Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/38877
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dc.contributor.authorKnedler, K E-
dc.contributor.authorGlasby, G P-
dc.contributor.authorFreeman, A G-
dc.date.accessioned2016-12-19T09:34:25Z-
dc.date.available2016-12-19T09:34:25Z-
dc.date.issued1983-09-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/38877-
dc.description133-137en_US
dc.description.abstractFe is present in much higher concentrations in the fine-grained sediments of the inner shelf off the West Coast of India than in the predominantly carbonate sediments of the outer shelf. The results of Mossbauer spectroscopic analyses of these sediments and their < 2 µm fractions are consistent with X-ray diffraction data and indicate that the Fe is principally associated with clay minerals, particularly montmorillonite. Chlorite and illite are less important sources of Fe in these sediments and Fe oxide hydroxides appear to be present only in small amounts. The inner shelf sediments also contain some pyrite. This indicates a more reducing environment in the inner shelf associated with relatively high detrital sedimentation in this region.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJMS Vol.12(3) [September 1983]en_US
dc.titleMineralogy and geochemistry of iron in some recent continental shelf sediments off Goaen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.12(3) [September 1983]

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