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Oxygen isotope composition of lunar rocks and meteorites. Data for lunar samples from Wiechert et al. (2001); Spicuzza et al. (2007); Hallis et al. (2010). Data for lunar meteorite samples compiled from the Meteoritical Bulletin. Angrite data from Greenwood et al. (2005), Irving et al. (2005, 2006). Δ17O is linearized using the format of Miller (2002): Δ17O = 1000 ln (1+ (δ17O/1000)) – λ1000 ln (1+ (δ18O/1000)) where λ = 0.5247. TFL = Terrestrial Fractionation Line. AFL = angrite fractionation (Greenwood et al., 2005). |
δ18O | δ17O | Δ17O: given | Δ17O: Miller (2002) | Comment |
---|---|---|---|---|
6.6760 | 3.4700 | -0.0020 | -0.031 | |
7.0050 | 3.6380 | -0.0050 | -0.035 |
Name | Class | δ18O | δ17O | Δ17O: calc | Δ δ18O | Δ δ17O | Δ Δ17O |
---|---|---|---|---|---|---|---|
Kaidun | CR2 | 6.8400 | 3.5700 | -0.016 | -0 | 0.02 | 0.02 |
Northwest Africa 6687 | Lunar (feldsp. breccia) | 6.8400 | 3.5800 | -0.007 | -0 | 0.03 | 0.03 |
Kalahari 009 | Lunar (basalt) | 6.8700 | 3.4500 | -0.152 | 0.03 | -0.1 | -0.12 |
Grapevine Mesa | CBa | 6.9490 | 3.4670 | -0.176 | 0.11 | -0.09 | -0.14 |
Arabian Peninsula 007 | Lunar (frag. breccia) | 6.6460 | 3.4840 | -0.001 | -0.19 | -0.07 | 0.03 |
Dar al Gani 1031 | EL4 | 6.6200 | 3.4700 | -0.001 | -0.22 | -0.08 | 0.03 |
Almahata Sitta | Ureilite-an | 6.6100 | 3.4100 | -0.056 | -0.23 | -0.14 | -0.02 |
Jiddat al Harasis 846 | OC3 | 6.7240 | 3.8820 | 0.355 | -0.12 | 0.33 | 0.39 |
Northwest Africa 10989 | Lunar | 6.5100 | 3.4200 | 0.006 | -0.33 | -0.13 | 0.04 |
Kalahari 008 | Lunar (anorth) | 6.5200 | 3.3200 | -0.099 | -0.32 | -0.23 | -0.07 |
Northwest Africa 13411 | OC5-an | 6.5260 | 3.8360 | 0.412 | -0.31 | 0.28 | 0.45 |
Northwest Africa 13411 | OC5-an | 6.4330 | 3.6660 | 0.292 | -0.41 | 0.11 | 0.32 |
Almahata Sitta | Ureilite-an | 6.4200 | 3.3600 | -0.007 | -0.42 | -0.19 | 0.03 |
Northwest Africa 12821 | EL3 | 6.4020 | 3.3670 | 0.01 | -0.44 | -0.19 | 0.04 |
Northwest Africa 7135 | Chondrite-ung | 6.4500 | 3.8590 | 0.475 | -0.39 | 0.31 | 0.51 |