0.01

0.05

3

NWA 12594

0.02

0.05

3

NWA 12594 repeat

0.01

0.05

3

NWA 2975

0.12

0.05

3

NWA 8657

−0.07

0.05

3

Zagami

−1.19

0.06

3

Zagami chip 2

−1.00

0.06

3

NWA 12564

0.01

0.05

3

NWA 12564 chip 2

0.04

0.05

3

NWA 12564 chip 2 repeat

0.05

0.05

3

NWA 13327

−0.07

0.05

3

Swayyah 002

−0.08

0.05

3

Swayyah 002 repeat

−0.05

0.05

3

Gabbroic

NWA 6963

0.63

0.06

3

NWA 6963 chip 2

0.49

0.06

3

Olivine-phyric

NWA 1068

−0.12

0.05

3

Poikilitic

NWA 7397

−0.29

0.06

3

NWA 13276

0.00

0.05

3

NWA 13276 chip 2a

0.02

0.06

3

NWA 13367

−0.03

0.05

3

NWA 13367 chip 2

−0.04

0.05

3

Nakhlite

Augite-olivine-rich

Qued Mya 005

−0.06

0.05

3

Qued Mya 005 chip 2

−0.15

0.06

3

NWA 10645

−0.44

0.06

3

Reference material

Basalt

BHVO-2

0.06

0.05

3

0.03

0.06

3

0.07b

0.06

0.08c

0.05

0.10d

0.05

0.12e

0.02e

BIR-1a

0.02

0.05

3

0.02f

0.04

0.02e

0.06e

Peridotite

JP-1

0.06

0.05

3

0.03f

0.05

  1. aWeathered exterior of NWA 13276 chip 1, excluded from the average.
  2. bDay et al.13.
  3. cNi et al.12.
  4. dHuang et al.15.
  5. eMoynier et al.96, uncertainty is expressed as 2 SE (twice the standard error).
  6. fLiu et al.5.
  7. gUncertainties for measured samples are reported as 2 SD (twice the standard deviation of standard solution analyses during an analytical session).
  8. hNumber of measurements per sample solution.