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

dc.contributor.author	Katupotha, K.N.J.
dc.date.accessioned	2014-05-12T09:36:34Z
dc.date.available	2014-05-12T09:36:34Z
dc.date.issued	2014-05-12T09:36:34Z
dc.identifier.citation	Katupotha, 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.uri	http://dr.lib.sjp.ac.lk/handle/123456789/1510
dc.description.abstract	Attached
dc.description.abstract	Pyrite (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.language.iso	en	en_US
dc.title	Pyrite Concentration and Paleoenvironmental Change of the Hiroshima Delta(Japan)	en_US
dc.type	Article	en_US
dc.date.published	1989