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GeoForschungsZentrum GFZ","grobid_abstract":"Das Sn-Lagerstättensystem Ehrenfriedersdorf ist an den in 140-200 m Tiefe untertägig aufgeschlossenen varistischen Granitstock des Saubergs gebunden. Die posttektonische nicht-foliierte Granitintrusion mit hohem lntrusionsniveau bei rund 2.000 m stellt einen Apikalbereich (\"Granitrücken\") des \"Mittelerzgebirgischen Teilplutons\" dar, der nach Ergebnissen von Gravimetrie und zahlreichen Explorationsbohrungen weiträumig das Gebiet E'dorf-Annaberg unterlagert. Die mehrphasige Sauberg-Subintrusion besteht aus hochfraktioniertem Alkalifeldspat Protolithionit-Granit mit starker spät-bis postmagmatischer Hochtemperatur Überprägung und charakteristischer F-Metasomatose. Im Endo-Kontaktbereich zu kambrischen Glimmergneisen treten stark wechselkörnige Randpegmatite mit aplitischen Bereichen auf (\"Stockscheider\"), im Exokontakt besteht ein nach dem Gefügebild fliessender Übergang von hydrothermal überprägten, mehrphasigen leukokraten Aplitgängen zu Sn-(W)-mineralisierten Quarzgängen. Schmelzeinschlüsse in Quarzen aus dem Stockscheider und Aplit-/Quarzgängen haben deutlich höhere Äquivalent-Wassergehalte als der experimentellen H 2 O Löslichkeit in einem haplogranitischen Niedrigdruck-System entsprechen und zeigen Solidus-Temperaturen bis \u003c 600°C. Vorläufige E-Mikrosondenanalysen belegen erhöhte Gehalte von F und P im %-Bereich. Die Viskosität der Schmelzen kann auf Werte von bis zu \u003c 1 o 2 Pa•s (bei 800°C) abgeschätzt werden und ist damit um Grössenordnungen niedriger als für normal-granitische Schmelze. Die untersuchten Granitproben haben peralumine Zusammensetzung und gehören zur Ilmenit-Serie (magnetische Suszeptibilitäten =50, 1 x 1 o-3 SI-Einheiten). Es handelt sich durchwegs um hochfraktionierte leukokrate low Ca Granite, wobei die lntrusionssequenz systematische Entwicklungstrends für Ta, Sn, W, F, Cs, U (Anreicherung), sowie Ti, Mg, Ca, Zr, Zr/Hf, }:SEE (Abreicherung) aufweist, und die Aplitgänge den höchsten Fraktionierungsgrad zeigen. Für die hydrothermal am geringsten mobilen Elementpaare lässt sich dabei fraktionierte Kristallisation als dominanter petrogenetischer Prozess definieren, während Streumuster für die meisten Elemente eine Überprägung im spät-oder postmagmatischen Bereich anzeigen. Insbesondere zeigt die ausgeprägte SEE-lnternfraktionierung (Tetraden Effekt) die Überprägung durch eine Komplexbildner-reiche Fluidphase bei hoher Temperatur. Dem hohen Fraktionierungsgrad entspricht auch die chemische Zusammensetzung der Glimmer-Komponente (Protolithionit), mit im Vergleich zur Erzgebirgs Granitsuite extrem niedrigen Ti-und Mg-Gehalten im 1000 bzw. 100 ppm-Bereich. Das Verteilungsmuster von o 18 O-und 6D-Werten von Protolithionit und kogenetischem Quarz macht für den Stockscheider eine primär-magmatische Fluidentwicklung ohne externen Beitrag wahrscheinlich. Die _konsistenten fN d-Werte von Stockscheider-Mineralen mit-17.6 ±0.6 (300 Ma) definieren ein paläoproterozoisches Edukt-Material (To M =","publication_date":"1995,,","grobid_abstract_attachment_id":"116060133"},"document_type":"paper","pre_hit_view_count_baseline":null,"quality":"low","language":"de","title":"Der Übergangsbereich Pegmatit-/Aplit-in Hydrothermal-Systeme am Beispiel Ehrenfriedersdorf/Erzgebirge","broadcastable":false,"draft":null,"has_indexable_attachment":true,"indexable":true}}["work"]; window.loswp.workCoauthors = [23017749]; window.loswp.locale = "en"; window.loswp.countryCode = "SG"; window.loswp.cwvAbTestBucket = ""; window.loswp.designVariant = "ds_vanilla"; window.loswp.fullPageMobileSutdModalVariant = "control"; window.loswp.useOptimizedScribd4genScript = false; window.loswp.appleClientId = 'edu.academia.applesignon';</script><script defer="" src="https://accounts.google.com/gsi/client"></script><div class="ds-loswp-container"><div 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In: Archäologische Untersuchungen zum Übergang von der Bronze- zur Eisenzeit zwischen Nordsee und Kaukasus. Regensburger Beiträge zur prähistorischen Archäologie 1 (1994) 165-186.