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  • 1
    Publication Date: 2023-06-27
    Keywords: 70-506; 70-506B; 70-506C; 70-507D; 70-507F; 70-509B; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Elevation of event; Event label; Glomar Challenger; Latitude of event; Leg70; Lithology/composition/facies; Longitude of event; North Pacific/MOUND; Sample code/label; Sample ID; see reference(s); Temperature, calculated; δ13C, carbonate; δ18O; δ18O, carbonate; δ Deuterium
    Type: Dataset
    Format: text/tab-separated-values, 109 data points
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  • 2
    Publication Date: 2023-06-27
    Keywords: 70-507A; 70-507F; Aluminium oxide; Antimony; Caesium; Cerium; Chromium; Cobalt; Copper; Deep Sea Drilling Project; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP; Europium; Event label; Glomar Challenger; Iron oxide, Fe2O3; Iron oxide, FeO; Lanthanum; Leg70; Lithium; Lithology/composition/facies; Lutetium; Magnesium oxide; Manganese dioxide; Manganese oxide; Nickel; North Pacific/MOUND; Other event; Phosphorus pentoxide; Potassium oxide; Replicates; Rubidium; Samarium; Scandium; see reference(s); Silicon dioxide; Sodium oxide; Terbium; Titanium dioxide; Ytterbium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 330 data points
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  • 3
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    PANGAEA
    In:  Supplement to: Honnorez, Jose J; von Herzen, Richard P; Barrett, T J; Borella, Peter E; Moorby, S A; Karato, Shun-ichiro; Shipboard Scientific Party (1983): Hydrothermal mounds and young ocean crust of the Galapagos: preliminary Deep Sea Drilling Results. In: Honnorez, J; Von Herzen, RP; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 70, 459-481, https://doi.org/10.2973/dsdp.proc.70.130.1983
    Publication Date: 2023-06-27
    Description: A total of 32 holes at five sites near 1°N, 86°W drilled on Deep Sea Drilling Project (DSDP) Leg 70 (November- December 1979) provide unique data on the origin of the hydrothermal mounds on the southern flank of the Galapagos Spreading Center. Hydrothermal sediments, primarily Mn-oxide and nontronite, are restricted to the immediate vicinity of the mounds (〈 100 m) and are probably formed by the interaction of upward-percolating hydrothermal solutions with seawater and pelagic sediments above locally permeable zones of ocean crust. Mounds as high as 25 meters form in less than a few hundred thousand years, and geothermal and geochemical gradients indicate that they are actively forming today. The lack of alteration of upper basement rocks directly below the mounds and throughout the Galapagos region indicates that the source of the hydrothermal solutions is deeper in the crust.
    Keywords: 70-506; 70-506B; 70-506C; 70-507A; 70-507D; 70-507F; 70-509B; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg70; North Pacific/MOUND
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 4
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    PANGAEA
    In:  Supplement to: Moorby, S A; Cronan, David S (1983): Chemical composition of sediments from Sites 506, 507, 508, and 509, Leg 70, Deep Sea Drilling Project. In: Honnorez, J; Von Herzen, RP; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 70, 269-275, https://doi.org/10.2973/dsdp.proc.70.112.1983
    Publication Date: 2023-06-27
    Description: Since its discovery in 1974 (Klitgord and Mudie, 1974), the Galapagos mounds hydrothermal field has received much attention. Sediment samples were taken during Leg 54 of the Deep Sea Drilling Project (DSDP) and by other expeditions to the area (e.g., Corliss et al., 1978). While a hydrothermal origin for the mounds sediments has been generally accepted, several different theories of origin for the mounds themselves have been proposed (e.g., Corliss et al., 1978; Natland et al., 1979; Williams et al., 1979). One of the aims of DSDP Leg 70 was to return to the mounds field and, using the new hydraulic piston cor er described elsewhere in this volume, to obtain more complete recovery of mounds sediments than had previously been possible. It was our hope that this would help in our understanding of the nature and origin of these deposits. In this chapter, we describe the results of chemical analysis of over 250 sediment samples taken during the course of Leg 70.
