TY - JOUR
T1 - Mössbauer, X-ray fluorescence and paleomagnetic studies of deep-sea sediments from the Peru Basin: Two million years of sedimentation history
AU - Drodt, M.
AU - Trautwein, A. X.
AU - König, Iris
AU - Suess, E.
AU - Dekkers, M. J.
PY - 1996/1/1
Y1 - 1996/1/1
N2 - Sediment cores with different sub-bottom depths (I: 45 cm and II: 700 cm) from the Peru Basin have been investigated. From the depth profile of the relative amount of Fe(II) a redox zone is obtained which correlates with the organic carbon flux into the sediment (core I). Mössbauer parameters suggest that the iron in the sediments is mainly contained in clay minerals and to varying extent also in goethite.
AB - Sediment cores with different sub-bottom depths (I: 45 cm and II: 700 cm) from the Peru Basin have been investigated. From the depth profile of the relative amount of Fe(II) a redox zone is obtained which correlates with the organic carbon flux into the sediment (core I). Mössbauer parameters suggest that the iron in the sediments is mainly contained in clay minerals and to varying extent also in goethite.
UR - http://www.scopus.com/inward/record.url?scp=0040596895&partnerID=8YFLogxK
U2 - 10.1007/BF02458915
DO - 10.1007/BF02458915
M3 - Scientific review articles
AN - SCOPUS:0040596895
SN - 0392-6737
VL - 18
SP - 341
EP - 345
JO - Nuovo Cimento della Societa Italiana di Fisica D - Condensed Matter, Atomic, Molecular and Chemical Physics, Biophysics
JF - Nuovo Cimento della Societa Italiana di Fisica D - Condensed Matter, Atomic, Molecular and Chemical Physics, Biophysics
IS - 2-3
ER -
