Regional retrograde alteration of sub-greenschist facies chlorite to smectite
dc.contributor.author | Huertas, Miguel Ortega | en_US |
dc.contributor.author | Nieto, Fernando | en_US |
dc.contributor.author | Velilla, Nicolás | en_US |
dc.contributor.author | Peacor, Donald R. | en_US |
dc.date.accessioned | 2006-09-11T18:49:40Z | |
dc.date.available | 2006-09-11T18:49:40Z | |
dc.date.issued | 1994-01 | en_US |
dc.identifier.citation | Nieto, Fernando; Velilla, Nicolás; Peacor, Donald R.; Huertas, Miguel Ortega; (1994). "Regional retrograde alteration of sub-greenschist facies chlorite to smectite." Contributions to Mineralogy and Petrology 115(3): 243-252. <http://hdl.handle.net/2027.42/47308> | en_US |
dc.identifier.issn | 1432-0967 | en_US |
dc.identifier.issn | 0010-7999 | en_US |
dc.identifier.uri | https://hdl.handle.net/2027.42/47308 | |
dc.description.abstract | Dioctahedral smectite is present as a retrograde alteration product of chlorite in Permian-Triassic red slates of the Malaguide Complex in Sierra de Espuña (Betic Cordillera). Mineral assemblages and textures, illite “crystallinity” indices, and fluid inclusion data indicate sub-greenschist facies conditions that reached at least 180°C in the higher-grade tectonic unit of the Malaguide Complex, preceding formation of smectite. Smectite, having K as the dominant interlayer cation, occurs ubiquitously intercalated with trioctahedral chlorite as thin packets of layers and as individual layers that commonly change to chlorite along layers. Although some chlorite is typically homogeneous and trioctahedral, much chlorite shows signs of alteration and has compositions corresponding to different degrees of smectite contaimination. The incompatibility of metamorphic grade with the occurrence of smectite, the general association of chlorite and smectite, and the textural relations collectively show that dioctahedral smectite is derived through replacement of trioctahedral chlorite. Such replacement occurs on a regional basis and demonstrates that caution must be used in interpreting the occurrence of smectite in pelites as being due to prograde processes. Alteration of trioctahedral chlorite under oxidizing conditions due to introduction of phreatic water after uplift of the Betic Cordillera is proposed as the cause of formation of smectite. | en_US |
dc.format.extent | 2469681 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 | Geology | en_US |
dc.subject.other | Geosciences | en_US |
dc.subject.other | Mineral Resources | en_US |
dc.subject.other | Mineralogy | en_US |
dc.title | Regional retrograde alteration of sub-greenschist facies chlorite to smectite | 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, MI, USA | en_US |
dc.contributor.affiliationother | Dpto Mineralogia y Petrología, Universidad de Granada-C.S.I.C., 18002, Granada, Spain; I.A.G.M., Universidad de Granada-C.S.I.C., 18002, Granada, Spain | en_US |
dc.contributor.affiliationother | Dpto Mineralogia y Petrología, Universidad de Granada-C.S.I.C., 18002, Granada, Spain; I.A.G.M., Universidad de Granada-C.S.I.C., 18002, Granada, Spain | en_US |
dc.contributor.affiliationother | Dpto Mineralogia y Petrología, Universidad de Granada-C.S.I.C., 18002, Granada, Spain; I.A.G.M., Universidad de Granada-C.S.I.C., 18002, Granada, Spain | en_US |
dc.contributor.affiliationumcampus | Ann Arbor | en_US |
dc.description.bitstreamurl | http://deepblue.lib.umich.edu/bitstream/2027.42/47308/1/410_2004_Article_BF00310765.pdf | en_US |
dc.identifier.doi | http://dx.doi.org/10.1007/BF00310765 | en_US |
dc.identifier.source | Contributions to Mineralogy and Petrology | en_US |
dc.owningcollname | Interdisciplinary and Peer-Reviewed |
Files in this item
Remediation of Harmful Language
The University of Michigan Library aims to describe library materials in a way that respects the people and communities who create, use, and are represented in our collections. Report harmful or offensive language in catalog records, finding aids, or elsewhere in our collections anonymously through our metadata feedback form. More information at Remediation of Harmful Language.
Accessibility
If you are unable to use this file in its current format, please select the Contact Us link and we can modify it to make it more accessible to you.