Carbon-sulfur-iron relationships in sedimentary rocks from southwestern Taiwan: influence of geochemical environment on greigite and pyrrhotite formation

NCUIR > College of Earth Sciences > Graduate Institute of Hydrological and Oceanic Sciences > journal & Dissertation > Item 987654321/36090

Please use this identifier to cite or link to this item: http://ir.lib.ncu.edu.tw/handle/987654321/36090

Title:	Carbon-sulfur-iron relationships in sedimentary rocks from southwestern Taiwan: influence of geochemical environment on greigite and pyrrhotite formation
Authors:	Kao,SJ;Horng,CS;Roberts,AP;Liu,KK
Contributors:	水文與海洋科學研究所
Keywords:	REACTIONS FORMING PYRITE;MARINE-SEDIMENTS;HOLOCENE SEDIMENTS;MAGNETIC POLARITIES;SULFATE REDUCTION;ORGANIC-CARBON;REACTIVE IRON;PO VALLEY;SULFIDE;BEARING
Date:	2004
Issue Date:	2010-07-08 09:31:48 (UTC+8)
Publisher:	中央大學
Abstract:	The importance of the magnetic iron sulfide minerals, greigite (Fe3S4) and pyrrhotite (Fe7S8), is often underappreciated in geochemical studies because they are metastable with respect to pyrite (FeS2). Based on magnetic properties and X-ray diffraction a
Relation:	CHEMICAL GEOLOGY
Appears in Collections:	[Graduate Institute of Hydrological and Oceanic Sciences] journal & Dissertation

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