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Langban; an exhalative sedimentary deposit?
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1979
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Sedimentary RecordUnited States SearchFacies AnalysisEngineeringDepositional ProcessOther| August 01Sedimentary GeologyEconomic GeologyGeologySediment AnalysisGeochemistrySedimentary PetrologyExhalative Sedimentary DepositSedimentologyEarth ScienceSediment Transport
Other| August 01, 1979 Langban; an exhalative sedimentary deposit? K. Bostroem; K. Bostroem Univ. Miami, Rosenstiel Sch., Miami, Fla., United States Search for other works by this author on: GSW Google Scholar H. Rydell; H. Rydell Search for other works by this author on: GSW Google Scholar O. Joensuu O. Joensuu Search for other works by this author on: GSW Google Scholar Author and Article Information K. Bostroem Univ. Miami, Rosenstiel Sch., Miami, Fla., United States H. Rydell O. Joensuu Publisher: Society of Economic Geologists First Online: 02 Mar 2017 Online ISSN: 1554-0774 Print ISSN: 0361-0128 GeoRef, Copyright 2006, American Geological Institute. Abstract, Copyright, Society of Economic Geologists Economic Geology (1979) 74 (5): 1002–1011. https://doi.org/10.2113/gsecongeo.74.5.1002 Article history First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation K. Bostroem, H. Rydell, O. Joensuu; Langban; an exhalative sedimentary deposit?. Economic Geology 1979;; 74 (5): 1002–1011. doi: https://doi.org/10.2113/gsecongeo.74.5.1002 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyEconomic Geology Search Advanced Search Abstract Chemical, mineralogical, and isotope analyses of hausmannite, braunite, and hematite ores from Laangban, Sweden, show that the precursor of this deposit has several similarities in its mineralogy, chemistry, and oxidation state with many deposits of Devonian and Recent ages, such as some deposits in Kazakhstan, in the Red Sea hot brine depressions, and in the East Pacific Rise. Possibly Rammelsberg, Meggen, Franklin Furnace, and Sterling Hill also belong to this type of deposit, for which an exhalative-sedimentary origin is proposed. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.