Subject |
is an instance of |
has chromite content |
has distinguishing feature |
has olivine grain shape |
has olivine content |
has fall location |
has metal content |
has formation cooling rate |
has name |
has olivine crystal distribution |
parent body radiu |
has olivine composition |
has weather |
has letter designation |
has relative abundance |
has value |
has total mass of find |
has phosphate content |
has fall coordinate |
has olivine composition uniformity |
has composition |
has troilite content |
has schreibersite content |
is a kind of |
has olivine grain size |
has find date |
has nickel content |
has mass |
has image |
has number of find |
has origin |
has minor mineral |
has definition |
main group pallasite | | 1 % or less by volume | mixture of iron-nickel alloy and non-metallic minerals | from angular fragments to rounded | 35 to 85 % by volume | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | higher than that of average solar system material | 2.5 to 4 degrees C per million years | based on the locale, region, or nearby town in which the fall occurred | from homogeneous to heterogeneous | 78 to 97 kilometers | Fo 88+-1 | | PAL | 1.5 % of meteorite falls | | 7207 kg | 1 % or less by volume | in degrees, minutes and seconds of lattitude and longitude | heterogeneous elements are zoned between grain rim and core | metallic iron plus olivine; core/mantle boundary samples | 0.1 to 7.3 % by volume | 0.3 to 2.8 % by volume | pallasite | typically one centimeter | | always greater than 4 % | | | 33 | planet or asteroid much larger than 100 km in diameter | schreibersite | |
meteorite find | | | | | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | | | based on the locale, region, or nearby town in which the fall occurred | | | | can be severe due to long exposure time to environmental corrosion agents | | | lower because the fall was not witnessed | 485755 kg | | in degrees, minutes and seconds of lattitude and longitude | | often minerals not found on Earth | | | meteorite | | when the meteorite was found | | | | 1691 | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | | a meteorite whose fall was not witnessed |
Imilac | main group pallasite | 1 % or less by volume | mixture of iron-nickel alloy and non-metallic minerals | from angular fragments to rounded | 35 to 85 % by volume | Atacama Desert southwest of Imilac, Chile | higher than that of average solar system material | 2.5 to 4 degrees C per million years | Imilac | from homogeneous to heterogeneous | 78 to 97 kilometers | Fo 88+-1 | grade 2 (subject to weathering) | PAL | | lower because the fall was not witnessed | 7207 kg | 1 % or less by volume | 24° 12.2' S., 68° 48.4' W. | heterogeneous elements are zoned between grain rim and core | 9.9% Ni, 21.1 ppm Ga, 46.0 ppm Ge, 0.071 ppm Ir | 0.1 to 7.3 % by volume | 0.3 to 2.8 % by volume | | typically one centimeter | 1820 | always greater than 4 % | 240 kg |
 | 33 | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | schreibersite | |