Presencia de mineralogías ricas en Zn como evidencias de la actividad hidrotermal enzonas de cizalla extensionales (Complejo Nevado-Filábride, Béticas)

Soto, Juan I.; Muñoz, Mercedes

Occurrence of Zn-rich assemblages controled by hydrothermal activity in extensional shear zones (Nevado-Filábride Complex, Betics)

dc.contributor.author	Soto, Juan I.
dc.contributor.author	Muñoz, Mercedes
dc.date.accessioned	2017-08-21T09:25:09Z
dc.date.available	2017-08-21T09:25:09Z
dc.date.issued	1993
dc.identifier.uri	http://hdl.handle.net/10272/14056
dc.description.abstract	Late Zn-rich assemblages have been found in several lithilogies of the Bédar-Macael unit and upper part of the Calar-Alto unit (Nevado-Filabride Complex). The nowadays brittle contacts between the nevado-filábride and alpujárride units are low-angle normal faults of an extensional system Middle Miocene in age. In metabasite rocks of the Bédar-Macael unit, Zn-rich staurolite (ZnO<13 wt%) partially transformed to gahnite-haematite+quartz assemblage has been found	es_ES
dc.language.iso	spa	es_ES
dc.publisher	Sociedad Geológica de España	es_ES
dc.rights	Atribución-NoComercial-SinDerivadas 3.0 España	*
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/es/	*
dc.subject.other	Zn-rich staurolite	es_ES
dc.subject.other	Hydrothermal fluids	es_ES
dc.subject.other	Extensional shear zones	es_ES
dc.subject.other	Brittle-ductile transition	es_ES
dc.subject.other	Betics	es_ES
dc.title	Presencia de mineralogías ricas en Zn como evidencias de la actividad hidrotermal enzonas de cizalla extensionales (Complejo Nevado-Filábride, Béticas)	es_ES
dc.title	Occurrence of Zn-rich assemblages controled by hydrothermal activity in extensional shear zones (Nevado-Filábride Complex, Betics)	eng
dc.type	info:eu-repo/semantics/article	es_ES
dc.rights.accessRights	info:eu-repo/semantics/openAccess	es_ES

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Geogaceta -- Nº 14, (1993)

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Presencia de mineralogías ricas en Zn como evidencias de la actividad hidrotermal enzonas de cizalla extensionales (Complejo Nevado-Filábride, Béticas)

Occurrence of Zn-rich assemblages controled by hydrothermal activity in extensional shear zones (Nevado-Filábride Complex, Betics)

dc.contributor.author	Soto, Juan I.
dc.contributor.author	Muñoz, Mercedes
dc.date.accessioned	2017-08-21T09:25:09Z
dc.date.available	2017-08-21T09:25:09Z
dc.date.issued	1993
dc.identifier.uri	http://hdl.handle.net/10272/14056
dc.description.abstract	Late Zn-rich assemblages have been found in several lithilogies of the Bédar-Macael unit and upper part of the Calar-Alto unit (Nevado-Filabride Complex). The nowadays brittle contacts between the nevado-filábride and alpujárride units are low-angle normal faults of an extensional system Middle Miocene in age. In metabasite rocks of the Bédar-Macael unit, Zn-rich staurolite (ZnO<13 wt%) partially transformed to gahnite-haematite+quartz assemblage has been found	es_ES
dc.language.iso	spa	es_ES
dc.publisher	Sociedad Geológica de España	es_ES
dc.rights	Atribución-NoComercial-SinDerivadas 3.0 España	*
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/es/	*
dc.subject.other	Zn-rich staurolite	es_ES
dc.subject.other	Hydrothermal fluids	es_ES
dc.subject.other	Extensional shear zones	es_ES
dc.subject.other	Brittle-ductile transition	es_ES
dc.subject.other	Betics	es_ES
dc.title	Presencia de mineralogías ricas en Zn como evidencias de la actividad hidrotermal enzonas de cizalla extensionales (Complejo Nevado-Filábride, Béticas)	es_ES
dc.title	Occurrence of Zn-rich assemblages controled by hydrothermal activity in extensional shear zones (Nevado-Filábride Complex, Betics)	eng
dc.type	info:eu-repo/semantics/article	es_ES
dc.rights.accessRights	info:eu-repo/semantics/openAccess	es_ES

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Name:: Presencia-de-mineralogias.pdf
Size:: 2.439Mb
Format:: PDF

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