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Meteorite composition

Meteorite composition. Major groupings: Stony meteorites Chondrites Achondrites Iron meteorites Octahedrites, hexahedrites, ataxites Stony-iron meteorites Pallasites Mesosiderites. Chondrites Carbonaceous chondrite class CI chondrite (Ivuna-like) group

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Meteorite composition

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  1. Meteorite composition • Major groupings: • Stony meteorites • Chondrites • Achondrites • Iron meteorites • Octahedrites, hexahedrites, ataxites • Stony-iron meteorites • Pallasites • Mesosiderites

  2. Chondrites • Carbonaceous chondrite class • CI chondrite (Ivuna-like) group • CM-CO chondrite (mini-chondrule) clan • CM chondrite (Mighei-like) group • CO chondrite (Ornans-like) group • CV-CK chondrite clan • CV chondrite (Vigarano-like) group • CV-oxA chondrite (oxidized, Allende-like) subgroup • CV-oxB chondrite (oxidized, Bali-like) subgroup • CV-red chondrite (reduced) subgroup • CK chondrite (Karoonda-like) group • CR chondrite clan • CR chondrite (Renazzo-like) group • CH chondrite (Allan Hills 85085-like) group • CB chondrite (Bencubbin-like) group • CBa chondrite subgroup • CBb chondrite subgroup • Ordinary chondrite class • H chondrite group • L chondrite group • LL chondrite group • Enstatite chondrite class • EH chondrite group • EL chondrite group • Other chondrite groups, not in one of the major classes • R chondrite (Rumuruti-like) group • K chondrite (Kakangari-like) grouplet (a grouplet is a provisional group with <5 members)

  3. Chondrites • Stony meteorites – most common meteorites and represent the oldest solids that are the building blocks of the solar system • Parent bodies were small-medium asteroids, not planetoids! • Contain up to 80% chondrules, which were freely floating molten drops in space Few mm to 1 cm spheres Mostly olivine and pyroxene, also feldspathic glass or crystals with minor troilite (FeS), chromite, phosphates 15 groups of chondrites

  4. Chondrite groups • Ordinary – make up 80% of the meteorites and 90% of chondritic meteorites, abundant chondrules, variable Fe-Ni lead to H, L, and LL chondrites • Carbonaceous chondrites –less the 5% of chondritic meteorites, few chondrules, more lithophile elements (Ca, Mg, K, Cr, Al, Cl,…), high levels of water and organic compounds - many types based on characteristic specimen • Enstatite Chondrites – 2% of chondritic meteorites, very chemically reduced – enstatite-rich chondrules and abundant metal and sulfide minerals

  5. Peekskill Meteorite Peekskill Meteor: October 9, 1992. This famous fireball was seen and filmed across several eastern states. It broke up into many fragments, one of which hit the trunk of Michelle Knapp's 1980 Chevy Malibu. When Ms. Knapp investigated a crash sound outside her Peekskill, NY home, she discovered the damaged trunk and found a warm 12-kg meteorite lying beside the car. 12-kg Ordinary Chondritic meteorite Car – $10K Meteorite – $75K

  6. Achondrites • Stony meteorite similar to terrestrial basalts or plutonic rocks, represent 8% of meteorites grouped on the basis of Fe/Mn and 17O/18O ratios characteristic of the parent body • 2/3 of these meteorites are HED type, originating from one asteroid, Vesta 4 - there is a large impact crater observed on this asteroid • Also includes Martian and lunar meteorites The Johnstown Diogenite. Lunar Meteorite Allan Hills 81005

  7. Martian Meteorites • All are igneous, lherzolitic to basaltic composition, and some contain hydrated carbonates and sulfates, evidence of liquid water • ALH84001 is 4.5 ga, contains carbonate veins 3.6 – 4 ga, Organic matter (PAH), aligned magnetite crystals, proposed nanofossils (careful!!) – very controversial… ALH84001 – round carbonate grains ALH84001 Nahkla Meteorite

  8. Iron Meteorites • 5% of meteorites, but 90% of the mass of recovered meteorites and all of the largest meteorites (66 tons is the record) - primarily composed of iron-nickel alloy intergrowths: • Kamacite – Fe-Ni alloy at 90:10 to 95:5 Fe:Ni • Taenite – Fe-Ni alloy at 80:20 to 45:65 Fe:Ni • Widmanstätten pattern – finely interweaved Kamacite and Taenite (Octahedrites) • Classified on Ni content: Ataxites>Octahedrites>Hexahedrites

  9. Stony-iron Meteorites • Mix of iron-nickel alloy and silicate minerals (mostly olivine), 1% of meteorites • Pallasites are thought to form a the core-mantle boundary of differentiated asteroids • Mesosiderite – equal parts metal alloy and silicate with a breccia texture

  10. Identifying a meteorite • Fusion crust – dull black to dark brown, often soft, can be weathered to red (but can flake off) • Density – generally dense • Chondrules are specifically meteoritic • Never porous, but can be ‘dimpled’ with surface depressions • 99% of meteorites are magnetic • Unusually high Ni content

  11. Fusion crust forms on entry through the atmosphere

  12. Meteorite/ Comet Impacts • P/T space??

  13. Chicxulub, Yucatan Peninsula, Mexico • K/T event at 64.98 ma, formed from a 6-12 mile diameter asteroid impact (50 megaton blast)

  14. Barringer Meteor Crater, Arizona, formed from Canyon Diable Meteorite

  15. Impact Craters • Many famous impact craters, hundreds known on earth (why might there have been plenty more??) • Sudbury, Ontario (250km diameter, 1.85 ga) • Chesapeake Bay (90km diameter, 35 ma) • Manson, Iowa (35km, 74ma) • Barringer, Arizona (1.2km, 49 ka) • Serpent Mound, Ohio (8km, 320 ma) Clearwater lakes, Quebec – 36+26km diameter, 290 ma

  16. Megatsunamis • Meteorite impact in the ocean displaces huge quantities of water instantly • The Chixculub crater impact generated a megatsunami 150-300 feet high

  17. Energy of an impact • Kinetic energy – going from very fast to stopping is a BIG change in energy • What happens to that energy?? • Impactite – any mineral formed as a result of this impact Shatter cone

  18. Materials indicating Meteorite Impacts • Tektites • Glass formed from impact

  19. Diaplectic Glass • Glass formed through fusion of different minerals – not melted, but fused…

  20. What Happens to minerals that are there but not melted? • Shock Quartz • Lamellae retaining evidence of impact

  21. Diamonds • Very small diamonds can form from impacts and are found in meteorite impact craters around the world • Diamonds can also form in meteorites- these can be gray to black Lonsdalite - Hexagonal allotrope of diamond, specific to meteorite impacts, thought to form from graphite in meteorites

  22. Quartz Polymorphs • Coesite and Stishovite found associated with impact craters

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