SUMMARY
.The
ariicls
del!lils
IW:IJIh
the
prIOIC!E!IS8of
.
l:ryStaJOiza-tIm· of
melted
'basalht,
rtbe
~e.
af
rwIh&JcIh
jJs~
iI!O
~.
litis
<lIPt'J,mum
~btian8bru1Cture
In
pri\ICIIILcIeI.
Under
the
Il8llIe''oaIIIt
.
sIboIlIe"
the
aut1mIl'S
UJDKleIr-9tand
bEire
It!le IIlIaIf:.eIrtl8
'WflBdl
!18
obtalMd
after
mel-iflin,g
Il1Odk:s
lOll'rodk:
mlDItt.ural~IImd
due
ItoItI1e
~~1IJJan,
of rtihIe
~.'lltre
studies on ·the
ory-ataII:LIrzJa,t1klin
IPIMC'eISIS
!Of
~If;fCI8I3It stonJe !WI8re made
on
basalt
from Mlkolowice, near Legnlca.
PE310ME
~s: IIO.lJY'H!H:HJl OIITHMa.ln.aoA: CTPYKTYPId mIaBJIeB-Boro, IIepeKPHCTaJIJIH30B8HHOro 683aJ1DTa Be06xo~HJlO
3BaTh· 1IIexam1311
ero
KPHCTa.JLT.IH3~.STOA
np06JIe-!lie IIOC~eBa BBC1'OSIIq8S1
pa6oTa.
IIo~ lIB3BaBHeM'
ltBlIIeBBOro cnn8aa
aBTOPLI' ixo~Pa3yJIeBaIOT B~,' IIOJIy'Iemroe B HTOre lLlIaB-JIEmUI IIOP01t IIltJIH HX ClIIeceA C mmpaBJIemroA:
Jq)JI-CTa.lIJIH3~eA:. paCIIJzaBa. JilccJIe,a;oaaHJUI KexaHH!W:8
KPHCT'aJIH3~ 6a3aJI&TOBOl'O paClLlIaBa npOBO~Ch
Ha 683aJIbTe H3 IIIe.cTHOCTH MHKioJIOBHD;e.