Magnetic properties of four stony meteorites, namely, Allende, Dhajala
and St, Severin (chondrites) and Norton County (achondrite) were stud
ied. The intensity of NRM, susceptibility and the Koenigsberger ratio
of these meteorites are moderate and in the range of igneous rocks. Sa
turation remanent hysteresis experiments of these meteorites reveal hi
gh remanent coercive forces, giving them very high retentive capabilit
y. A study of susceptibility variation with temperature (in low temper
ature region) and the Lowrie-Fuller Test reveals that the magnetic mat
erial in these rocks is in a very fine grained form giving high stabil
ity to these meteorites, The laboratory demagnetization experiments (A
F and thermal) indicate high mdf and blocking temperatures suggest the
ir suitability to palaeofield intensity determinations, These magnetic
properties which are similar to those of other stony meteorites sugge
st that the magnetic mineral in these meteorites is probably tetrataen
ite along with other minerals such as troilite, kamacite, magnetite, e
tc., with high coercive force and carry a magnetic remanence acquired
in an extraterrestrial field.