Chlorite-illite/muscovite interlayered and interstratified crystals: A TEM/STEM study
dc.contributor.author | Lewis, Daniel D. | en_US |
dc.contributor.author | Peacor, Donald R. | en_US |
dc.contributor.author | Wintsch, Robert P. | en_US |
dc.contributor.author | Lee, Jung Hoo | en_US |
dc.date.accessioned | 2006-09-11T18:51:52Z | |
dc.date.available | 2006-09-11T18:51:52Z | |
dc.date.issued | 1984-12 | en_US |
dc.identifier.citation | Lee, Jung Hoo; Peacor, Donald R.; Lewis, Daniel D.; Wintsch, Robert P.; (1984). "Chlorite-illite/muscovite interlayered and interstratified crystals: A TEM/STEM study." Contributions to Mineralogy and Petrology 88(4): 372-385. <http://hdl.handle.net/2027.42/47340> | en_US |
dc.identifier.issn | 1432-0967 | en_US |
dc.identifier.issn | 0010-7999 | en_US |
dc.identifier.uri | https://hdl.handle.net/2027.42/47340 | |
dc.description.abstract | Phyllosilicates in rocks which are transitional from mudstone to slate from Lehigh Gap, Pa., have been studied by a variety of techniques, including high resolution Transmission Electron Microscopy and Analytical Electron Microscopy. The principal minerals are “white mica” which is transitional from illite in mudstone to ordered twolayer mica in slate, and chlorite. 7Å berthierine occurs more rarely. Dioctahedral and trioctahedral layers are shown to be interleaved in individual crystals at all scales between the following two end members: (1) both random and regular 1∶1 interlayering at the scale of individual layers, as shown, in part, by lattice fringe images. (2) packets of trioctahedral and dioctahedral layers up to a few thousand Ångstroms or microns in thickness, detectable with ordinary optical techniques. The complete range of intermediate structures is represented in samples which are in transition to slate. Bulk analytical (EMPA), X-ray diffraction or other measurements are shown to result in averages over both kinds of layers when TEM techniques are not used. | en_US |
dc.format.extent | 6261084 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 | Geosciences | en_US |
dc.subject.other | Mineral Resources | en_US |
dc.subject.other | Geology | en_US |
dc.subject.other | Mineralogy | en_US |
dc.title | Chlorite-illite/muscovite interlayered and interstratified crystals: A TEM/STEM study | 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.affiliationother | Department of Geology, Indiana University, 47405, Bloomington, Indiana, USA | en_US |
dc.contributor.affiliationother | Department of Geology, Indiana University, 47405, Bloomington, Indiana, USA; Exon Company USA, P.O. Box 120, 80201, Denver, Colorado, USA | en_US |
dc.contributor.affiliationumcampus | Ann Arbor | en_US |
dc.description.bitstreamurl | http://deepblue.lib.umich.edu/bitstream/2027.42/47340/1/410_2004_Article_BF00376762.pdf | en_US |
dc.identifier.doi | http://dx.doi.org/10.1007/BF00376762 | en_US |
dc.identifier.source | Contributions to Mineralogy and Petrology | en_US |
dc.owningcollname | Interdisciplinary and Peer-Reviewed |
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