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LL chondrite comparison table
Subject has alteration temperature range has olivine and low Ca pyroxene homogeneity has part feldspar has metamorphism mechanism has degree of secondary process has chondrule glass type has part chondrule has degree of aqueous alteration has total mass of find has structural state of low Ca pyroxene has part matrix has degree of thermal metamorphism has part carbon has petrologic type is a kind of has part water has number of find
LL3 chondrite greater than 5 % deviationsminor primary grains only  clear, isotropic, variable abundancechondrules very sharply definednone90 kgpredominantly monoclinicclastic and minor opaquenone0.2 to 1 % by weight3type 3 chondrite0.3 to 3 % by weight5
LL4 chondritethe range over at which the alteration took placeless than 5 % mean deviationssecondary, grains than 2 micronsthermal metamorphismproviding insight into geological evolution of parent asteroiddevitrified, absentchondrules well defined 124 kggreater than 20 % monoclinictransparent, recrystallized, small crystalsweakless than 0.2 % by weight4type 4 chondriteless than 1.5 % by weight2
LL5 chondritethe range over at which the alteration took placehomogeneoussecondary, 2 to 50 micron grainsthermal metamorphismproviding insight into geological evolution of parent asteroiddevitrified, absentchondrules readily delineated 184 kgless than 20 % monoclinictransparent, recrystallized, moderate size crystalsmoderateless than 0.2 % by weight5type 5 chondriteless than 1.5 % by weight9
LL6 chondritethe range over at which the alteration took placehomogeneoussecondary, grains greater than 50 micronsthermal metamorphismproviding insight into geological evolution of parent asteroiddevitrified, absentchondrules poorly defined 715 kgorthorhombictransparent, recrystallized, coarse crystalsstrongless than 0.2 % by weight6type 6 chondriteless than 1.5 % by weight20

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