Gounelle, M., Meibom, A., Hennebelle, P.
The radioactive isotope $^{60}$Fe ($T_{1/2} = 1.5 $ Myr) was present in the early solar system. It is unlikely that it was injected directly into the nascent solar system by a single, nearby...
Sandford, S. A., Aléon, J., Alexander, C. M. O’D., Araki, T., Bajt, S., Baratta, G. A., ...
This presenation will provide an overview of the efforts and results produced by the Organics Preliminary Examination Team during their studies of the samples returned from comet Wild 2 by the...
Noble gas signature of the Late Heavy Bombardment in the Earth's atmosphere (2007)
The Lunar cratering record is consistent with the occurrence of a late heavy bombardment (LHB), which marked the end of terrestrial planet accretion 3.8 billion years ago. However, clear evidence of...
Noble gas signature of the late heavy bombardment in the Earth's atmosphere (2007)
The Lunar cratering record is consistent with the occurrence of a late heavy bombardment (LHB), which marked the end of terrestrial planet accretion 3.8 billion years ago. However, clear evidence of...
Noble gas signature of the Late Heavy Bombardment in the Earth's atmosphere (2007)
The Lunar cratering record is consistent with the occurrence of a late heavy bombardment (LHB), which marked the end of terrestrial planet accretion 3.8 billion years ago. However, clear evidence of...
Noble gas signature of the late heavy bombardment in the Earth's atmosphere (2007)
The Lunar cratering record is consistent with the occurrence of a late heavy bombardment (LHB), which marked the end of terrestrial planet accretion 3.8 billion years ago. However, clear evidence of...
Noble gas signature of the Late Heavy Bombardment in the Earth's atmosphere (2007)
The Lunar cratering record is consistent with the occurrence of a late heavy bombardment (LHB), which marked the end of terrestrial planet accretion 3.8 billion years ago. However, clear evidence of...
Noble gas signature of the late heavy bombardment in the Earth's atmosphere (2007)
The Lunar cratering record is consistent with the occurrence of a late heavy bombardment (LHB), which marked the end of terrestrial planet accretion 3.8 billion years ago. However, clear evidence of...
Frei, R., Gervilla, F., Meibom, A., Proenzad, J. A., Garridob, C. J.
11 pages, 3 figures, 1 table.
Research article - Comet 81P/Wild 2 under a microscope (2006)
Brownlee, D., Tsou, P., Aleon, J., Alexander, C. M. O., Araki, T., Bajt, S., ...
Mineralogy and Petrology of Comet Wild 2 Nucleus Samples. (2006)
Zolensky, M.E., Zega, T.J., Yano, H., Wirick, S., Westphal, A.J., Weisberg, M.K., ...
Isotopic compositions of cometary matter returned by Stardust (2006)
McKeegan, K. D., Aleon, J., Bradley, J., Brownlee, D., Busemann, H., Butterworth, A., ...
Comet 81P/Wild 2 under a microscope (2006)
Brownlee, D., Tsou, P., Aleon, J., Alexander, C. M. O., Araki, T., Bajt, S., ...
Research article - Comet 81P/Wild 2 under a microscope (2006)
BROWNLEE, D, TSOU, P, ALEON, J, ALEXANDER, C, ARAKI, T, BAJT, S, ...
Gervilla, F., Proenza, J. A., Frei, R., González-Jiménez, J. M., Garrido, C. J., Melgarejo, J. C., ...
The Mayarí-Baracoa ophiolitic belt in eastern Cuba hosts abundant chromite deposits of historical economic importance. Among these deposits, the chemistry of chromite ore is very variable, ranging...
Gervilla, F., Proenza, J. A., Frei, R., González-Jiménez, J. M., Garrido, C. J., Melgarejo, J. C., ...
The Mayarí-Baracoa ophiolitic belt in eastern Cuba hosts abundant chromite deposits of historical economic importance. Among these deposits, the chemistry of chromite ore is very variable, ranging...
16O-poor refractory inclusions in CB chondrites. (2001)
Krot, A. N., McKeegan, K. D., Russell, S. S., Meibom, A., Weisberg, M. K., Zipfel, J., ...
H2-rich fluids from serpentinization: Geochemical and biotic implications
Sleep, N. H., Meibom, A., Fridriksson, Th., Coleman, R. G., Bird, D. K.
Metamorphic hydration and oxidation of ultramafic rocks produces serpentinites, composed of serpentine group minerals and varying amounts of brucite, magnetite, and/or FeNi alloys. These minerals...
H2-rich fluids from serpentinization: Geochemical and biotic implications
Sleep, N. H., Meibom, A., Fridriksson, Th., Coleman, R. G., Bird, D. K.
Metamorphic hydration and oxidation of ultramafic rocks produces serpentinites, composed of serpentine group minerals and varying amounts of brucite, magnetite, and/or FeNi alloys. These minerals...