    Keywords: 70-506; 70-506C; 70-506D; 70-507D; 70-509B; Coupled plasma emission spectrophotometry; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Glomar Challenger; Iron; Iron 2+; Leg70; North Pacific/MOUND; Ratio; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 70 data points
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  • 5
    Publication Date: 2023-08-28
    Description: A suite of ferromanganese oxide crust specimens was collected by R.R.S. Shackleton in 1975 as part of the continuing study at Imperial College of North West Indian Ocean nodules and encrustations. The samples analysed were drilled out at points of varying depth within the specimens using a hand drill with a 2 mm stainless steel bit. The samples were then ground up and dried in a desiccator. They were subjected to a standard HF/HNO3/HClO4 attack, and taken into solution for analysis by atomic absorption spectrophotometry for Fe, M n, Co, Pb, Cu, Zn, Al, Ti, Mg, Ca, Cd and Li. Analytical precisions were generally better than 10 96, and usually better than 5 %. However, Cd and Li had precisions generally worse than 15 % , because their concentrations were nearer the detection limit of the method.
    Keywords: Aluminium; Atomic absorption spectrophotometry; BC; Box corer; Cadmium; Calcium; Cobalt; Copper; Deposit type; Dredge; DRG; Elevation of event; Event label; GC; Geochemistry; Gravity corer; Identification; Indian Ocean; Iron; Latitude of event; Lead; Lithium; Longitude of event; Magnesium; Manganese; manganese micronodule; manganese nodule; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; ocean; sediment; Shack. 1326D; Shackleton; Shackleton75/5; Shackleton75/5_1317b; Shackleton75/5_1318b; Shackleton75/5_1321a; Shackleton75/5_1323c; Shackleton75/5_1326a; Titanium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 451 data points
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  • 6
    Publication Date: 2023-08-28
    Keywords: Age, dated; Age, dated standard deviation; Alpha spectrometry; Calculated; Depth comment; DISTANCE; Dredge; DRG; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; NZOI-1122; Sample code/label; Sample comment; TANG1122-U23; Tangaroa (1960); Thorium; Thorium, standard deviation; Thorium-230; Thorium-230, standard deviation; Thorium-230/Uranium-232 ratio; Thorium-230/Uranium-232 ratio, standard deviation; Thorium-230/Uranium-234 ratio; Thorium-230/Uranium-234 ratio, standard deviation; Tonga-Kermadec ridge; Uranium; Uranium, standard deviation; Uranium/Thorium ratio; Uranium/Thorium ratio, standard deviation; Uranium-234; Uranium-234, standard deviation; Uranium-234/Uranium-238 activity ratio; Uranium-234/Uranium-238 activity ratio, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 150 data points
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  • 7
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    PANGAEA
    In:  Supplement to: Cronan, David S; Glasby, Geoffrey P; Moorby, S A; Thomson, J; Knedler, K E; McDougall, J C (1982): A submarine hydrothermal manganese deposit from the south-west Pacific island arc. Nature, 298(5873), 456-458, https://doi.org/10.1038/298456a0
    Publication Date: 2023-08-28
    Description: Hydrothermal deposits of a wide variety of types are being found with increasing frequency on or near actively spreading mid-ocean ridges. However, they also have a potential to occur in other submarine volcanic settings, including island arcs. To follow up indications of mineralization associated with submarine hydrothermal activity in the south-west Pacific island arc, a joint New Zealand Oceanographic Institute/Imperial College research cruise was mounted in May 1981 aboard the RV Tangaroa. During this cruise, over 130 sampling stations were occupied, at one of which were dredged manganese deposits with strong hydrothermal affinities. This is the first report of such deposits from an island arc setting.
