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Sample 15668

Fine-grained, Olivine-normative Basalt 15.1 grams

Section titled “Fine-grained, Olivine-normative Basalt 15.1 grams”

Figure 1: Photo of 15668. Sample is 3 cm across. NASA S71-49725.

Lunar sample 15668 was collected by rake about 20 meters from Hadley Rille (Swann et al. 1971). It is a vesicular, subophitic basalt with a very fine grain size (quite unlike other Apollo 15 basalts). Olivine phenocrysts are seen in hand specimen. It has been dated at 3.13 ± 0.06 b.y., which is younger than most Apollo 15 basalts.

Ryder (1985) gives the only description. The “mode” attributed to Rhodes and hubbard (1973) is probably a calculated “norm” based on their analysis, as olivine phenocrysts are “conspicuous” in hand specimen. The texture is subophitic and the average grain size of this basalt is very fine (0.1 mm.). A few small olivine phenocrysts are seen in thin section (figure 2). Euhedral chromite is present in olivine; ulvospinel and ilmenite in the groundmass. Interstial glass is present and shows immiscibility.

Ryder and Schuraytz (2001) repeated the analysis of Ryder and Steele (1988). Helmke et al. (1972) found higher trace elements than Neal (2001), Fruchter et al. (1973), and Ryder (figure 4). It is possible that this rocklet is something special, but probably not.

Rhodes and
Hubbard 1973
Olivine0.8
Pyroxene59.6
Plagioclase31.2
Opaques4.9
Mesostasis3

Husain (1974) reported an age of 3.13 ± 0.06 b.y by Ar/Ar plateau, but if you take the highest temperature release steps only, you get an age similar to the other Apollo 15 basalts (figure 5).

Figure 2: Photomicrographs of 15668,13 by C Meyer @ 50x.

Figure 3: Chemical composition of 15668 compared with other Apollo samples.

Pearce et al. (1973) reported magnetic properties.

There are only two thin sections of 15668.

Figure 4: Normalized rare-earth-element diagram for 15668 (data by Neal 2001). Data for 15601 is for comparison.

Figure 5: Ar/Ar plateau diagram for 15668 (from Husain 1974).

Table 1. Chemical composition of 15668.

reference Ryder2001
2.5 g
Rhodes73Chappell73 Fruchter73Ryder88Neal2001Helmke72
weight
SiO2 %
TiO2
Al2O3
FeO
MnO
MgO
44.6
2.43
8.81
22.32
0.28
10.13
(b)
(b)
(b)
(b) 22.4
(b)
(b)
45.48
2.56
9.09
(a) 22.22
0.31
9.19
(b) 45.01
(b) 2.53
(b) 8.73
(b) 22.58
(b) 0.31
(b) 9.96
(b)
(b)
(b)
(b) 2.74
(b) 8.2
(b) 22.3
46.7
(a) 2.37
(a) 9.1
(a) 21.9
0.38
8.9
(c )
(c )
(c )
(c )
(c )
(c )
CaO
Na2O
9.71
0.234
(b)
(b) 0.248
10.23
(a) 0.26
(b) 10.16
(b) 0.28
(b)(b) 0.2669.9
(a) 0.25
(c )
(c )
K2O
P2O5
S %
sum
0.043
0.064
(b)
(b)
0.05
0.08
0.08
(b) 0.04
(b) 0.07
(b) 0.05
(b)
(b)
(b)
0.12(c )
Sc ppm
V
43.5(a)44(a) 44.6(a) 44.7
197
(d)(d) 39.5(a)
Cr
Co
Ni
Cu
Zn
Ga
Ge ppb
As
Se
Rb
Sr
Y
Zr
Nb
Mo
Ru
Rh
4426
49
9
(b) 4310
53.1
(b) 80
(b)
(a)
(a)
(a)
3700(b) 4250
55
(a) 3462
(a) 46.8
(a) 3397
(a) 55.9
57.2
13.8
23.5
4.19
(d)
(d)
(d)
(d) 4200
(d) 54
(d) 3.7
(a)
(a)
(a)
6
93
24
86
11
(b)
(b) 112
(b)
(b)
(b)
(a)0.92
99
28
87
7.43
0.09
(d)
(d)
(d)
(d)
(d)
(d)
Pd ppb
Ag ppb
Cd ppb
In ppb
Sn ppb
Sb ppb
Te ppb
Cs ppm
260
0.03
(d)
(d)
Ba
La
Ce
39
4.82
13.7
(a)
(a)
(a)
4.5(a) 4.95
11.7
53.2
(a) 5.19
(a) 14.5
(d)(d) 6.68
(d) 17.6
(a)
(a)
Pr
Nd
Sm
12
3.45
(a)
(a)
3.1(a) 3.52.23
10.4
(a) 3.57
(d)(d) 13.3
(d) 4.45
(a)
(a)
Eu
Gd
0.88(a)0.92(a) 0.907(a) 0.93
4.93
(d) 0.99
(d) 5.7
(a)
(a)
Tb
Dy
Ho
Er
0.77(a)0.85(a) 0.83
5.2
1.01
2.9
(d) 0.95
(d) 6.2
(d) 1.14
(d) 2.08
(a)
(a)
(a)
(a)
Tm
Yb
Lu
Hf
2.18
0.29
2.69
(a)
(a)
(a)
1.6
0.29
2.3
(a) 2.26
(a) 0.319
(a) 2.63
0.39
(a) 2.47
(a) 0.32
(a) 2.77
(d)
(d)
(d) 2.9
(d) 0.394
(a)
(a)
Ta
W ppb
Re ppb
Os ppb
Ir ppb
Pt ppb
0.37(a)0.37(a)0.43
40
(d)
(d)
Au ppb
Th ppm
U ppm
0.38(a)0.42(a) 0.51
0.11
(d)
(d)
technique: (a) INAA, (b) XRF, (c ) fused bead, elec. Probe, (d) ICP-MS

Lunar Sample Compendium C Meyer 2010

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