Table 1
Ablated meteorites analyzed in this work.
Name | Type | Rec. | Fe | Si | Mg | Ca | Al | Cr | Mn | Na | K | Ni | C | T [K] | Bulk ref. |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Košice | H5 | fall | 28.85 | 16.51 | 13.80 | 1.14 | 1.07 | 0.350 | 0.230 | 0.600 | 0.090 | 1.00 | 0.05 | 4660 | [1] |
Pultusk | H5 | fall | 27.18 | 17.04 | 14.32 | 1.30 | 1.34 | 0.253 | 0.194 | 0.616 | 0.075 | 1.61 | − | 3770 | [2], [3] |
Buzzard Coulee | H4 | fall | − | − | − | − | − | − | − | − | − | − | − | 4020 | N/A |
NWA 869 | L3–6 | find | 19.47 | 18.25 | 14.54 | 1.44 | 1.09 | 0.280 | 0.260 | − | − | 1.37 | − | 4830 | [4], [3] |
Mocs | L5–6 | fall | 23.16 | 17.95 | 15.50 | 1.24 | 1.16 | 0.310 | 0.290 | 0.512 | 0.058 | 1.32 | − | 4680 | [5] |
Knyahinya | L/LL5 | fall | 20.80 | 19.17 | 15.00 | 1.33 | 1.28 | 0.406 | 0.270 | 0.746 | 0.090 | 1.16 | 0.21 | 4340 | [6], [7] |
Ragland | LL3.4 | find | 20.00 | 18.50 | 13.30 | 1.32 | 1.24 | 0.411 | 0.219 | 0.287 | 0.047 | 0.87 | 0.61 | 4240 | [8], [7] |
Chelyabinsk | LL5 | fall | 19.20 | 18.30 | 15.50 | 1.35 | 1.18 | 0.400 | 0.270 | 0.760 | 0.100 | 1.11 | − | 4330 | [9], [10] |
Kheneg Ljouâd | LL5/6 | fall | − | − | − | − | − | − | − | − | − | − | − | 3820 | N/A |
Eagle | EL6 | fall | 23.19 | 20.19 | 14.43 | 0.54 | 1.80 | 0.220 | 0.220 | 0.616 | 0.075 | 1.38 | 0.32 | 4530 | [7] |
Allende | CV3 | fall | 23.16 | 15.94 | 15.47 | 1.84 | 1.82 | 0.404 | 0.150 | 0.349 | 0.038 | 1.40 | 0.29 | 4350 | [11] |
Lancé | CO3.5 | fall | 25.33 | 15.90 | 14.43 | 1.80 | 1.44 | 0.328 | 0.144 | 0.446 | 0.045 | 1.40 | 0.40 | 4610 | [12], [7] |
Murchison | CM2 | fall | 22.13 | 13.58 | 12.02 | 1.35 | 1.14 | 0.328 | 0.176 | 0.178 | 0.033 | 1.13 | 1.85 | 3860 | [7], [13] |
Sariçiçek | Howardite | fall | 14.40 | 23.75 | 9.94 | 5.34 | 3.77 | 0.756 | 0.460 | 0.255 | 0.025 | 0.05 | − | 4050 | [14] |
Stannern | Eucrite | fall | 13.93 | 23.23 | 4.21 | 7.61 | 6.49 | 0.220 | 0.400 | 0.430 | 0.061 | 0.0002 | − | 4250 | [15], [16] |
Bilanga | Diogenite | fall | 12.20 | 24.80 | 18.00 | 0.50 | 0.44 | 0.601 | 0.348 | 0.009 | 0.011 | 0.002 | − | 3680 | [12], [17] |
Tissint | Shergottite | fall | 15.34 | 21.60 | 10.31 | 4.65 | 2.57 | 0.417 | 0.400 | 0.534 | 0.017 | 0.04 | − | 4830 | [18], [19] |
NWA 11303 | Lunar | find | 2.76 | 20.68 | 2.61 | 12.01 | 15.66 | 0.050 | 0.050 | 0.250 | 0.020 | − | − | 4610 | [20](a) |
Norton County | Aubrite | fall | 2.37 | 24.20 | 25.94 | 0.85 | 0.15 | 0.068 | 0.120 | 0.163 | 0.010 | 0.06 | − | 4000 | [21] |
Dhofar 1575 | Ureilite | find | 14.76 | 18.47 | 21.25 | 0.77 | 0.28 | 0.522 | 0.310 | 0.063 | 0.025 | 0.13 | 2.80 | 3790 | [22](b) |
Mincy | Mesosiderite | find | − | 22.19 | 11.02 | 3.78 | 3.54 | 0.523 | 0.410 | 0.163 | 0.007 | 0.47 | − | 4690 | [23] |
Mount Joy | Iron | find | 92.72 | 1.09 | − | − | − | 0.005 | − | − | − | 5.68 | − | 3900 | [24], [25] |
Notes. The tested meteorites are described by their name, classification, recovery type, the bulk composition of the main species in wt%, and the estimated plasma temperature. The final column includes the source of the reported bulk chemical composition values. Bulk composition references: [1] Ozdín et al. (2015), [2] Dyakonova & Kharitonova (1961), [3] Phelan et al. (2022), [4] Metzler et al. (2011), [5] Miura et al. (1995), [6] Kallemeyn et al. (1989), [7] Jarosewich (1990), [8] Recca et al. (1986), [9] Galimov et al. (2013), [10] Kirillov et al. (2021), [11] Jarosewich et al. (1987), [12] Kusuno et al. (2013), [13] Braukmüller et al. (2018), [14] Unsalan et al. (2019), [15] McCarthy et al. (1973), [16] Kitts & Lodders (1998), [17] Mittlefehldt et al. (2012), [18] Herd et al. (2013), [19] Liu et al. (2016), [20] Korotev & Irving (2021), [21] Easton (1985), [22] Vdovykin (1970), [23] Simpson & Ahrens (1977), [24] Wasson (1969), [25] Wasson et al. (2007). Meteorites for which no chemical composition reference was found are denoted as N/A. (a)Mean composition from 24 typical feldspathic lunar meteorites in [20]; (b)Mean composition from six ureilites in [22].
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