Some Mexican Meteorites’ Age: from the Origin of Solar System until Their Arrive at the Lab
Keywords:
meteorites, meteoriticist, Solar System, meteorites’ ageAbstract
Meteorites are rocks that originated in the early stages of the Solar System and represent either fragments of asteroids that did not become a full planet or remains of a differentiated planet. The importance of studying them is that they are one of the main evidences to determine the geochemical composition and history of formation and evolution of planets, particularly the inner or terrestrial planets. There are two main types of meteorites, stony and metallic; each representing a specific region of a planetary body. The story of a meteorite can be eventful because it can be transformed by several processes during its more than 4,500 million years. These processes can be accretion, weathering, collisions, partial melting, metamorphism, fall into Earth surface to end with their finding. Furthermore, the meteorites show that in other planets magmatic processes occurred with mechanisms similar to those in Earth. In this work we show how we can study the history of each meteorite using as example some Mexican meteorites. We will show that chemical elements and isotopes and their ratios are the clue to unravel this story.
References
AMELIN Y. et al., “U–Pb chronology of the Solar System's oldest solids with variable 238U/235U”, Earth and Planetary Science Letters, 2010, vol. 300, Núm. 3-4, pp. 343–350.
AMELIN, Y.; Alexander N. Krot; Ian D. Hutcheon y Alexander A. Ulyanov, “Lead isotopic ages of chondrules and Calcium-Aluminium-Rich inclusions”, Science, 2002, vol. 297, Núm. 5587, pp. 1678-1683.
BERNATOWICZ, T.J.; F.A. Podosek; T.D. Swindle y M. Honda, “I-Xe systematics in LL chondrites”, Geochimica et Cosmochimica Acta, 1998, vol. 52, Núm. 5, pp. 1113-1121.
BISCHOFF, A., “Meteorite classification and the definition of new chondrite classes as a result of successful meteorite search in hot and cold deserts”, Planetary and Space Science, 2001, vol.49, Núm. 8, pp. 769-776.
BOUVIER, A.; J. Blichert-Toft; F. Moynier; J. Vervoort y F. Albarede, “Pb-Pb dating constraints on the accretion and cooling history of chondrites”, Geochimica et Cosmochimica Acta, 2007, vol. 71, Núm. 6, pp. 1583-1604.
FASSETT, C. y D. Minton, “Impact bombardment of the terrestrial planets and the early history of the Solar System”, Nature Geoscience, 2013, vol. 6, pp. 520-524.
GANGULY, J.; M. Tirone; S. Chakraborty y K. Domanik, “H-chondrite parent asteroid: A multistage cooling, fragmentation and re-accretion history constrained by thermometric studies, diffusion kinetic modeling and geochronological data”, Geochimica et Cosmochimica Acta, 2013, vol. 105, pp.206–220.
GRAF, T. y K. Marti, “Collisional records in LL-chondrites”, Meteoritics, 1994, vol. 29, Núm. 5, pp. 643-648.
—————————, “Collisional history of H chondrites”, Journal of Geophysical Research, 1995, vol. 100, Núm. E10, pp. 21, 247-21,263.
HERNÁNDEZ-BERNAL, M. S. y J.S. Solé-Viñas, “Single Chondrule K-Ar ages of Mexican Ordinary Meteorites as tracers of extended impact events”, Revista Mexicana de Ciencias Geológicas, 2010, vol. 27, Núm. 1, pp. 123-133.
JESSBERGER, E. K.; B. Dominik; T. Staudacher y G. F. Herzog, 1980, “40Ar-39Ar ages of Allende”, Icarus, 1980, vol. 42, Núm. 3, pp. 380-405.
LIBOUREL, J. y C. M. Corrigan, “Asteroids: New Challenges, New Targets”, Elements, 2014, vol. 10, Núm. 1, pp. 11–17.
LINDSAY, F. N. et. al., “40Ar/39Ar Dating of Tuxtuac (LL5)”, 76th Annual Meteoritical Society Meeting, id.5324, 2013.
PRAVDIVTSEVA, O.; A. Meshik; M. Petaev y C. M. Hohenberg, “I-Xe Ages and the Thermal History of the Toluca IAB Meteorite”, Lunar and Planetary Science XXXIX, 2008, Núm. 1391, p. 2504.
ROTH, A. S. G. et al., “Cosmogenic helium and neon in individual chondrules from Allende and Murchison: Implications for the precompaction exposure history of chondrules”, Meteoritics and Planetary Science, 2011, vol. 46, Núm. 7, pp. 989–1006.
ROZITIS, B.; E. MacLennan y J. Emery, “Cohesive forces prevent the rotational breakup of rubble-pile asteroid (29075) 1950DA”, Nature, 2014, vol. 512, Núm. 7513, pp. 174-175.
SCHMITZ, B. et al., “A fossil winonaite-like meteorite in Ordovician limestone: A piece of the impactor that broke up the L-chondrite parent body?”, Earth and Planetary Science Letters, 2014, vol. 400, pp.145–152.
Published
Issue
Section
License
Copyright (c) 2017 Revista Digital Universitaria

This work is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License.

Revista Digital Universitaria es editada por la Universidad Nacional Autónoma de México se distribuye bajo una Licencia Creative Commons Atribución-NoComercial 4.0 Internacional. Basada en una obra en http://revista.unam.mx/.