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  • 2010-2014  (120)
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Year
  • 1
    Keywords: Sulfidlagerstätte ; Meereskunde ; Meeresressourcen
    Type of Medium: Book
    Pages: 14 S. , Ill., graph. Darst., Kt.
    Language: English
    Note: Auch als elektron. Dokument erschienen
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  • 2
    Online Resource
    Online Resource
    Kiel
    Keywords: Sulfidlagerstätte ; Meereskunde ; Meeresressourcen
    Type of Medium: Online Resource
    Pages: Online-Ressource (pdf-Datei: 14 S., xyz MB) , Ill., graph. Darst., Kt.
    Language: English
    Note: Auch als gedrucktes Dokument erschienen
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  • 3
    Keywords: Hochschulschrift
    Type of Medium: Online Resource
    Pages: Online-Ressource ( PDF-Datei : 16 S., 1 MB) , Ill..
    Series Statement: Kinder- und Schüleruni Kiel : für Schülerinnen und Schüler von 12 bis 16 Jahren 2010.11,03
    Language: German
    Note: Auch als gedr. Dokument vorh
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  • 4
    Keywords: Hochschulschrift
    Type of Medium: Book
    Pages: [16] S. , Ill..
    Series Statement: Kinder- und Schüleruni Kiel : für Schülerinnen und Schüler von 12 bis 16 Jahren 2010.11,03
    Language: German
    Note: Auch als elektronisches Dokument vorh
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  • 5
    Keywords: Sulfidlagerstätte ; Meereskunde ; Meeresressourcen
    Type of Medium: Book
    Pages: 14 S. , Ill., graph. Darst., Kt.
    Language: German
    Note: Auch als elektron. Dokument erschienen
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  • 6
    Online Resource
    Online Resource
    Kiel
    Keywords: Sulfidlagerstätte ; Meereskunde ; Meeresressourcen
    Type of Medium: Online Resource
    Pages: Online-Ressource (pdf-Datei: 14 S., 3,5 MB) , Ill., graph. Darst., Kt.
    Language: German
    Note: Auch als gedrucktes Dokument erschienen
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  • 7
    Type of Medium: Online Resource
    Pages: 32 S.; graph. Darst.
    Edition: Online-Ausg. Online-Ressource
    Series Statement: GEOMAR Report N.S. 16
    Language: English , German
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  • 8
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    Unknown
    PANGAEA
    In:  Supplement to: Klevenz, Verena; Bach, Wolfgang; Schmidt, Katja; Hentscher, Michael; Koschinsky, Andrea; Petersen, Sven (2011): Geochemistry of vent fluid particles formed during initial hydrothermal fluid-seawater mixing along the Mid-Atlantic Ridge. Geochemistry, Geophysics, Geosystems, 12, Q0AE05, https://doi.org/10.1029/2011GC003704
    Publication Date: 2024-04-22
    Description: We present geochemical data of black smoker particulates filtered from hydrothermal fluids with seawater-dilutions ranging from 0–99%. Results indicate the dominance of sulphide minerals (Fe, Cu, and Zn sulphides) in all samples taken at different hydrothermal sites on the Mid-Atlantic Ridge. Pronounced differences in the geochemistry of the particles between Logatchev I and 5°S hydrothermal fields could be attributed to differences in fluid chemistry. Lower metal/sulphur ratios (Me/H2S 〈 1) compared to Logatchev I result in a larger amount of particles precipitated per liter fluid and the occurrence of elemental sulphur at 5°S, while at Logatchev I Fe oxides occur in larger amounts. Systematic trends with dilution degree of the fluid include the precipitation of large amounts of Cu sulphides at a low dilution and a pronounced drop with increasing dilution. Moreover, Fe (sulphides or oxides) precipitation increases with dilution of the vent fluid by seawater. Geochemical reaction path modeling of hydrothermal fluid–seawater mixing and conductive cooling indicates that Cu sulphide formation at Logatchev I and 5°S mainly occurs at high temperatures and low dilution of the hydrothermal fluid by seawater. Iron precipitation is enhanced at higher fluid dilution, and the different amounts of minerals forming at 5°S and Logatchev I are thermodynamically controlled. Larger total amounts of minerals and larger amounts of sulphide precipitate during the mixing path when compared to the cooling path. Differences between model and field observations do occur and are attributable to closed system modeling, to kinetic influences and possibly to organic constituents of the hydrothermal fluids not accounted for by the model.
