Subject |
has augite grain size |
has weather resistance |
has minerology |
is an instance of |
has distinguishing feature |
has fragmentation probability |
has fall location |
has likely origin |
has solidification mechanism |
has name |
has genesi |
has relative abundance |
has prototype |
has total mass of find |
has composition |
is a kind of |
has olivine grain size |
has find date |
has property |
has number of find |
has origin |
has ablative mass loss |
has solidification timescale |
has petrology |
Antarctic meteorite | | which depends on its composition | | | | during meteor phase which depends on composition | indicated by letters in the beginning of name | | | 3 or 4 letter contracted from find location then last two digits of year then id number | | | | 485755 kg | often minerals not found on Earth | meteorite | | recovery year is first 2 numbers in name | | 1691 | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | directly proportional to initial velocity | | |
brachinite | | low | olivine, augite, Fe-sulfide, some orthopyroxene and some sodic plagioclase | | no chondrules | high because it is more friable than iron meteorite | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | metamorphosed chondrite, partial melting residue | cooling in deep underground chambers | based on the locale, region, or nearby town in which the fall occurred | fractional crystallization | 7.1 % of meteorite falls | Brachina meteorite | 1606 kg | olivine and some clinopyroxene | dunitic wehrlite | | | formed by separation of molten rock in a gravity field | 70 | asteroid | high because it is more friable than iron meteorite | very slow | medium- to coarse-grained equigranular |
ALH 84025 | up to 2.7 millimeters | which depends on its composition | olivine, augite, Fe-sulfide, some orthopyroxene and some sodic plagioclase | Antarctic meteorite | no chondrules | during meteor phase which depends on composition | indicated by letters in the beginning of name | metamorphosed chondrite, partial melting residue | cooling in deep underground chambers | ALH 84025 | | | Brachina meteorite | 485755 kg | often minerals not found on Earth | | up to 1.8 millimeters | 1984 | formed by separation of molten rock in a gravity field | 1691 | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | directly proportional to initial velocity | very slow | medium- to coarse-grained equigranular |