TY - JOUR
T1 - Mossbauer studies of palygorskite and some aspects of palygorskite mineralogy.
AU - Heller-Kallai, L.
AU - Rozenson, I.
PY - 1981
Y1 - 1981
N2 - In three samples of palygorskite, Fe3+ was found from Mossbauer data to occupy edge sites with relatively regular 6-coordination, and M(1) or M(2) sites in the interior of the chains. Data obtained on heating are compatible with a model of palygorskite dehydroxylate previously proposed by Preisinger (1963, in Clays and Clay Minerals, Proc. 10th Nat. Conf., Austin, Texas, 1961, pp 365-371). -D.F.B.
AB - In three samples of palygorskite, Fe3+ was found from Mossbauer data to occupy edge sites with relatively regular 6-coordination, and M(1) or M(2) sites in the interior of the chains. Data obtained on heating are compatible with a model of palygorskite dehydroxylate previously proposed by Preisinger (1963, in Clays and Clay Minerals, Proc. 10th Nat. Conf., Austin, Texas, 1961, pp 365-371). -D.F.B.
UR - http://www.scopus.com/inward/record.url?scp=0019687118&partnerID=8YFLogxK
U2 - 10.1346/CCMN.1981.0290309
DO - 10.1346/CCMN.1981.0290309
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AN - SCOPUS:0019687118
SN - 0009-8604
VL - 29
SP - 226
EP - 232
JO - Clays and Clay Minerals
JF - Clays and Clay Minerals
IS - 3
ER -