    Keywords: Aluminium; Area/locality; ATA-13ROV; ATA-17ROV; ATA-24ROV; ATA-30ROV; ATA-35ROV; ATA-42ROV; ATA-46ROV; ATA-57ROV; ATA-67ROV; Barium; Cadmium; Caesium; Calcium; Copper; DEPTH, sediment/rock; DERIDGE; Event label; From Mantle to Ocean: Energy-, Material- and Life-cycles at Spreading Axes; HYDROMAR-III; HYDROMAR-V; HYDROMAR-V-13; HYDROMAR-V-17; HYDROMAR-V-24; HYDROMAR-V-30; Hydrothermal fluid; ICP-OES, Inductively coupled plasma - optical emission spectrometry; Inductively coupled plasma - mass spectrometry (ICP-MS); Iron; L Atalante; LAtalante Leg1 (ATA07_12); LAtalante Leg2 (ATA08_01); Lead; M68/1; M68/1-03-ROV; M68/1-12-ROV; M68/1-20-ROV; M78/2; M78/2_281; M78/2_297; M78/2_308; Magnesium; Manganese; Maria S. Merian; MARSUED3; MARSUED5; MARSUED-IV; MARSUED-IV-35; MARSUED-IV-42; MARSUED-IV-46; MARSUED-IV-57; MARSUED-IV-67; Meteor (1986); Mid-Atlantic Ridge at 10-15°N; Mid-Atlantic Ridge at 4-11°S; Molybdenum; MSM04/3; MSM04/3_244-ROV-3; MSM04/3_244-ROV-7; MSM04/3_253-ROV-9; MSM04/3_255ROV-12; MSM04/3_255ROV-17; MSM04/3_255ROV-3; MSM04/3_255ROV-4; MSM04/3_259-ROV-25; MSM04/3_275-ROV-5; MSM04/3_275-ROV-7; MSM10/3; MSM10/3_290ROV-11; MSM10/3_313ROV-12; MSM10/3_315ROV-19; pH; Remote operated vehicle; ROV; Rubidium; Sample code/label; Strontium; Sulfur; Temperature, technical; tropical/subtropical North Atlantic; Tungsten; Uranium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 936 data points
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  • 9
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    Unknown
    Schweizerbart
    In:  Neues Jahrbuch für Mineralogie: Abhandlungen = Journal of Mineralogy and Geochemistry, 190 (3). pp. 327-340.
    Publication Date: 2020-08-07
    Description: In many subaerial hydrothermal ore deposits arsenian pyrite is an important host for Au, however, arsenian pyrite is rare on the modern seafloor. During a recent survey for submarine hydrothermal mineralization in the western Woodlark Basin volcanic breccias containing abundant arsenian pyrite were dredged from the flanks of a volcanic seamount in a water depth of 2000 m. This area is particularly interesting because it is located at the transition from continental splitting to oceanic spreading where enhanced heat flow and deep crustal faults may fertilize mineralization. The sulfidic breccia is essentially monomictic and matrix-supported containing altered dacitic clasts. Mineralogical investigation of the breccia reveals silicification and sulfidation as the main alteration types. Quartz occurs in fragments and also constitutes the breccia matrix attesting to silicification as a significant alteration process. Pyrite is the dominant ore mineral with only minor amounts of Fe-oxyhydroxide and goethite. Bulk geochemistry shows a slight enrichment of Au (0.12 ppm) in association with elements such as As-Ag-Hg-Zn-Pb-Sb, key elements indicative of a low sulfidation environment. Three generations of pyrite are recognized on the basis of morphology. Arsenic-free, early framboidal pyrite (py1) is overgrown by arsenian colloform (py2) or massive pyrite (py3) containing up to 3.93 wt% As. Arsenic speciation in the pyrite is in the form of As1- and As3+. The presence of arsenian pyrite in hydrothermal breccias at this seamount indicates the potential for Au mineralization in the area.
    Type: Article , PeerReviewed
    Format: text
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  • 10
    Publication Date: 2017-06-23
    Description: The western Woodlark Basin lies within a gold-rich metallogenic province. This area is characterized by detachment faults that record ongoing extension and act as major pathways for the circulation of hydrothermal fluids. Dredging from the flanks of a submarine ridge southeast of Cheshire Seamount, western Woodlark Basin retrieved hydrothermally altered monomictic to polymictic crackle, mosaic and chaotic breccias with at least 30% clasts N2 mmin diameter. The precursor rocks are andesitic to rhyolitic in composition, but have been intensely hydrothermally altered, with about 90% of the volcanic glass replaced by secondaryminerals. The breccias show five generations of quartz growth, with the first being related to magmatic processes and the remaining four to alteration stages including silicification, chloritization, illitization, sericitization, albitization, and sulfidation. Needle-like crystals ofmordenite (zeolite)withmultiple growth centers growon the fourth generation of quartz. Notable textural variants in the breccias are vesicles, perlitic cracks, and zoned alteration halos that mantle the rims of clasts. Electron microprobe analyses on chlorite from breccia samples have identified clinochlore as the main chlorite type and indicate a formation temperature in the range of 210–304 °C. This and the elevated Au–As–Ag–Hg–Zn–Pb–Sb contents of a mineralized sample indicate hydrothermal alteration temperatures N200 °C suggesting that these breccias may represent the upflow zone of a hydrothermal system and highlight the potential for seafloor massive sulfides in the area. The breccias show elevated contents of immobile trace elements and LREE as well as a depletion in Ta and Nb suggesting that the precursor rocks were formed in a rift-related suprasubduction environment.
    Type: Article , PeerReviewed
    Format: text
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