</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="26456549" href="https://uni-jena.academia.edu/PeterEttel">Peter Ettel</a></div><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Zum Übergang von der späten Urnenfelder- zur älteren Hallstattzeit in Oberfranken. In: Archäologische Untersuchungen zum Übergang von der Bronze- zur Eisenzeit zwischen Nordsee und Kaukasus. Regensburger Beiträge zur prähistorischen Archäologie 1 (1994) 165-186.","attachmentId":38443741,"attachmentType":"pdf","work_url":"https://www.academia.edu/14846796/Zum_%C3%9Cbergang_von_der_sp%C3%A4ten_Urnenfelder_zur_%C3%A4lteren_Hallstattzeit_in_Oberfranken_In_Arch%C3%A4ologische_Untersuchungen_zum_%C3%9Cbergang_von_der_Bronze_zur_Eisenzeit_zwischen_Nordsee_und_Kaukasus_Regensburger_Beitr%C3%A4ge_zur_pr%C3%A4historischen_Arch%C3%A4ologie_1_1994_165_186","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/14846796/Zum_%C3%9Cbergang_von_der_sp%C3%A4ten_Urnenfelder_zur_%C3%A4lteren_Hallstattzeit_in_Oberfranken_In_Arch%C3%A4ologische_Untersuchungen_zum_%C3%9Cbergang_von_der_Bronze_zur_Eisenzeit_zwischen_Nordsee_und_Kaukasus_Regensburger_Beitr%C3%A4ge_zur_pr%C3%A4historischen_Arch%C3%A4ologie_1_1994_165_186"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="6" data-entity-id="81635246" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/81635246/Pal%C3%A4ofluide_in_st%C3%B6rungskontrollierten_Bruchsystemen_der_Aachener_Geothermie_Bohrung">Paläofluide in störungskontrollierten Bruchsystemen der Aachener Geothermie-Bohrung</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="37293746" href="https://independent.academia.edu/FranzMichaelMeyer">Franz Michael Meyer</a></div><p class="ds-related-work--metadata ds2-5-body-xs">2006</p><p class="ds-related-work--abstract ds2-5-body-sm">Einleitung In der vorliegenden Arbeit werden geologische Prozesse im Untergrund des linksrheinischen Rhenoherzynikums und deren Verhältnis zum regionaltektonischen Rahmen anhand der Proben aus der Aachener GeothermieBohrung mit dem Schwerpunkt des Fluidund Stofftransportes untersucht. Die methodische Vorgehensweise basiert auf einer systematischen und detaillierten Bestandsaufnahme der Paläofluide in Form von Flüssigkeitseinschlüssen an Kernmaterial der Bohrung. Im Aachener Raum wurden Untersuchungen von Flüssigkeitseinschlüssen hauptsächlich an postvariszischen Pb-Zn-Gangvorkommen durchgeführt. Die Homogenisierungstemperaturen (Th) von NaCl-CaCl2-Lösungen unterschiedlicher Salinität liegen zwischen 70°C und maximal 190°C (Redecke 1992, Stroink 1993, Muchez et al. 1994, Glasmacher 1995). Für die tektonischmetallogentische Entwicklung des Rheinischen-Schiefergebirges können generell zwei Fluid-Aktivitätsperioden unterschieden werden (Behr et al. 1993). Die im Zuge der variszischen Ge...</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Paläofluide in störungskontrollierten Bruchsystemen der Aachener Geothermie-Bohrung","attachmentId":87611689,"attachmentType":"pdf","work_url":"https://www.academia.edu/81635246/Pal%C3%A4ofluide_in_st%C3%B6rungskontrollierten_Bruchsystemen_der_Aachener_Geothermie_Bohrung","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/81635246/Pal%C3%A4ofluide_in_st%C3%B6rungskontrollierten_Bruchsystemen_der_Aachener_Geothermie_Bohrung"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="7" data-entity-id="38101132" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/38101132/Dilettantismus_in_der_Hydrologie_%C3%9Cbergangserscheinung_oder_Schicksal_%C3%9Cbersetzung_ins_Deutsche_">Dilettantismus