madal/kesksüsinikterastes suhteliselt kõrgel martensiitmuutuse algtemperatuuril Ms moodustunud tihedate kihtidena (alla 1 µm) paigutunud martensiit (vt martensiit; vrd nõelmartensiit)
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Martensiit moodustub osaliselt terastes süsinikusisaldusega alla u.1.0 % ja ainult terastes süsinikusisaldusega alla u.0,5 % paralleelsete maatrikpakettidena või kihilisena.
product of martensitic transformation in low- to medium-carbon steels with a relatively high Ms temperature; the martensite crystallites have an apperance of tightly arranged thin (less 1 µm) laths separated by low-angle boundaries (see: martensite; compare: acicular martensite)
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Martensite formed partly in steels containing less than approx. 1.0 % C and solely in steels containing less than approx. 0.5 % C as parallel arrays of packets or lath shape.
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