The age of SNC meteorites and the antiquity of the Martian surface
By A. Bouvier, J. Blichert‐Toft, J. Vervoort, F. Albarède. 2005
133 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Atmospheric Science
View Paper: https://www.semanticscholar.org/paper/deb9ae79ca0ee93e326366384143854ec118623b
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
- A. Withers
- M. Hirschmann
- T. O. S. University
- Research School of Earth Sciences
- D. Geology
- T. Yoshizaki
- William F. McDonough Department of Earth Science
- H. Dalton
In Atmospheric Science
Citations in the corpus
- Hydrogen isotope evidence for loss of water from Mars through time (2008, background): “This observation is inconsistent with the recent suggestion that acidic crustal fluids have reset the radiogenic isotope ‘clocks’ of most Martian meteorites [Bouvier et al., 2005].”
- Constraints on the depths and temperatures of basaltic magma generation on Earth and other terrestrial planets using new thermobarometers for mafic magmas (2009, background): “If, however, the young internal isochron ages of many Martian meteorites, such as Yamato 980459, are actually due to resetting by shock-induced melting or aqueous alteration (Bouvier et al., 2005), a late stage megaplumemight not be required.”
- The global martian volcanic evolutionary history (2009, background): “However, recently Bouvier et al. (2005, 2008) argued that the young Shergottite ages represent hydrothermal alteration and the crystallization age is 4.1 Ga.”
- The composition of Mars (2019, background): “otopic systematics of Martian meteorites. Martian meteorites have a wide ranges of (= 238U/204Pb) values and Pb isotopic heterogeneity (Nakamura et al., 1982; Misawa et al., 1997; Borg et al., 2005; Bouvier et al., 2005, 2008a, 2009; Chen and Wasserburg, 1986; Gaffney et al., 2007; Moriwaki et al., ”
- Ventilation of CO2 from a reduced mantle and consequences for the early Martian greenhouse (2008, background): “Evidence for ancient ~4 Ga ages for some SNC meteorites (Bouvier et al., 2005) likely results from terrestrial Pb contamination (Gaffney et al.”
- The Lu–Hf and Sm–Nd isotopic composition of CHUR: Constraints from unequilibrated chondrites and implications for the bulk composition of terrestrial planets (2008, background): “When initial Hf and Nd isotopic compositions of terrestrial (e.g., Vervoort et al., 1999, 2000; Blichert-Toft et al., 2005; and references therein), Martian (Nakamura et al.; 1982; Bouvier et al., 2005, 2008; Debaille et al., 2008a,b), lunar (Unruh et al., 1984; Unruh and Tatsumoto, 1984), and euc”