Comet impactite, Carbon Quartz Extraterrestrial formed TEKTITE
Robin Brett Author and Article Information American Mineralogist (1967) 52 (5-6): 721-733. Article history Cite Share Permissions Abstract Electron microprobe analyses indicate that Ni-Fe spherules within impactite glass bombs from the Meteor Crater area, Arizona, contain from 20 to 65 weight percent Ni.
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Tektites are "splash droplets" from major meteorite impacts on the Earth. Some of the most prized tektites are the unique bottle-glass green Moldavites from the Czech Republic, which were formed by a massive impact 15 million years ago in what is now Germany.
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The meteorite collection goes back to the earliest history of the Museum. The first meteorite in the collection was a 46g piece of the Searsmont (H5 ordinary chondrite) donated in 1872 by Mr. G.M. Brainerd of Rockville, Maine. In 1874 the Museum purchased the S.C.H. Bailey mineral collection which included eight meteorites.
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The criteria for differentiating between impact and volcanic glasses are their very low water content (compared to obsidians), the presence of high-temperature and/or high-pressure phases, and.
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Impactites have shown a wider range of values, not only going well above 0.2%, but going below 0.2%, as well, thereby overlapping obsidian and tektites. This "fact" raises several questions which I would like to find answers, but that pursuit is outside the focus of this study.
Tektite
These impactite bombs, com-monly contain small Ni-Fe spherules. Previous analysesof metallic spherulesfrom meteorite impact craters indicate that the spherules are richer in Ni than the parent meteorite from which they were derived. The Ni content of metallic spherulesin tektites is consistently low with respect to impactite spherules.
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Recently, the detailed microscopic and crystallographic study of impact ejecta from Kamil crater and the Australasian tektite strewn field pointed in turn to a different coesite formation.
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These terrestrial rocks, physically altered by the tremendous heat, pressure and shock waves associated with very large meteorite impacts, are known as impactites. Usually only the very largest crater-forming events generate the energy required to melt, fragment, or even vaporize terrestrial rocks.
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What makes them the same? Both fascinating stone categories combine the energy of earth and space to bring you healing that is out-of-this-world. Discover a power beyond your imagination when you work with fascinating Tektites and bold Impactites.
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Just as information, tektite is, like impactite, a preamble for minerals that occur after a meteoroid. So to be precise moldavite is a tektite. Everything labeled tektite can be classified even more accurate because tektite by itself is no name for a mineral :) Reply
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A tektite is a terrestrial molten rock fragment ejected out of the crater during a meteor impacts, it is formed during collision with large meteorites. An impactite is a terrestrial rock modified by the high stresses of pressure and temperature during a meteorite impact, it is generally the rocks present in the impact crater.
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Figure 2 shows the groupings of tektite and impactite formation ages. Geological vs. geochronological ages Occasionally geological ages based on stratigraphy have been given lower values than have been found by the fission track and K-Ar methods. One sug- gested explanation (BAKEB, I960) is that tektites might somehow have been created long.
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Impactite Specimen Showcase. Your Horoscope with Impactites. Magic of Moldavite; Black Tektite from Above. Tektite Jewelry Showcase. Craters for your Collection. Expand your world and your crystal collection with Tektites and Impactites. Explore the Satin Crystals Tektite Shop or buy them right here on the blog:
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Characteristics Impactite includes shock-metamorphosed target rocks, melts ( suevites) and mixtures of the two, as well as sedimentary rocks with significant impact-derived components (shocked mineral grains, tektites, anomalous geochemical signatures, etc.). In June 2015, NASA reported that impact glass has been detected on the planet Mars.
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1. Impact diamonds: Impact diamonds are the result of shock transformation of graphite or coal at pressures in excess of 30 GPa ( Masaitis 1993; Koeberl et al. 1997; Gilmour 1998 ). Occurrences of impact diamond are known from several impact structures (review by Gilmour, 1998).
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Characteristics. Although tektites are superficially similar to some terrestrial volcanic glasses (), they have unusual distinctive physical characteristics that distinguish them from such glasses.First, they are completely glassy and lack any microlites or phenocrysts, unlike terrestrial volcanic glasses.Second, although high in silica (>65 wt%), the bulk chemical and isotopic composition of.