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  2. Nonmagmatic meteorite - Wikipedia

    en.wikipedia.org/wiki/Nonmagmatic_meteorite

    Nonmagmatic meteorite. Nonmagmatic meteorite (also nonmagmatic iron meteorite) is a deprecated term formerly used in meteoritics to describe iron meteorites that were originally thought to have not formed by igneous processes, to differentiate them from the magmatic meteorites, produced by the crystallization of a metal melt. [1]

  3. Chondrite - Wikipedia

    en.wikipedia.org/wiki/Chondrite

    A chondrite / ˈkɒndraɪt / is a stony (non- metallic) meteorite that has not been modified, by either melting or differentiation of the parent body. [a][1] They are formed when various types of dust and small grains in the early Solar System accreted to form primitive asteroids. Some such bodies that are captured in the planet's gravity well ...

  4. Achondrite - Wikipedia

    en.wikipedia.org/wiki/Achondrite

    Achondrite. A eucrite achondrite from the Millbillillie meteorite shower. An achondrite[1] is a stony meteorite that does not contain chondrules. [2][3] It consists of material similar to terrestrial basalts or plutonic rocks and has been differentiated and reprocessed to a lesser or greater degree due to melting and recrystallization on or ...

  5. Meteorite - Wikipedia

    en.wikipedia.org/wiki/Meteorite

    Meteorite. The 60- tonne, 2.7 m-long (8.9 ft) Hoba meteorite in Namibia is the largest known intact meteorite. [1] A meteorite is a rock that originated in outer space and has fallen to the surface of a planet or moon. When the original object enters the atmosphere, various factors such as friction, pressure, and chemical interactions with the ...

  6. Micrometeorite - Wikipedia

    en.wikipedia.org/wiki/Micrometeorite

    A micrometeorite is a micrometeoroid that has survived entry through the Earth's atmosphere. Usually found on Earth 's surface, micrometeorites differ from meteorites in that they are smaller in size, more abundant, and different in composition. The IAU officially defines meteoroids as 30 micrometers to 1 meter; micrometeorites are the small ...

  7. L chondrite - Wikipedia

    en.wikipedia.org/wiki/L_chondrite

    L chondrite. The L type ordinary chondrites are the second most common group of meteorites, accounting for approximately 35% of all those catalogued, and 40% of the ordinary chondrites. [1] The ordinary chondrites are thought to have originated from three parent asteroids, with the fragments making up the H chondrite, L chondrite and LL ...

  8. Carbonaceous chondrite - Wikipedia

    en.wikipedia.org/wiki/Carbonaceous_chondrite

    Alternative names. C chondrites. Carbonaceous chondrites or C chondrites are a class of chondritic meteorites comprising at least 8 known groups and many ungrouped meteorites. They include some of the most primitive known meteorites. The C chondrites represent only a small proportion (4.6%) [1] of meteorite falls.

  9. Troilite - Wikipedia

    en.wikipedia.org/wiki/Troilite

    Troilite (/ ˈtrɔɪlaɪt /) is a rare iron sulfide mineral with the simple formula of FeS. It is the iron-rich endmember of the pyrrhotite group. Pyrrhotite has the formula Fe (1-x) S (x = 0 to 0.2) which is iron deficient. As troilite lacks the iron deficiency which gives pyrrhotite its characteristic magnetism, troilite is non-magnetic.