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  • 1
    ISSN: 1525-1314
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Sapphirine occurs in a 3-5 m wide zone between amphibole-lherzolite and garnetiferous metagabbro at Finero in the Ivrea Zone, NW Italian Alps. Layers consisting of plag + hb + sa + cpx + opx + sp + gt are interbanded with spinel pyroxenites, which may contain sapphirine replacing spinel. All minerals are very magnesian, with XMg between 0.78 and 0.92. Bulk rock analyses suggest that precursors to the sapphirine-bearing rocks were igneous cumulates of plagioclase + olivine + hornblende + spinel. Up to 16wt% CaO does not inhibit sapphirine formation and it is the unusually Mg-rich nature of the host rocks which allows sapphirine development. The early igneous assemblage was replaced by one of cpx + sa + hb +± plag at a pressure of 9 ± 1 kbar and temperatures of 900 ± 50°C. Subsequent rapid uplift caused the instability of gt, gt + hb, hb and sa + cpx to form opx + plag ± sp ± sa symplectites.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-05-12
    Keywords: Abbott Seamount; Colahan Seamount; Daikakuji Seamount; De Veuster Seamount; Dredge; DRG; East Daikakuji Seamount; Elevation of event; Event label; Halsley Seamount; Hancock Seamount; HULA I; Kure Seamount; Ladd Seamount; Latitude of event; Longitude of event; Method/Device of event; Midway Seamount; Nero Seamount; North Kammu Seamount; Pearl and Hermes Seamount; Salmon Seamount; Seamount 63; Seamounts 72-74; SO141; SO141_04DR; SO141_05DR; SO141_06DR; SO141_07DR; SO141_08DR; SO141_09DR; SO141_10DR; SO141_11DR; SO141_12DR; SO141_13DR; SO141_14DR; SO141_15DR; SO141_16DR; SO141_17DR; SO141_18DR; SO141_19DR; SO141_20DR; SO141_21DR; SO141_22DR; SO141_23DR; SO141_24DR; SO141_25DR; SO141_26DR; SO141_27DR; SO141_28DR; SO141_29DR; SO141_30DR; SO141_31DR; SO141_32DR; SO141_33DR; SO141_34DR; SO141_35DR; SO141_36DR; SO141_37DR; SO141_38DR; Sonne; South Kammu Seamount; Townsend Cromwell Seamount; Uniform resource locator/link to file; Yuryaku Seamount
    Type: Dataset
    Format: text/tab-separated-values, 35 data points
    Location Call Number Limitation Availability
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  • 3
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    PANGAEA
    In:  Geologisch-Paläontologisches Institut, Christian-Albrechts-Universität, Kiel
    Publication Date: 2023-05-12
    Keywords: Copper; Date/Time of event; DEPTH, sediment/rock; Dredge, chain bag; DRG_C; Electron microprobe (EMP); Elevation of event; Event label; FOUNDATION HOT SPOT; Iron; Latitude of event; Longitude of event; Manganese; Nickel; Replicate; Sample code/label; Sample type; SO157; SO157_05DS; SO157_48DS; SO157_65DS; Sonne; Sulfur, total; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 51 data points
    Location Call Number Limitation Availability
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  • 4
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    Unknown
    PANGAEA
    In:  Supplement to: Devey, Colin W; Ackermand, Dietrich; Binard, Nicolas; Chmarzynski, P; Franke-Bruckmaier, B; Geldmacher, Jörg; Graupner, T; Haake, F W; Haase, Karsten M; Hemond, Christophe; Krüger, O; Mühlhan, Norbert; O'Connor, John; Ott, S; Peucker-Ehrenbrink, Bernhard; Pototzki, Frank; Segl, Monika; Tichomirov, W (1993): Cruise report SO-84: The St Helena hotspot - Las Palmas-Cape Town 02.01.93-20.02.93. Berichte - Reports, Geologisch-Paläontologisches Institut und Museum, Christian-Albrechts-Universität, Kiel; 64; 1-103; ISSN 0175-9302, TIB - Technische Informationsbibliothek Universitätsbibliothek Hannover, Berichte-Reports, Geologisch-Paläontologisches Institut der Universität Kiel, 64, 103 pp, https://doi.org/10.2312/reports-gpi.1993.64
    Publication Date: 2024-02-03
