LL5 chondrite Comparison Table

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LL5 chondrite comparison table

Subject has weather resistance has olivine shock metamorphism is independent of has shock pressure has acronym has olivine composition has image has weather has relative abundance has fragmentation probability has metamorphism mechanism has weathering stage has number of fragment has find date has comment has orthopyroxene shock metamorphism has plagioclase shock metamorphism has degree of shock metamorphism has mass has shock diagnostic mineral has name be shock has fall location is an instance of has pyroxene composition has shock stage has composition has value has fall coordinate has ablative mass loss classified by

DaG 222 which depends on its composition planar fractures, undulatory extinction, irregular fractures the nature and degree of thermal metamorphism or aqueous alteration 15 to 20 GPa DaG
can be severe due to long exposure time to environmental corrosion agents during meteor phase which depends on composition shock metamorphism W3 1996 breccia clinoenstatite lamellae on (100), undulatory extinction, planar fractures, irregular fractures undulatory extinction weakly shocked 0.837 kg orthopyroxene for enstatite chondrite DaG 222 before, during or after other types of metamorphism Dar al Gani plateau, Libyan Sahara Desert S3 shock stage chondrite S3 bronzite, olivine and minor oligoclase lower because the fall was not witnessed 27° 27.20' N., 16° 18.76' E. directly proportional to initial velocity

Dag 596 which depends on its composition undulatory extinction, irregular fractures the nature and degree of thermal metamorphism or aqueous alteration 5 to 10 GPa DaG Fa% 29.6
can be severe due to long exposure time to environmental corrosion agents during meteor phase which depends on composition thermal metamorphism W1 1 1998 undulatory extinction, irregular fractures, some planar fractures undulatory extinction, irregular fractures very weakly shocked 0.189 kg orthopyroxene for enstatite chondrite based on the locale, region, or nearby town in which the fall occurred before, during or after other types of metamorphism Dar al Gani plateau, Libyan Sahara Desert LL5 chondrite Fs% 22.5 S2 bronzite, olivine and minor oligoclase lower because the fall was not witnessed 27° 12.82' N. 16°16.89' E. directly proportional to initial velocity A. Sexton, Open University, UK. Meteoritical Bulletin No 83

Dag 633 which depends on its composition undulatory extinction, irregular fractures the nature and degree of thermal metamorphism or aqueous alteration 5 to 10 GPa DaG Fa% 27.1
can be severe due to long exposure time to environmental corrosion agents during meteor phase which depends on composition thermal metamorphism W2 1 1998 contains angular fragments undulatory extinction, irregular fractures, some planar fractures undulatory extinction, irregular fractures very weakly shocked 0.210 kg orthopyroxene for enstatite chondrite based on the locale, region, or nearby town in which the fall occurred before, during or after other types of metamorphism Dar al Gani plateau, Libyan Sahara Desert LL5 chondrite Fs% 23.4 S2 bronzite, olivine and minor oligoclase lower because the fall was not witnessed 26° 55.14' N. 16° 40.65' E. directly proportional to initial velocity A. Sexton, Open University, UK. Meteoritical Bulletin No 84

DaG 639 which depends on its composition planar fractures, undulatory extinction, irregular fractures the nature and degree of thermal metamorphism or aqueous alteration 15 to 20 GPa DaG Fa% 26.8
can be severe due to long exposure time to environmental corrosion agents during meteor phase which depends on composition thermal metamorphism W2 1 1998 clinoenstatite lamellae on (100), undulatory extinction, planar fractures, irregular fractures undulatory extinction weakly shocked 0.237 kg orthopyroxene for enstatite chondrite based on the locale, region, or nearby town in which the fall occurred before, during or after other types of metamorphism Dar al Gani plateau, Libyan Sahara Desert LL5 chondrite Fs% 22.1 S3 bronzite, olivine and minor oligoclase lower because the fall was not witnessed 26° 56.41' N. 16° 25.14' E. directly proportional to initial velocity A. Sexton, Open University, UK. Meteoritical Bulletin No 84

