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Oxygen isotope composition of differentiated achondrites. Data for angrites and HEDs from Greenwood et al. (2005). Data for Martian meteorites from Franchi et al. (1999). EFL: eucrite fractionation line (Greenwood et al., 2005), AFL: angrite fractionation line (Greenwood et al., 2005), MFL: Martian fractionation line (Franchi et al., 1999), TFL: terrestrial fractionation line. M: average value of Martian meteorite analyses from Franchi et al. (1999). E: bulk terrestrial mantle (Mattey et al., 1994). Open squares: HEDs, open triangles: angrites, open circles: Martian meteorites. Δ17O is linearized using the format of Miller (2002): Δ17O = 1000 ln (1+ (δ17O/1000)) – λ1000 ln (1+ ( δ18O/1000)) where λ = 0.5247. |
δ18O | δ17O | Δ17O: given | Δ17O: Miller (2002) | Comment |
---|---|---|---|---|
6.6400 | 2.7700 | Not given | -0.71 |
Name | Class | δ18O | δ17O | Δ17O: calc | Δ δ18O | Δ δ17O | Δ Δ17O |
---|---|---|---|---|---|---|---|
Dhofar 732 | Achondrite-ung | 6.6400 | 2.7700 | -0.71 | 0 | 0 | 0 |
Ooldea 014 | Achondrite-prim-ung | 6.5670 | 2.7660 | -0.676 | -0.07 | -0 | 0.03 |
Northwest Africa 5517 | Achondrite-ung | 6.6180 | 2.5700 | -0.898 | -0.02 | -0.2 | -0.19 |
Northwest Africa 5517 | Achondrite-ung | 6.8070 | 2.6510 | -0.915 | 0.17 | -0.12 | -0.21 |
Northwest Africa 4024 | Winonaite | 6.6000 | 3.0100 | -0.449 | -0.04 | 0.24 | 0.26 |
Northwest Africa 10085 | K4 | 6.8730 | 2.6740 | -0.927 | 0.23 | -0.1 | -0.22 |
Errachidia 004 | Winonaite | 6.6550 | 3.0220 | -0.466 | 0.02 | 0.25 | 0.24 |
Northwest Africa 11558 | Achondrite-ung | 6.9900 | 2.7160 | -0.946 | 0.35 | -0.05 | -0.24 |
Northwest Africa 7531 | CR7 | 7.0480 | 2.7290 | -0.963 | 0.41 | -0.04 | -0.25 |
Northwest Africa 7680 | Achondrite-ung | 7.0400 | 2.6500 | -1.038 | 0.4 | -0.12 | -0.33 |
Northwest Africa 11729 | Eucrite-an | 6.3120 | 3.0620 | -0.247 | -0.33 | 0.29 | 0.46 |