    Description: The SO-84 cruise from Las Palmas to Cape Town studied the underwater volcanism associated with the St Helena hotspot. Wide-spaced grid mapping of a region south and west of St Helena island identified three previously unknown hotspot volcanoes (which we named Josephine 16°27'S-9°W, Jade 16°13'S-7°46'W and Benjamin 16°12'S-8°31'W) and several older, probably near-ridge-generated seamounts. The newly discovered hotspot seamounts, and the previously-known seamounts of Bagration, Bonaparte and Kutuzov were mapped and sampled. Onboard geochemical studies confirm that they all show trace-element (Rb, Nb, Y, Zr, Sr) enriched, hotspot magma-type compositions. Morphological studies and the state of the samples collected from the seamounts (all have at least 1 mm-thick Mn crusts) suggest that none of the volcanoes is presently active, and that the St Helena hotspot is probably extinct at the present time. Josephine appears to be the youngest volcano, and one dredge here yielded fossil hydrothermal material (Fe-hydroxides). To test the hypothesis that the extinction of the hotspot is due to its magmas being channelled to the Mid-Atlantic Ridge, several dredges were taken on the ridge opposite St Helena. Furthermore, in the proposed influence zone of the St Helena plume head, Grattan seamount (9°44'S-12°48'W) was also sampled to examine whether its composition has been affected by the St Helena plume. During the transit from Las Palmas to St Helena, several sediment cores were taken in 3000 m water depth close to the ridge axis for palaeoclimatological work.
    Keywords: 12DS; 13DS; 14DS; 1DS; 20DS; 21DS; 22DS; 23DS; 24DS; 25DS; 26DS; 27DS; 31DS; 35DS; 37DS; 42DS; 43DS; 44DS; 47DS; 49DS; 53DS; 54DS; 55DS; 59DS; 60DS; 63DS; 64DS; 65DS; 68DS; 69DS; 71DS; 72DS; 74DS; 7DS; 83DS; Comment; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Event label; GIK/IfG; GIK17835-1; GIK17841-1; GIK17846-1; GIK17847-1; GIK17848-1; GIK17854-1; GIK17855-1; GIK17856-1; GIK17857-1; GIK17858-1; GIK17859-1; GIK17860-1; GIK17861-1; GIK17865-1; GIK17869-1; GIK17871-1; GIK17876-1; GIK17877-1; GIK17878-1; GIK17881-1; GIK17883-1; GIK17887-1; GIK17888-1; GIK17889-1; GIK17893-1; GIK17894-1; GIK17897-1; GIK17898-1; GIK17899-1; GIK17902-1; GIK17903-1; GIK17905-1; GIK17906-1; GIK17908-1; GIK17917-1; Identification; Institute for Geosciences, Christian Albrechts University, Kiel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Size; SO84; Sonne; South Atlantic; ST. HELENA HOTSPOT; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 725 data points
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2024-03-25
    Description: The Red Sea is a very young ocean, and is one of the most interesting areas on Earth (ocean in statu nascendi). It is the only ocean where hydrothermal activity associated with ore formation occurs in a sterile environment (anoxic, hot, saline). In addition, its geographical position means that it is predestined to record the monsoonal history of the region in detailed sedimentary sequences. The major aim of the present project is to investigate the dynamics of hydrothermal systems in selected Deeps (Atlantis-II, Discovery, Kebrit, Al Wajh), Additional palaeoceanographic and microbiological questions should also be addressed. Specific aims are: 1. To study the hydrographic changes in individual Deeps (hydrothermal region Atlantis-II) and to investigate the causes of the temperature increase in the last few years (increased heat flow - higher temperature of the brine supply - higher brine flow rates?). 2.a. To document the influence of the hydrothermal systems on the sedimentary organic matter in the Deeps. In particular, the thermogenic production and migration of hydrocarbons in the sediments will be studied. The complex formation mechanisms (bacterial, thermogenic) of short-chain hydrocarbons (trace gases) will also be examined, 2.b. in addition, the polar and macromolecular fraction in samples from the various deeps will be studied in order to elucidate the formation, structure and source of the macromolecular oil fraction. 3. To clarify the palaeoceanographic conditions, sea-level changes and the climatic history (relationship of the circulation system and nutrient supply to the monsoon) of the southern Red Sea. 4. To separate microorganisms from the brines and to characterise them in terms of their metabolic physiology and ecology, and to describe their taxonomy.
