Mossbauer, X-ray fluorescence and paleomagnetic studies of deep-sea sediments from the Peru Basin: Two million years of sedimentation history

被引：2

作者：

Drodt, M

Trautwein, AX

Konig, I

Suess, E

Dekkers, MJ

机构：

[1] GEOMAR RES CTR MARINE GEOSCI,D-24148 KIEL,GERMANY

[2] UNIV UTRECHT,PALEOMAGNET LAB,3584 CD UTRECHT,NETHERLANDS

来源：

NUOVO CIMENTO DELLA SOCIETA ITALIANA DI FISICA D-CONDENSED MATTER ATOMIC MOLECULAR AND CHEMICAL PHYSICS FLUIDS PLASMAS BIOPHYSICS | 1996年 / 18卷 / 2-3期

关键词：

D O I：

10.1007/BF02458915

中图分类号：

O4 [物理学];

学科分类号：

0702 ;

摘要：

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). Mossbauer parameters suggest that the iron in the sediments is mainly contained in clay minerals and to varying extent also in goethite.

引用

页码：341 / 345

页数：5