The Earth–Moon system during the late heavy bombardment period – Geochemical support for impacts dominated by comets-Reference-Cited by-同舟云学术

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The Earth–Moon system during the late heavy bombardment period – Geochemical support for impacts dominated by comets

Published:2009-12 Issue:2 Volume:204 Page:368-380
ISSN:0019-1035
Container-title:Icarus
language:en
Short-container-title:Icarus

Author:

Gråe Jørgensen Uffe,Appel Peter W.U.,Hatsukawa Yuichi,Frei Robert,Oshima Masumi,Toh Yosuke,Kimura Atsushi

Publisher

Elsevier BV

Subject

Space and Planetary Science,Astronomy and Astrophysics

Reference83 articles.

1. Continentally-derived solutes in shallow Archean seawater: Rare Earth element and Nd isotope evidence in iron formation from the 2.9Ga Pongola Supergroup, South Africa;Alexander;Geochim. Cosmochim. Acta,2008

2. Asteroid extinction hypothesis;Alvarez;Science,1981

3. Extraterrestrial iridium, sediment accumulation and the habitability of the early Earth’s surface;Anbar;J. Geophys. Res.,2001

4. Recognizable primary volcanic and sedimentary features in a low-strain domain of the highly deformed, oldest known (3.7–3.8Gyr) Greenstone Belt, Isua, West Greenland;Appel;Terra Nova,1998

5. Bockelée-Morvan, D., and 11 colleagues, 1998. Deuterated water in Comet C/1996 B2 (Hyakutake) and its implications for the origin of comets. Icarus 193, 147–162.

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