Phlogopite-chlorite reaction mechanisms and physical conditions during retrograde reactions in the Marble Formation, Franklin, New Jersey
dc.contributor.author | Peacor, Donald R. | en_US |
dc.contributor.author | Yau, Yu -Chyi | en_US |
dc.contributor.author | Anovitz, Lawrence M. | en_US |
dc.contributor.author | Essene, Eric J. | en_US |
dc.date.accessioned | 2006-09-11T18:51:47Z | |
dc.date.available | 2006-09-11T18:51:47Z | |
dc.date.issued | 1984-12 | en_US |
dc.identifier.citation | Yau, Yu -Chyi; Anovitz, Lawrence M.; Essene, Eric J.; Peacor, Donald R.; (1984). "Phlogopite-chlorite reaction mechanisms and physical conditions during retrograde reactions in the Marble Formation, Franklin, New Jersey." Contributions to Mineralogy and Petrology 88(3): 299-306. <http://hdl.handle.net/2027.42/47339> | en_US |
dc.identifier.issn | 1432-0967 | en_US |
dc.identifier.issn | 0010-7999 | en_US |
dc.identifier.uri | https://hdl.handle.net/2027.42/47339 | |
dc.description.abstract | A retrograde assemblage in a specimen from the Franklin Marble Formation containing an unusual occurrence of three micas has been studied. Microprobe analyses of the margarite, muscovite and phlogopite reveal significant sodium and fluorine but otherwise show little mutual solid solution. The conditions that prevailed during the retrogression estimated from phase equilibria are T =370–450° C and =0.03–0.3 at an assumed pressure of 2 kb. | en_US |
dc.format.extent | 2266725 bytes | |
dc.format.extent | 3115 bytes | |
dc.format.mimetype | application/pdf | |
dc.format.mimetype | text/plain | |
dc.language.iso | en_US | |
dc.publisher | Springer-Verlag | en_US |
dc.subject.other | Mineralogy | en_US |
dc.subject.other | Geosciences | en_US |
dc.subject.other | Mineral Resources | en_US |
dc.subject.other | Geology | en_US |
dc.title | Phlogopite-chlorite reaction mechanisms and physical conditions during retrograde reactions in the Marble Formation, Franklin, New Jersey | en_US |
dc.type | Article | en_US |
dc.subject.hlbsecondlevel | Geology and Earth Sciences | en_US |
dc.subject.hlbsecondlevel | Chemistry | en_US |
dc.subject.hlbtoplevel | Science | en_US |
dc.description.peerreviewed | Peer Reviewed | en_US |
dc.contributor.affiliationum | Department of Geological Sciences, The University of Michigan, 48109, Ann Arbor, Michigan, USA | en_US |
dc.contributor.affiliationum | Department of Geological Sciences, The University of Michigan, 48109, Ann Arbor, Michigan, USA | en_US |
dc.contributor.affiliationum | Department of Geological Sciences, The University of Michigan, 48109, Ann Arbor, Michigan, USA | en_US |
dc.contributor.affiliationum | Department of Geological Sciences, The University of Michigan, 48109, Ann Arbor, Michigan, USA | en_US |
dc.contributor.affiliationumcampus | Ann Arbor | en_US |
dc.description.bitstreamurl | http://deepblue.lib.umich.edu/bitstream/2027.42/47339/1/410_2004_Article_BF00380175.pdf | en_US |
dc.identifier.doi | http://dx.doi.org/10.1007/BF00380175 | en_US |
dc.identifier.source | Contributions to Mineralogy and Petrology | en_US |
dc.owningcollname | Interdisciplinary and Peer-Reviewed |
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