Pyrite Concentration and Paleoenvironmental Change of the Hiroshima Delta(Japan)

dc.contributor.authorKatupotha, K.N.J.
dc.date.accessioned2014-05-12T09:36:34Z
dc.date.available2014-05-12T09:36:34Z
dc.date.issued2014-05-12T09:36:34Z
dc.date.published1989
dc.description.abstractAttached
dc.description.abstractPyrite (FeS2) content in brackish and salt marsh sediments is relatively higher than the amount in freshwater marsh sediments. Different values of pyrite sulfur (FeS2-S) content in sediments from the Hiroshima Delta indicate that poorly drained salt marsh had developed between 27.0m and 28.0m below mean sea – level and palaeo -sea- level was constant for several hundreds of years in the same depth during the early Holocene Epoch.
dc.identifier.citationKatupotha, K.N.J. (1989). Pyrite Concentration and Paleoenvironmental Change of the Hiroshima Delta(Japan). The Korean Journal of Quaternary Research, 3(1), 47-54.
dc.identifier.urihttp://dr.lib.sjp.ac.lk/handle/123456789/1510
dc.language.isoenen_US
dc.titlePyrite Concentration and Paleoenvironmental Change of the Hiroshima Delta(Japan)en_US
dc.typeArticleen_US

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