    Keywords: Dredge; DRG; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; NZOI-1122; TANG1122-U23; Tangaroa (1960); Tonga-Kermadec ridge
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 8
    Publication Date: 2023-08-28
    Keywords: Aluminium; Atomic absorption spectrometry (AAS); Calcium; Cobalt; Copper; DISTANCE; Dredge; DRG; Iron; Manganese; Minerals; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; NZOI-1122; Sample code/label; Sample comment; TANG1122-U23; Tangaroa (1960); Tonga-Kermadec ridge; X-ray diffraction (XRD); Zinc
    Type: Dataset
    Format: text/tab-separated-values, 97 data points
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  • 9
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    PANGAEA
    In:  Supplement to: Cronan, David S; Galacz, A; Mindeszenty, A; Moorby, S A; Polgari, M (1991): Tethyan ferromanganese oxide deposits from Jurassic rocks in Hungary. Journal of the Geological Society, 148(4), 655-668, https://doi.org/10.1144/gsjgs.148.4.0655
    Publication Date: 2024-04-16
    Description: Fossil manganese nodules and encrustations from seamount' and basin' localities in the Transdanubian Central Mountains of Hungary are lithologically, mineralogically and chemically similar to some modern marine ferromanganese oxide deposits, and show no evidence of postdepositional changes other than cementation. Five groups of deposits were encountered: Fe/Mn nodules, encrusted shells, pavements, stains, and Fe oxide encrusted intraclasts, the first three of which are specific to the 'seamount' environment and the last to the basins'. Optical and electron microprobe investigation of the samples shows them to exhibit many similarities with modern ferromanganese oxide deposits, and that many of the nodules are surrounded by a halo of dispersed ferromanganese oxides, strongly suggesting that they continued to accrete metals through the pore waters of unlithified sediments for a period after burial. By contrast, pavements which appear to have grown on hardgrounds at the sea floor show little or no evidence of derivation of metals from underlying sediments. Geochemical investigations on the deposits show the seamount' varieties to be closer in composition to most modern nodules and crusts than the basin' varieties, and that the latter are essentially manganese and trace-element-poor ferruginous deposits. Nevertheless, all can be more or less compositionally equated with modern ferromanganese oxide deposits forming in marginal Atlantic environments, which would be in accord with the proposed depositional environment of the Transdanubian Central Mountains based on other evidence.
    Keywords: Aluminium; Beryllium; Chromium; Cobalt; Copper; CRNHG1; CRNHG2; CRNHG3; Deposit type; DEPTH, sediment/rock; Description; Event label; Geologic age name; HAM; Hammer; Harskut, Hungary; Identification; Inductively coupled plasma atomic emission spectroscope (ICP-AES); Iron; Lanthanum; Lead; Magnesium; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Phosphorus; Potassium; Sediment type; Tardosbanya-Banyahegy, Hungary; Titanium; Tuzkoves Arok, Hungary; Vanadium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 63 data points
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  • 10
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    PANGAEA
    In:  Supplement to: Moorby, S A; Cronan, David S; Glasby, Geoffrey P (1984): Geochemistry of hydrothermal Mn-oxide deposits from the S.W. Pacific island arc. Geochimica et Cosmochimica Acta, 48(3), 433-441, https://doi.org/10.1016/0016-7037(84)90272-2
    Publication Date: 2024-04-16
    Description: Hydrothermal Mn-oxide crusts have been removed from the Tonga-Kermadec Ridge, the first such hydrothermal deposits to be reported in the S.W. Pacific island arc. In several respects the deposits are similar to hydrothermal Mn-crusts from oceanic spreading centre settings. They are limited in areal extent, comprise well-crystalline birnessite and generally display extreme fractionation of Mn from Fe. They are strongly depleted in many elements compared to hydrogenous Mn deposits but are comparatively enriched in Li, Zn, Mo and Cd. The Group IA and Group IIA metals show strong intercorrelations and the behaviour of Mg in the purest samples may indicate the extent to which normal seawater has influenced the composition of the deposits. Certain aspects of the deposits are not typical of hydrothermal Mn deposits. In particular at least some of the crusts have developed on a sediment or unconsolidated talus substrate. Some crusts, or specific layers within some crusts, display a chemical composition which suggests a significant input from normal seawater.
    Keywords: Aluminium; Cadmium; Calcium; Cobalt; Copper; DISTANCE; Dredge; DRG; Event label; Inductively coupled plasma atomic emission spectroscope (ICP-AES); Iron; Latitude of event; Lithium; Longitude of event; Magnesium; Manganese; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; NZOI-1122; Potassium; Sample code/label; Sample comment; Silicon dioxide; Sodium; Strontium; TANG1122-U23; TANG1122-U24; Tangaroa (1960); Titanium; Tonga-Kermadec ridge; Vanadium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 851 data points
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