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NARROW
GeoRef Subject
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elements, isotopes
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carbon (1)
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hydrogen
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D/H (1)
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isotope ratios (1)
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isotopes
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stable isotopes
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D/H (1)
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oxygen (1)
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meteorites
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meteorites
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stony meteorites
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chondrites
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carbonaceous chondrites
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CI chondrites
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Orgueil Meteorite (1)
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Primary terms
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carbon (1)
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hydrogen
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D/H (1)
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isotopes
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stable isotopes
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D/H (1)
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meteorites
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stony meteorites
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chondrites
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carbonaceous chondrites
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CI chondrites
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Orgueil Meteorite (1)
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oxygen (1)
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Comets: Where We Are, How We Got Here, and Where We Want To Go Next
The Rosetta Mission and the Chemistry of Organic Species in Comet 67P/Churyumov–Gerasimenko
Abstract The first meteorites were acquired by the Natural History Museum (NHM) in 1803. At this time when meteorites had just begun to be generally accepted as extraterrestrial by the scientific community. Over the last 200 years the collection has grown to be one of the largest and most diverse in the world. The collection is made up of approximately 1900 meteorites, including examples of all of the main types, from about 90 different countries. It is the largest collection of meteorite falls (meteorites observed to have fallen through the atmosphere, in contrast to those found later) in the world. The current strength of the collection and associated research can be attributed to the passion for meteorites shown by members of the Department of Mineralogy over the years, especially keepers Nevil Story-Maskelyne, Lazarus Fletcher and George Prior.
Abstract It has been almost 25 years since the widespread acceptance of the presence of meteorites from Mars in the world’s collections. The martian meteorites differ from meteorites from the asteroid belt in that they have crystallization ages younger than 4.568 billion years; evidence for a martian origin rests on the presence of trapped martian atmospheric gases within the specimens. The first three martian meteorites, Shergotty, Nakhla and Chassigny, gave their names to the groups into which the specimens were all placed: the SNCs. Since then this group has grown to over 30 members, and is divided into seven subgroups. The acronym ‘SNC’ is no longer appropriate, and the meteorites are simply referred to as ‘martian’. The meteorites are all igneous, most are shocked and many show evidence of martian aqueous activity. Study of martian meteorites is a valuable complement to spacecraft observations of Mars, and helps in the understanding of primary magmatic and secondary alteration processes occurring on Mars.