Dag 635 | has image
 |  |
is an instance of Dar al Gani meteorite |  |
is an instance of S3 shock stage chondrite |  |
is an instance of H5 chondrite |  |
has mass 1.390 kg |  |
has find date 1998 |  |
has weathering stage W2 |  |
has olivine composition Fa% 19.8 |  |
has pyroxene composition Fs% 17.7 |  |
classified by A. Sexton, Open University, UK. Meteoritical Bulletin No 84  |  |
has number of fragments 1 |  |
has fall coordinates 26° 54.29' N. 16° 40.74' E.  |  |
Dar al Gani meteorite | has fall location Dar al Gani plateau, Libyan Sahara Desert |  |
has acronym DaG |  |
S3 shock stage chondrite | has olivine shock metamorphism planar fractures, undulatory extinction, irregular fractures |  |
has plagioclase shock metamorphism undulatory extinction |  |
has orthopyroxene shock metamorphism clinoenstatite lamellae on (100), undulatory extinction, planar fractures, irregular fractures |  |
H5 chondrite | has total mass of finds 1267 kg |  |
has number of finds 76 |  |
shocked chondrite | is independent of the nature and degree of thermal metamorphism or aqueous alteration |  |
can be shocked before, during or after other types of metamorphism |  |
has shock pressure the equilibration peak shock pressure in GPa (gigapascals) for ordinary chondrites only |  |
has shock diagnostic mineral olivine and plagioclase for ordinary chondrite |  |
has shock diagnostic mineral olivine for carbonaceous chondrite |  |
has shock diagnostic mineral orthopyroxene for enstatite chondrite |  |
S3 shock stage meteorite | has shock stage S3 |  |
has shock pressure 15 to 20 GPa |  |
has degree of shock metamorphism weakly shocked |  |
H chondrite | has synonym bronzite chondrite |  |
has chondrule abundance 60 to 80 % by volume |  |
has matrix abundance 10 to 15 % by volume |  |
has refractory inclusion abundance 0.1 to 1 % by volume |  |
has metal abundance 10 % by volume |  |
has chondrule mean diameter 0.3 millimeters |  |
has total iron content high |  |
has metal iron content 12 to 21 % |  |
has iron metal and iron sulfide 75 % of total iron |  |
type 5 chondrite | has petrologic type 5 |  |
has degree of thermal metamorphism moderate |  |
has olivine and low Ca pyroxene homogeneity homogeneous |  |
has structural state of low Ca pyroxene less than 20 % monoclinic |  |
has chondrule glass type devitrified, absent |  |
has part feldspar secondary, 2 to 50 micron grains |  |
has part maximum bulk Ni in metal greater than 20 % by weight, kamacite and taenite in exsolution relationship |  |
has part sulfide Ni content less than 0.5 % by weight |  |
has part matrix transparent, recrystallized, moderate size crystals |  |
has part chondrule chondrules readily delineated |  |
has part carbon less than 0.2 % by weight |  |
has part water less than 1.5 % by weight |  |
meteorite | has fall date recorded by eyewitness or inferred from dating methods |  |
has fall map which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity |  |
can have crater image |  |
has original mass which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site |  |
has composition often minerals not found on Earth |  |
has relative abundance |  |
has impact velocity when it hits the ground which is smaller than its velocity before it enters the atmosphere |  |
has impact angle |  |
has weather resistance which depends on its composition |  |
has monetary value large if the fall was witnessed |  |
has name based on the locale, region, or nearby town in which the fall occurred |  |
often produce power outages and failures in electrical equipment due to EMP (electromagnetic pulse) |  |
can be associated with crater |  |
has origin meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal |  |
vaporizes completely if size is between 3 micrometers and 3 millimeters |  |
can survive fall if size is larger than 3 mm and velocity is less than 24 km per second |  |
can survive fall if it fragments because smaller pieces with less mass are more easily slowed by the atmosphere |  |
has ablative mass loss depending on composition, more friable stony meteoroids loses more mass than iron meteoroid |  |
has ablative mass loss directly proportional to initial velocity |  |
can shatter during impact phase |  |
can fragment during meteor phase |  |
has fragmentation probability during meteor phase which depends on composition |  |
meteorite find | has value lower because the fall was not witnessed |  |
has weathering can be severe due to long exposure time to environmental corrosion agents |  |
altered chondrite | has degree of secondary processing providing insight into geological evolution of parent asteroid |  |
shocked meteorite | has metamorphism mechanism shock metamorphism |  |
ordinary chondrite | has abundance most common chondrite observed from falls |  |
thermally altered chondrite | has metamorphism mechanism thermal metamorphism |  |
has alteration temperature range the range over at which the alteration took place |  |
rock | has part mineral |  |
has texture |  |
has genesis |  |
chondrite | has petrologic type range which depends on degree of aqueous alteration and thermal metamorphism |  |
has homogeneity of olivine and low Ca pyroxene definition goes here |  |
has part metal maximum bulk in weight % |  |
has part mean Ni content of sulfides in weight % |  |
undifferentiated meteorite | has peak temperature less than 950 degree Celsius during its entire history since solidification |  |
has parent body asteroid smaller than 100 km in diameter |  |
has age oldest and most primitive rock in solar system |  |
conglomerate | has sediment mechanism agglomeration of particles, many of which record individual, diverse histories |  |