{"id":{"repo_id":"salamanca","oai_identifier":"oai:gredos.usal.es:10366/108988"},"canonical_url":"https://search.dev.ndltd.org/etd/salamanca/oai:gredos.usal.es:10366/108988","repository":{"repo_id":"salamanca","name":"Universidad de Salamanca","base_url":"https://gredos.usal.es/oai/request"},"display":{"title":"Las mineralizaciones magmático-hidrotermales de Sn‐W‐(Nb‐Ta) del distrito de Navasfrías (SO de Salamanca)","abstract":"[EN] The most important objectives outlined in the development of this work are: - Define the morphological and structural characteristics of different types of mineralization found in the district of Navasfrías: disseminated in granite and aplite facies boundary in pegmatitic dikes and peribatolíticos intra and intragraníticas quartz veins. - Characterize mineralogical, chemical and isotopic, establishing the paragenetic mineral associations and sequences of each of the types and physicochemical conditions of formation. - To establish this, a model that explains metallogenetic spatial and genetic characteristics of this mineralization in the geological context magmáticohidrotermal system in which they are providing, at a time, scanning guidelines and criteria for future research.","abstract_html":"[EN] The most important objectives outlined in the development of this work are: - Define the morphological and structural characteristics of different types of mineralization found in the district of Navasfrías: disseminated in granite and aplite facies boundary in pegmatitic dikes and peribatolíticos intra and intragraníticas quartz veins. - Characterize mineralogical, chemical and isotopic, establishing the paragenetic mineral associations and sequences of each of the types and physicochemical conditions of formation. - To establish this, a model that explains metallogenetic spatial and genetic characteristics of this mineralization in the geological context magmáticohidrotermal system in which they are providing, at a time, scanning guidelines and criteria for future research.","abstract_has_math":false,"creators":["Llorens González, Teresa"],"institution":null,"degree_name":null,"degree_level":null,"degree_discipline":null,"degree_department":null,"school":null,"contributors":[],"advisors":[],"committee_chairs":[],"committee_members":[],"year":2011,"date_issued":"2011","date_published":"2011","updated_at":"2026-07-27T20:57:03Z","subjects":["Tesis y disertaciones académicas","Universidad de Salamanca (España)","Tesis Doctoral","Academic dissertations","Geología","Geology","Navasfrías (Salamanca, España)","Batolitos","Batholiths","Minerales","Minerals"],"languages":[],"rights":[],"rights_urls":[],"identifier_entries":[{"key":"dc:identifier","label":"Identifier","values":["hdl:10366/108988"],"render_values":[{"text":"hdl:10366/108988","href":null,"code":true}]}]},"links":{"outbound_url":"https://doi.org/10.14201/gredos.108988","outbound_label":"DOI","outbound_source":"dc:identifier.doi"},"metadata_groups":[{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date.issued","label":"Date","values":["2011"]},{"key":"dc:type","label":"Dc Type","values":["info:eu-repo/semantics/doctoralThesis"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["Tesis y disertaciones académicas","Universidad de Salamanca (España)","Tesis Doctoral","Academic dissertations","Geología","Geology","Navasfrías (Salamanca, España)","Batolitos","Batholiths","Minerales","Minerals"]}]},{"id":"identifiers","label":"Identifiers","entries":[{"key":"dc:identifier","label":"Identifier","values":["hdl:10366/108988"]},{"key":"dc:identifier.doi","label":"DOI","values":["10.14201/gredos.108988"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description.other","label":"Dc Description Other","values":["[EN] The most important objectives outlined in the development of this work are: - Define the morphological and structural characteristics of different types of mineralization found in the district of Navasfrías: disseminated in granite and aplite facies boundary in pegmatitic dikes and peribatolíticos intra and intragraníticas quartz veins. - Characterize mineralogical, chemical and isotopic, establishing the paragenetic mineral associations and sequences of each of the types and physicochemical conditions of formation. - To establish this, a model that explains metallogenetic spatial and genetic characteristics of this mineralization in the geological context magmáticohidrotermal system in which they are providing, at a time, scanning guidelines and criteria for future research.","[ES] Los objetivos más importantes planteados en el desarrollo de este trabajo son los siguientes: - Definir las características morfológicas y estructurales de los distintos tipos de mineralización que se encuentran en el distrito de Navasfrías: diseminada en las facies graníticas y aplíticas de borde, en los diques pegmatíticos intra y peribatolíticos y en las venas de cuarzo intragraníticas. - Caracterizarlos mineralógica, química e isotópicamente, estableciendo las asociaciones minerales y secuencias paragenéticas de cada uno de los tipos, así como las condiciones físico-químicas de su formación. - Establecer, con todo ello, un modelo metalogenético que explique espacial y genéticamente las características de estas mineralizaciones en el contexto geológico del sistema magmáticohidrotermal en el que se encuentran facilitando, a la vez, guías y criterios de exploración para futuras investigaciones."]},{"key":"dc:title","label":"Title","values":["Las mineralizaciones magmático-hidrotermales de Sn‐W‐(Nb‐Ta) del distrito de Navasfrías (SO de Salamanca)"]}]}],"canonical_facts":{"dc:date.issued":["2011"],"dc:description.other":["[EN] The most important objectives outlined in the development of this work are: - Define the morphological and structural characteristics of different types of mineralization found in the district of Navasfrías: disseminated in granite and aplite facies boundary in pegmatitic dikes and peribatolíticos intra and intragraníticas quartz veins. - Characterize mineralogical, chemical and isotopic, establishing the paragenetic mineral associations and sequences of each of the types and physicochemical conditions of formation. - To establish this, a model that explains metallogenetic spatial and genetic characteristics of this mineralization in the geological context magmáticohidrotermal system in which they are providing, at a time, scanning guidelines and criteria for future research.","[ES] Los objetivos más importantes planteados en el desarrollo de este trabajo son los siguientes: - Definir las características morfológicas y estructurales de los distintos tipos de mineralización que se encuentran en el distrito de Navasfrías: diseminada en las facies graníticas y aplíticas de borde, en los diques pegmatíticos intra y peribatolíticos y en las venas de cuarzo intragraníticas. - Caracterizarlos mineralógica, química e isotópicamente, estableciendo las asociaciones minerales y secuencias paragenéticas de cada uno de los tipos, así como las condiciones físico-químicas de su formación. - Establecer, con todo ello, un modelo metalogenético que explique espacial y genéticamente las características de estas mineralizaciones en el contexto geológico del sistema magmáticohidrotermal en el que se encuentran facilitando, a la vez, guías y criterios de exploración para futuras investigaciones."],"dc:identifier":["hdl:10366/108988"],"dc:identifier.doi":["10.14201/gredos.108988"],"dc:subject":["Tesis y disertaciones académicas","Universidad de Salamanca (España)","Tesis Doctoral","Academic dissertations","Geología","Geology","Navasfrías (Salamanca, España)","Batolitos","Batholiths","Minerales","Minerals"],"dc:title":["Las mineralizaciones magmático-hidrotermales de Sn‐W‐(Nb‐Ta) del distrito de Navasfrías (SO de Salamanca)"],"dc:type":["info:eu-repo/semantics/doctoralThesis"]},"updated_at":"2026-07-27T20:57:03Z"}