Subject |
has part mean Ni content of sulfide |
has solidification timescale |
has part carbon |
has olivine shock metamorphism |
has part matrix |
is independent of |
has shock pressure |
has acronym |
has matrix abundance |
has shock texture |
has letter designation |
has sediment mechanism |
has origin |
has likely origin |
has image |
has weather |
has distinguishing feature |
has degree of secondary process |
has part feldspar |
has metal abundance |
has refractory inclusion abundance |
has solidification mechanism |
has chondrule mean diameter |
has petrology |
has weathering stage |
is a kind of |
has chondrule glass type |
has age |
has number of fragment |
has number of find |
has find date |
has part water |
has comment |
has orthopyroxene shock metamorphism |
has plagioclase shock metamorphism |
has characteristic mineral |
has degree of shock metamorphism |
has mass |
has peak temperature |
has shock diagnostic mineral |
be shock |
has fall location |
is an instance of |
has pyroxene composition |
has shock stage |
has part metal maximum bulk |
be an acronym for |
has homogeneity of olivine and low Ca pyroxene |
has structural state of low Ca pyroxene |
has matrix composition |
has value |
has fall coordinate |
has minerology |
has total mass of find |
has chondrule abundance |
has parent body |
has part chondrule |
has olivine grain characteristic |
classified by |
has petrologic type range |
DaG 609 | | very rapid | | | | | 15 to 20 GPa | DaG | | | AUEC | | 4 Vesta | cumulates, crystallized melts, impact mixing |
 | can be severe due to long exposure time to environmental corrosion agents | no chondrules | | | | | extrusion onto the surface of the planet or asteroid via a volcanic eruption | | coarse-grained orthopyroxenites, gabbros, fine- to coarse-grained basalts, brecciated | W2 | | | | 2 | 23 | 1998 | | iron-rich, monomict, with chromite grains | | | anorthite-pigeonite Ca-rich | weakly shocked | 0.696 kg | | | | Dar al Gani plateau, Libyan Sahara Desert | eucrite | Fs% 27-63 | S3 | | Howardite, Eucrite, Diogenite | | | | lower because the fall was not witnessed | 26° 53.13' N. 16° 34.81' E. | orthopyroxene, olivine, chromite; pigeonite, calcic plagioclase, silica | 231 kg | | | | | A. Sexton, Open University, UK. A. Sexton, Meteoritical Bulletin No 83 | |
low shock ureilite | | very slow | | fracturing, undulatory extinction and kink bands | | | less than 20 GPa | | | silicates show minor fracturing, undulatory extinction and kink bands primarily in olivine | AURE | | asteroid | partial melting residue | | | no chondrules | | | | | cooling in deep underground chambers | | coarse-grained granular | | S3 shock stage meteorite | | | | 6 (out of date) | | | | | | olivine-pigeonite about 90% by volume | low | | | small euhedral graphite crystals can sometimes be distinguished | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | | | S2-S3 | | | | | carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume | | in degrees, minutes and seconds of lattitude and longitude | olivine, pyroxene (some combination of pigeonite, orthopyroxene, augite) | 9 kg (out of date) | | | | reduced rims contacting carbonaceous matrix material 0.1 mm FeO-free olivine and/or enstatite rims riddled with tiny inclusions of low-Ni metal | | |
S3 shock stage chondrite | in weight % | | in weight % | planar fractures, undulatory extinction, irregular fractures | fine grained disequilibrium mixture of silicates, oxides, metal, sulfides and organic constituents | the nature and degree of thermal metamorphism or aqueous alteration | 15 to 20 GPa | | in volume % | | | agglomeration of particles, many of which record individual, diverse histories | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | | | | | providing insight into geological evolution of parent asteroid | usually plagioclase tectosilicate | in volume % | in volume % | | millimeters | | | S3 shock stage meteorite | | oldest and most primitive rock in solar system | | 1691 | | in weight % | | clinoenstatite lamellae on (100), undulatory extinction, planar fractures, irregular fractures | undulatory extinction | | weakly shocked | | less than 950 degree Celsius during its entire history since solidification | orthopyroxene for enstatite chondrite | before, during or after other types of metamorphism | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | | | S3 | in weight % | | definition goes here | definition goes here | | | in degrees, minutes and seconds of lattitude and longitude | | 485755 kg | in volume % | asteroid smaller than 100 km in diameter | small sphere of about 1 mm diameter of formerly melted minerals | | | which depends on degree of aqueous alteration and thermal metamorphism |