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Sample 75061

Figure 1: Map of Apollo 17 showing location of soil samples and coarse-fines (Meyer 1973). S73-24071

Figure 2: Map of station 5, Apollo 17.

75060 was collected from the top surface of a flat boulder of basalt on the rim of Camelot Crater. It is made up of comminuted pieces of that boulder mixed with some soil that was undoubtedly kicked up by meteorite impacts in the adjacent soil. 75075 is a large piece of the boulder and 75080 is a sample of nearby soil (also very basaltic).

The maturity of 75061 is $I_s/FeO = 33$ and the average grain size is 112 microns (Morris 1978, Graf 1993). Heiken and McKay (1974) reported on 24% agglutinate. Meyer (1973) found that most all of the 4 – 10 mm coarse fines were mare basalt.

The FeO content of 75061 is very high (figure 3), and the composition is similar to the basaltic boulder (table).

Muller (1974) determined 42 ppm nitrogen in 75061. Petrowski et al. (1974) determined 94 ppm carbon, 49 ppm nitrogen and 43 ppm hydrogen

Figure 3: Composition of 75061 compared with other Apollo soils.

Figure 5: Carbon content and maturity index for 75061.

Keith et al. (1974) determined the cosmic-ray-induced activity of 22Na = 187 dpm/kg, 26Al = 180 dpm/kg, 46Sc = 86 dpm/kg, 48V = 47 dpm/kg, 54Mn = 200 dpm/ kg and 56Co = 490 dpm/kg. Rancitelli et al. (1974) determined the cosmic-ray-induced activity of 22Na = 171 dpm/kg, 26Al = 174 dpm/kg, 46Sc = 112 dpm/kg,

Section titled “Modal content of soil 75061 (90-150 micron).”

From Heiken and McKay 1974.

75061
Agglutinates24 %
Basalt26.6
Breccia4.9
Anorthosite
Norite
Gabbro
Plagioclase4.6
Pyroxene29.6
Olivine0.3
Ilmenite5.3
Orange glass1
Glass other3.2

Figure 4: Normalized rare-earth-element diagram for 75061 compared with highland soil 72221.

48V = 26 dpm/kg, 54Mn = 286 dpm/kg, 7 Be = 350 dpm/ kg and 56Co = 548 dpm/kg.

average grain size = 112 microns

Figure 6: Grain size distribution of 75060 (Graf 1993, data from McKay).

Table 1. Chemical composition of 75061

reference LSPET73
weight
39.32
10.31
10.42
18.19
0.25
9.53
10.72
0.33
0.08
0.06
0.13
Rhodes74
(a)
(a)
(a)
(a)
(a)
(a)
(a)
(a)
Wiesman76 Korotev92
Rhodes74
Rose74Keith74 Rancitelli74 Brunfelt74unpublished
SiO2 %
TiO2
Al2O3
FeO
MnO
MgO
CaO
Na2O
K2O
P2O5
S %
sum
(a) 11(b)1817.939.7
10.46
10.6
(c ) 17.86
0.24
9.65
(d)
(d)
(d)
(d)
(d)
(d)
9.5
10.5
16.8
0.24
7.8
(c )
(c )
(c )
(c )
(c )
(a) 0.35
(a) 0.075
(b)0.3440.3610.72
(c ) 0.37
0.08
(d)
(d)
(d) 0.0790.0728.96
0.39
(e) 0.084
(c )
(c )
(c )
Sc ppm
V
7570(c ) 78
95
(d)
(d)
65
137
(c )
(c )
Cr
Co
3284(a) 3090(b) 3480
26.3
27.83280 (c ) 3284
(c ) 36
(d)
(d)
2840
25
(c )
(c )
Ni
Cu
115(a)100100(c ) 154
27
(d)
(d)
6.9(c )
Zn
Ga
Ge ppb
As
25(a)12
4.3
(d)
(d)
30
4.1
(c )
(c )
Se
Rb
Sr
1.6
166
(a) 1.11
(a) 1.66
(b)(b) 1302101
(c ) 157
(d)
(d)
1.3
173
(c )
(c )
Y
Zr
83
237
(a)
(a)
25033091
(c ) 340
(d)
(d)
Nb
Mo
Ru
Rh
21(a)20(d)
Pd ppb
Ag ppb
Cd ppb
In ppb
Sn ppb
Sb ppb
Te ppb
Cs ppm
0.075(c )
Ba
La
Ce
89.5
7.07
23.6
(b) 80
(b) 6.4
(b) 21
105
7.34
21.3
(c )
(c )
(c ) 135(d)76
5.7
(c )
(c )
Pr
Nd
23.1(b) 2020(c )
Sm
Eu
9.09
1.77
(b) 8.24
(b) 1.64
8.62
1.74
(c )
(c )
8.44
1.33
(c )
(c )
Gd
Tb
13.4(b)2.112.18(c )2.2(c )
Dy
Ho
15.5(b)12.6(c )
Er
Tm
9.02(b)
Yb
Lu
Hf
Ta
W ppb
Re ppb
8.36(b) 7.94
1.12
7.37
1.4
8.21
1.12
7.93
1.4
(c )
(c )
(c )
(c ) 9.6(d)9.8
1.08
6.8
1.32
120
(c )
(c )
(c )
(c )
(c )
Os ppb
Ir ppb
< 55(c )
Pt ppb
Au ppb
Th ppm
< 6
1.1
< 7
0.5
(c )
(c )
0.910.87(e) 0.61(c )
U ppm
technique: (a) XRF, (b) IDMS, (c ) INAA, (d) “microchemical”, (e) radiation count.
0.21(b) 0.230.3(c )0.2480.22(e) 0.22(c )

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