    Keywords: Al-Wajh Deep; Atlantis II Deep; Chain Deep; CTD/Rosette; CTD-RO; Discovery Deep; Dredge; DRG; GIK/IfG; GIK17016-1; GIK17017-1; GIK17017-2; GIK17017-3; GIK17017-4; GIK17017-5; GIK17017-6; GIK17017-7; GIK17017-8; GIK17020-1; GIK17021-1; GIK17021-2; GIK17022-2; GIK17023-1; GIK17023-2; GIK17023-3; GIK17023-4; GIK17023-5; GIK17023-6; GIK17023-7; GIK17024-1; GIK17025-1; GIK17026-1; GIK17026-2; GIK17026-3; GIK17026-4; GIK17026-5; GIK17026-6; GIK17026-8; GIK17027-1; GIK17027-2; GIK17028-1; GIK17029-1; GIK17029-2; GIK17029-3; GIK17029-4; GIK17029-5; GIK17029-6; GIK17029-7; GIK17032-1; GIK17034-1; GIK17034-2; GIK17034-3; GIK17036-1; GIK17036-2; GIK17036-3; GIK17037-2; GIK17037-4; GIK17038-1; GIK17038-10; GIK17038-11; GIK17038-12; GIK17038-13; GIK17038-14; GIK17038-16; GIK17038-2; GIK17038-3; GIK17038-4; GIK17038-5; GIK17038-6; GIK17038-7; GIK17038-8; GIK17038-9; GIK17039-1; GIK17039-2; GIK17039-3; GIK17040-2; GIK17041-2; GIK17042-2; Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; Kebrit Deep; MUC; MultiCorer; North Al-Wajh Deeps; Red Sea; ROTES MEER; SO121; SO121_1; SO121_10; SO121_11; SO121_12; SO121_13; SO121_14; SO121_16; SO121_17; SO121_18; SO121_19; SO121_2; SO121_20; SO121_21; SO121_22; SO121_23; SO121_24; SO121_25; SO121_26; SO121_27; SO121_28; SO121_29; SO121_30; SO121_31; SO121_33; SO121_35; SO121_36; SO121_37; SO121_38; SO121_39; SO121_4; SO121_40; SO121_41; SO121_42; SO121_43; SO121_44; SO121_48; SO121_53; SO121_55; SO121_56; SO121_58; SO121_59; SO121_6; SO121_62; SO121_64; SO121_66; SO121_67; SO121_68; SO121_69; SO121_7; SO121_70; SO121_71; SO121_72; SO121_75; SO121_76; SO121_77; SO121_78; SO121_79; SO121_8; SO121_80; SO121_81; SO121_86; SO121_87; SO121_88; SO121_89; SO121_9; SO121_91; SO121_93; SO121_95; SO121_96; SO121-96; Sonne; Umm Lajj Deep
    Type: Dataset
    Format: application/zip, 19 datasets
    Location Call Number Limitation Availability
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