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Table 2 Average mineral compositions of olivine (Ol) and plagioclase (Pl) grains in lunar meteorite Northwest Africa (NWA) 2977 PTS 01-1 (this work), in comparison with those of Zhang et al. (2011)

From: Mineralogy and petrology of lunar meteorite Northwest Africa 2977 consisting of olivine cumulate gabbro including inverted pigeonite

 

This work

Zhang et al. (2011)

Oxide (wt%) No.

Ol 16

Pl 7

Ol

Pl

Pl

SiO2

37.72(0.33)

46.16(1.35)

38.1

45.0

49.4

TiO2

b.d.

b.d.

0.08

 

0.11

Al2O3

b.d.

34.07(0.80)

b.d.

35.2

32.3

Cr2O3

0.05(0.02)

b.d.

0.03

  

FeO

26.31(0.40)

0.08(0.02)

27.6

0.24

0.45

MnO

0.33(0.06)

0.04(0.02)

0.24

  

MgO

34.02(0.26)

0.18(0.07)

33.5

0.08

0.17

CaO

0.11(0.03)

18.04(0.60)

0.15

19.1

15.7

Na2O

b.d.

0.93(0.33)

b.d.

0.67

1.34

K2O

b.d.

0.17(0.05)

b.d.

0.09

1.24

P2O5

b.d.

0.15(0.01)

   

Total

98.54

99.82

99.6

100.4

100.7

Mg#

70

 

68

  

An

 

90.6

 

93.5

80.1

Ab

 

8.4

 

6.0

12.3

Or

 

0.5

 

0.5

7.5

  1. Our values in parentheses are the standard deviations (1σ) of the individual mineral compositions and reflect the compositional variation of each mineral in polished thin section (PTS) 01-1 (this work)
  2. No. number of analyses, b.d. below the detection limit