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PNAS：W同位素制約地球早期地幔對流模式( 二 )


PNAS：W同位素制約地球早期地幔對流模式
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主要參考文獻(xiàn)
Kleine T, Mezger K, Münker C, et al. Hf-W isotope systematics of chondrites, eucrites, and martian meteorites: Chronology of core formation andearly mantle differentiation in Vesta and Mars[J]. Geochimica et Cosmochimica Acta, 2004, 68(13): 2935–2946.
Mei Q F, Yang J H, Wang Y F, et al. Tungsten isotopic constraints on homogenization of the Archean silicate Earth: Implications for the transition of tectonic regimes[J]. Geochimica et Cosmochimica Acta, 2020, 278: 51–64.（見亮點(diǎn)報道《太古宙硅酸鹽地球均一化的W同位素證據(jù)及對地球構(gòu)造體制轉(zhuǎn)換的制約》）
Rizo H, Walker R J, Carlson R W, et al. Early Earth differentiationinvestigated through 142Nd, 182W, and highly siderophile element abundances in samples from Isua, Greenland[J]. Geochimica et Cosmochimica Acta, 2016, 175: 319–336.
Touboul M, Puchtel I S and Walker R J. 182W evidence for long-term preservation of early mantle differentiation products[J]. Science, 2012, 335: 1065–1069.
Tusch J, Münker C, Hasenstab E, et al. Convective isolation of Hadean mantle reservoirs through Archean time[J]. Proceedings of the National Academy of Sciences, 2021, 118(2): e2012626118.
Willbold M, Elliott T and Moorbath S. The tungsten isotopic composition of the Earth’s mantle before the terminal bombardment[J]. Nature, 2011, 477: 191–195.
Willbold M, Mojzsis S J, Chen H W, et al. Tungsten isotope composition of the Acasta Gneiss Complex[J]. Earth and Planetary Science Letters, 2015, 419: 168–177.


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