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  • AND-2A; ANDRILL; Antarctic Geological Drilling; Core; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Difference weighting of wet and dry sediment mass; DRILL; Drilling/drill rig; McMurdo Sound; McMurdo Station; SMS; Southern McMurdo Sound; Type; Water content, wet mass  (1)
  • Alkalinity, total; AND-2A; Bromide; Chloride; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; Lithium; Magnesium; McMurdo Sound; McMurdo Station; pH; Potassium; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; Salinity; SMS; Sodium; Southern McMurdo Sound; SPP1158; Sulfate  (1)
  • Geothermalfelder  (1)
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  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Panter, Kurt S; Talarico, Franco M; Bassett, K; Del Carlo, Paola; Field, B; Frank, T; Hoffmann, Stefan; Kuhn, Gerhard; Reichelt, Lucia; Sandroni, Sonja; Taviani, Marco; Bracciali, Laura; Cornamusini, G; von Eynatten, Hilmar; Rocchi, Sergio; SMS Science Team (2009): Petrologic and geochemical composition of the AND-2A Core, ANDRILL Southern McMurdo Sound Project, Antarctica. Terra Antartica, 15(1), 147-192, hdl:10013/epic.36329.d001
    Publication Date: 2024-01-20
    Description: The compositional record of the AND-2A drillcore is examined using petrological, sedimentological, volcanological and geochemical analysis of clasts, sediments and pore waters. Preliminary investigations of basement clasts (granitoids and metasediments) indicate both local and distal sources corresponding to variable ice-volume and ice-flow directions. Low abundance of sedimentary clasts (e.g., arkose, litharenite) suggests reduced contributions from sedimentary covers while intraclasts (e.g., diamictite, conglomerate) attest to intrabasinal reworking. Volcanic material includes pyroclasts (e.g., pumice, scoria), sediments and lava. Primary and reworked tephra layers occur within the Early Miocene interval (1093 to 640 metres below sea floor mbsf). The compositions of volcanic clasts reveal a diversity of alkaline types derived from the McMurdo Volcanic Group. Finer-grained sediments (e.g., sandstone, siltstone) show increases in biogenic silica and volcanic glass from 230 to 780 mbsf and higher proportions of terrigenous material c. 350 to 750 mbsf and below 970 mbsf. Basement clast assemblages suggest a dominant provenance from the Skelton Glacier - Darwin Glacier area and from the Ferrar Glacier - Koettlitz Glacier area. Provenance of sand grains is consistent with clast sources. Thirteen Geochemical Units are established based on compositional trends derived from continuous XRF scanning. High values of Fe and Ti indicate terrigenous and volcanic sources, whereas high Ca values signify either biogenic or diagenic sources. Highly alkaline and saline pore waters were produced by chemical exchange with glass at moderately elevated temperatures.
    Keywords: Alkalinity, total; AND-2A; Bromide; Chloride; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; Lithium; Magnesium; McMurdo Sound; McMurdo Station; pH; Potassium; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; Salinity; SMS; Sodium; Southern McMurdo Sound; SPP1158; Sulfate
    Type: Dataset
    Format: text/tab-separated-values, 234 data points
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  • 2
    Publication Date: 2024-01-20
    Keywords: AND-2A; ANDRILL; Antarctic Geological Drilling; Core; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Difference weighting of wet and dry sediment mass; DRILL; Drilling/drill rig; McMurdo Sound; McMurdo Station; SMS; Southern McMurdo Sound; Type; Water content, wet mass
    Type: Dataset
    Format: text/tab-separated-values, 5050 data points
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  • 3
    Publication Date: 2021-03-29
    Description: Zur Nutzung von Erdwärme aus Teufen zwischen 2–5 km werden häufig Systeme aus einer Injektions- und Förderbohrung (‚Dubletten-System‘) genutzt. Dabei wird durch die Injektionsbohrung ein Fluid in den Untergrund verpresst, welches sich erhitzt und durch die Förderbohrung wieder an die Oberfläche gelangt. Ein wesentlicher Parameter für die produktive Nutzung von solchen Dubletten-Systemen ist eine hohe Permeabilität der Gesteine im Untergrund. Häufig werden in solchen geothermischen Reservoiren die Wegsamkeiten für Fluide von Brüchen kontrolliert, die bereits vorhanden sind oder künstlich erzeugt werden müssen (hydraulische Stimulation). Deshalb ist die Kenntnis über existierende Bruchgeometrien sowie Vernetzung der Bruchsysteme von fundamentaler Notwendigkeit zur Abschätzung der Permeabilität von geothermischen Reservoiren. Seismische Verfahren und Bohrkernanalysen besitzen im Allgemeinen dafür eine zu geringe Auflösung. Daher bieten sich dreidimensionale Rekonstruktionen des Bruchsystems aus analogen Obertageaufschlüssen an (vgl. Philipp et al. 2005; 2006)...
    Description: conference
    Keywords: 551 ; VDH 110 ; VAE 150 ; TOO 000 ; VRG 000 ; Untere Trias ; Strukturelle Erscheinungen {Strukturgeologie} ; Geothermik {Geophysik} ; Geothermalfelder ; Karlshafen 〈Region〉 ; Reinhausen 〈Gleichen, Göttingen, Region〉 ; Mittlerer Buntsandstein ; Strukturgeologie ; Permeabiblität ; Geothermische Energie
    Language: German
    Type: anthologyArticle , publishedVersion
    Format: application/pdf
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