Lazbuddie low 85.7 % of meteorite falls high because it is more friable than iron meteorite thermal metamorphism based on the locale, region, or nearby town in which the fall occurred strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity LL5 chondrite bronzite, olivine and minor oligoclase in degrees, minutes and seconds of lattitude and longitude high because it is more friable than iron meteorite

Roosevelt Co 094 low 85.7 % of meteorite falls high because it is more friable than iron meteorite thermal metamorphism based on the locale, region, or nearby town in which the fall occurred strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity LL5 chondrite bronzite, olivine and minor oligoclase in degrees, minutes and seconds of lattitude and longitude high because it is more friable than iron meteorite

Sahara 97021 which depends on its composition planar fractures, undulatory extinction, irregular fractures the nature and degree of thermal metamorphism or aqueous alteration 15 to 20 GPa
can be severe due to long exposure time to environmental corrosion agents during meteor phase which depends on composition shock metamorphism W2 February 1997 clinoenstatite lamellae on (100), undulatory extinction, planar fractures, irregular fractures undulatory extinction weakly shocked 0.895 kg orthopyroxene for enstatite chondrite Sahara 97021 before, during or after other types of metamorphism Sahara Desert S3 shock stage chondrite S3 often minerals not found on Earth lower because the fall was not witnessed y° 08' 52" N., x° 28' 49" W. directly proportional to initial velocity

Tuxtuac low 85.7 % of meteorite falls high because it is more friable than iron meteorite thermal metamorphism based on the locale, region, or nearby town in which the fall occurred strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity LL5 chondrite bronzite, olivine and minor oligoclase in degrees, minutes and seconds of lattitude and longitude high because it is more friable than iron meteorite

Next LL chondrite: LL6 chondrite Up: LL chondrite, type 5 chondrite Previous LL chondrite: LL4 chondrite

