A determination of the neon isotopic composition of the deep mantle: Earth and Planetary Science Let

By R. Yokochi, B. Marty. 2004

146 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Geophysics

View Paper: https://www.semanticscholar.org/paper/4b7fd022fc0a347b47df2e3abc9a2cb5f16732c5

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Astronomy and Astrophysics

1. Z. Leinhardt
2. S. Stewart
3. M. Gudel
4. J. Tucker
5. S. Mukhopadhyay
6. H. Lammer
7. K. Meech
8. M. Mottl

In Geophysics

1. Z. Leinhardt
2. S. Stewart
3. J. Tucker
4. S. Mukhopadhyay
5. M. Mace
6. L. Noack
7. M. Godolt
8. E. Pilat-Lohinger

Citations in the corpus

• The Origin of the Moon Within a Terrestrial Synestia (2018, background): “…deep terrestrial mantle sample a reservoir that is isotopically distinct from the upper mantle (Holland & Ballentine, 2006; Mukhopadhyay, 2012; Mundl et al., 2017; Parai et al., 2012; Pető et al., 2013; Rizo et al., 2016; Tucker & Mukhopadhyay, 2014; Tucker et al., 2012; Yokochi & Marty, 2004).”
• Water and astrobiology (2007, background): “0; Yokochi and Marty, 2004, 2005) is nearly as high as the Solar value of 13.8, and is significantly higher than that of (1) meteoritic Ne–”
• The origins and concentrations of water, carbon, nitrogen and noble gases on Earth (2014, methodology): “If the proto-Earth reached such a significant size in a few Ma when the nebular gas was still present, a massive solar-like atmosphere could have been captured (Sasaki, 1990; Yokochi and Marty, 2004).”
• Evidence for multiple magma ocean outgassing and atmospheric loss episodes from mantle noble gases (2013, methodology): “9) in primitive OIBs supports the presence of nebular He and Ne in the deep mantle (Mukhopadhyay, 2012; Yokochi and Marty, 2004).”
• Origin and evolution of the atmospheres of early Venus, Earth and Mars (2018, background): “…have been trapped from the protoplanetary disk, and left in solar composition in the interiors of early Venus and Earth (e.g. Mizuno et al. 1980; Sasaki and Nakazawa 1989; Porcelli and Pepin 2000; Dixon et al. 2000; Porcelli et al. 2001; Becker et al. 2003; Halliday 2004; Yokochi and Marty 2004).”