in der Hydrologie: Übergangserscheinung oder Schicksal (Übersetzung ins Deutsche)</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="71493746" href="https://independent.academia.edu/RalfDannowski">Ralf Dannowski</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Vít Klemeš: COMMON SENSE AND OTHER HERESIES – Selected Papers on Hydrology and Water Resources Engineering. Edited by C. D. Sellars, Canadian Water Resources Association, Cambridge, Ontario, Canada, 2000, 1-25. – ISBN 1-896513-18-2, 1986</p><p class="ds-related-work--abstract ds2-5-body-sm">Der unbefriedigende Zustand in der Hydrologie ist aller Erkenntnis nach Ergebnis der Diskrepanz zwischen theoretischer Bestätigung der Hydrologie als Wissenschaft mit eigenem Anspruch und der praktischen Unmöglichkeit, sie als Hauptfach statt immer nur als Anhängsel von Wasserbau, Geographie, Geologie usw. zu studieren. In der Folge neigen die Anschauungen von Hydrologen zu starker Verzerrung in Richtung ihrer nicht-hydrologischen Herkunftsdisziplinen, und ihr hydrologisches Grundwissen weist breite Lücken auf, die eine ansehnliche Vielfalt von Fehlkonzeptionen produzieren. Dieser Zustand paralysiert oft die Fähigkeit von Hydrologen, zwischen Hydrologie und Wasserwirtschaft, Hydrologie und Statistik, Fakten und Annahmen, Wissenschaftlichkeit und Nützlichkeit usw. zu unterscheiden, mit entsprechenden Gefahren sowohl für die wissenschaftliche Entwicklung der Hydrologie wie auch für ihre praktische Brauchbarkeit. Die Gefahr wächst mit der Verbreitung computerbasierter "hydrologischer" Modelle, deren billig hingeschusterte Eignung zur Datenanpassung als Beweis für ihre Vertrauenswürdigkeit ausgegeben wird - und als Rechtfertigung, sie für verführerische, aber hydrologisch unhaltbare Extrapolationen einzusetzen. Diese Punkte werden unter anderem mittels einer Diskussion der Hochwasserhäufigkeitsanalyse illustriert. Der Beitrag schließt mit einigen Überlegungen zu Minimalstandards für den Test hydrologischer Simulationsmodelle, die zumindest ein bescheidenes Niveau an Vertrauenswürdigkeit sichern würden, und mit ein paar Vorschlägen zu den Ingredienzien einer Langzeitkur, die die Hydrologie davor bewahren kann, sich Alchemie und Astrologie in den Annalen des Dilettantismus hinzuzugesellen.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Dilettantismus in der Hydrologie: Übergangserscheinung oder Schicksal (Übersetzung ins Deutsche)","attachmentId":58129898,"attachmentType":"pdf","work_url":"https://www.academia.edu/38101132/Dilettantismus_in_der_Hydrologie_%C3%9Cbergangserscheinung_oder_Schicksal_%C3%9Cbersetzung_ins_Deutsche_","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/38101132/Dilettantismus_in_der_Hydrologie_%C3%9Cbergangserscheinung_oder_Schicksal_%C3%9Cbersetzung_ins_Deutsche_"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="8" data-entity-id="41312606" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/41312606/Klaus_Schmidt_G%C3%B6bekli_Tepe_Untersuchungen_zur_Gewinnung_und_Nutzung_von_Wasser_im_Bereich_des_steinzeitlichen_Bergheiligtums">Klaus Schmidt, Göbekli Tepe – Untersuchungen zur Gewinnung und Nutzung von Wasser im Bereich des steinzeitlichen Bergheiligtums</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="859720" href="https://independent.academia.edu/%C3%87i%C4%9FdemK%C3%B6ksalSchmidt">Çiğdem Köksal-Schmidt</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Wasserwirtschaftliche Innovationen im archäologischen Kontext Von den prähistorischen Anfängen bis zu den Metropolen der Antike, 2012</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Klaus Schmidt, Göbekli Tepe – Untersuchungen zur Gewinnung und Nutzung von Wasser im Bereich des steinzeitlichen 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