Subject	has weather resistance	has olivine shock metamorphism	is independent of	has shock pressure	has acronym	has olivine composition	has image	has weather	has relative abundance	has fragmentation probability	has metamorphism mechanism	has weathering stage	has number of fragment	has find date	has comment	has orthopyroxene shock metamorphism	has plagioclase shock metamorphism	has degree of shock metamorphism	has mass	has shock diagnostic mineral	has name	be shock	has fall location	is an instance of	has pyroxene composition	has shock stage	has composition	has value	has fall coordinate	has ablative mass loss	classified by
DaG 222	which depends on its composition	planar fractures, undulatory extinction, irregular fractures	the nature and degree of thermal metamorphism or aqueous alteration	15 to 20 GPa	DaG			can be severe due to long exposure time to environmental corrosion agents		during meteor phase which depends on composition	shock metamorphism	W3		1996	breccia	clinoenstatite lamellae on (100), undulatory extinction, planar fractures, irregular fractures	undulatory extinction	weakly shocked	0.837 kg	orthopyroxene for enstatite chondrite	DaG 222	before, during or after other types of metamorphism	Dar al Gani plateau, Libyan Sahara Desert	S3 shock stage chondrite		S3	bronzite, olivine and minor oligoclase	lower because the fall was not witnessed	27° 27.20' N., 16° 18.76' E.	directly proportional to initial velocity
Dag 596	which depends on its composition	undulatory extinction, irregular fractures	the nature and degree of thermal metamorphism or aqueous alteration	5 to 10 GPa	DaG	Fa% 29.6		can be severe due to long exposure time to environmental corrosion agents		during meteor phase which depends on composition	thermal metamorphism	W1	1	1998		undulatory extinction, irregular fractures, some planar fractures	undulatory extinction, irregular fractures	very weakly shocked	0.189 kg	orthopyroxene for enstatite chondrite	based on the locale, region, or nearby town in which the fall occurred	before, during or after other types of metamorphism	Dar al Gani plateau, Libyan Sahara Desert	LL5 chondrite	Fs% 22.5	S2	bronzite, olivine and minor oligoclase	lower because the fall was not witnessed	27° 12.82' N. 16°16.89' E.	directly proportional to initial velocity	A. Sexton, Open University, UK. Meteoritical Bulletin No 83
Dag 633	which depends on its composition	undulatory extinction, irregular fractures	the nature and degree of thermal metamorphism or aqueous alteration	5 to 10 GPa	DaG	Fa% 27.1		can be severe due to long exposure time to environmental corrosion agents		during meteor phase which depends on composition	thermal metamorphism	W2	1	1998	contains angular fragments	undulatory extinction, irregular fractures, some planar fractures	undulatory extinction, irregular fractures	very weakly shocked	0.210 kg	orthopyroxene for enstatite chondrite	based on the locale, region, or nearby town in which the fall occurred	before, during or after other types of metamorphism	Dar al Gani plateau, Libyan Sahara Desert	LL5 chondrite	Fs% 23.4	S2	bronzite, olivine and minor oligoclase	lower because the fall was not witnessed	26° 55.14' N. 16° 40.65' E.	directly proportional to initial velocity	A. Sexton, Open University, UK. Meteoritical Bulletin No 84
DaG 639	which depends on its composition	planar fractures, undulatory extinction, irregular fractures	the nature and degree of thermal metamorphism or aqueous alteration	15 to 20 GPa	DaG	Fa% 26.8		can be severe due to long exposure time to environmental corrosion agents		during meteor phase which depends on composition	thermal metamorphism	W2	1	1998		clinoenstatite lamellae on (100), undulatory extinction, planar fractures, irregular fractures	undulatory extinction	weakly shocked	0.237 kg	orthopyroxene for enstatite chondrite	based on the locale, region, or nearby town in which the fall occurred	before, during or after other types of metamorphism	Dar al Gani plateau, Libyan Sahara Desert	LL5 chondrite	Fs% 22.1	S3	bronzite, olivine and minor oligoclase	lower because the fall was not witnessed	26° 56.41' N. 16° 25.14' E.	directly proportional to initial velocity	A. Sexton, Open University, UK. Meteoritical Bulletin No 84
Lazbuddie	low								85.7 % of meteorite falls	high because it is more friable than iron meteorite	thermal metamorphism										based on the locale, region, or nearby town in which the fall occurred		strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity	LL5 chondrite			bronzite, olivine and minor oligoclase		in degrees, minutes and seconds of lattitude and longitude	high because it is more friable than iron meteorite
Roosevelt Co 094	low								85.7 % of meteorite falls	high because it is more friable than iron meteorite	thermal metamorphism										based on the locale, region, or nearby town in which the fall occurred		strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity	LL5 chondrite			bronzite, olivine and minor oligoclase		in degrees, minutes and seconds of lattitude and longitude	high because it is more friable than iron meteorite
Sahara 97021	which depends on its composition	planar fractures, undulatory extinction, irregular fractures	the nature and degree of thermal metamorphism or aqueous alteration	15 to 20 GPa				can be severe due to long exposure time to environmental corrosion agents		during meteor phase which depends on composition	shock metamorphism	W2		February 1997		clinoenstatite lamellae on (100), undulatory extinction, planar fractures, irregular fractures	undulatory extinction	weakly shocked	0.895 kg	orthopyroxene for enstatite chondrite	Sahara 97021	before, during or after other types of metamorphism	Sahara Desert	S3 shock stage chondrite		S3	often minerals not found on Earth	lower because the fall was not witnessed	y° 08' 52" N., x° 28' 49" W.	directly proportional to initial velocity
Tuxtuac	low								85.7 % of meteorite falls	high because it is more friable than iron meteorite	thermal metamorphism										based on the locale, region, or nearby town in which the fall occurred		strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity	LL5 chondrite			bronzite, olivine and minor oligoclase		in degrees, minutes and seconds of lattitude and longitude	high because it is more friable than iron meteorite