Presencia de Cloritoide en las pizarras ordovícicas del sinforme de Alcañices (Zamora)

dc.contributor.authorFernández Fernández, A.
dc.contributor.authorMoro Benito, M. C.
dc.date.accessioned2017-08-21T08:37:51Z
dc.date.available2017-08-21T08:37:51Z
dc.date.issued1993
dc.description.abstractIn the present work we describe for the first time the presence of chloritoid associated with slates of Llanvirn-Llandellian age (Latedo Formation) o f the southern flank of the Alcahices Synform (Zamora). Usually this mineral metamorphic appears in islated prismatic crystals or forming aggregates that are radial, parallel or oblique to the SI and S3 schistosity of the slates. Analysis by electronic microprobe, EDAX and X-ray difraction (XRD) indicates that these chloritoids belong to the ferrous variety, with low MgO contents and without zoning or appreciable differences among the crystals and they mainly correspond to the triclinic polytypees_ES
dc.identifier.urihttp://hdl.handle.net/10272/14055
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherChloritoides_ES
dc.subject.otherLlanvirn-Llandellian slateses_ES
dc.subject.otherAlcahices synformes_ES
dc.subject.otherZamoraes_ES
dc.titlePresencia de Cloritoide en las pizarras ordovícicas del sinforme de Alcañices (Zamora)es_ES
dc.titlePresence ofchloritoid in the ordovician slates of the Alcañices synform (Zamora)eng
dc.typejournal articlees_ES
dspace.entity.typePublication

Files

Original bundle

Now showing 1 - 1 of 1
Loading...
Thumbnail Image
Name:
Presencia-de.pdf
Size:
1.8 MB
Format:
Adobe Portable Document Format