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  • Data  (27)
  • 1965-1969  (27)
  • 1966  (27)
Collection
Keywords
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  • 1965-1969  (27)
Year
  • 1
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    PANGAEA
    In:  Supplement to: Sigal, Jacques; Truillet, René (1966): Étude micropaléontologique et illustration des filons-couches granoclassés du Capo Sant'Andrea (Sicile). Bulletin de la Societe Geologique de France, 7, 986-993, hdl:10013/epic.46163.d001
    Publication Date: 2023-08-28
    Description: In the region near Taormina, Sicily, the Mesozoic sedimentary veins which contain fillings have various ages ranging from Dogger-Malm until Paleocene-Ypresian. One can observe the development of graded sills parallel to the dip of the banking, formed by the superposition of limestone sequences with Globigerina, Gümbelines and Globotruncana. This study describes and illustrates these graded sills and the embedded fossil manganese nodules they contain.
    Keywords: Aluminium; Calcium; Capo Sant'Andrea, Sicilia; DEPTH, sediment/rock; HAM; Hammer; Iron; Magnesium; Manganese; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Phosphorus; Sample ID; SIGT01; Titanium; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 16 data points
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  • 2
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    PANGAEA
    In:  Supplement to: SCRIPPS Institution of Oceanography (1966): ZETES Expedition, March - August 1966, List of cores and dredge hauls copied from shipboard logs. Scripps Institution of Oceanography, UC San Diego, unpublished, 9 pp, https://www.ngdc.noaa.gov/mgg/curator/data/argo/zetes/zetes_expedition_report.pdf
    Publication Date: 2023-08-28
    Description: The cores and dredges described are taken during the R/V Argo ZETES Expedition from March until August 1966 by the Scripps Institute of Oceanography. A total of 53 cores and dredges were recovered and are available at Scripps Institute of Oceanography for sampling and study.
    Keywords: Argo; Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; DRG; Elevation of event; Event label; GC; Gravity corer; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; Uniform resource locator/link to image; ZETES; ZTES03AR; ZTES03AR-001D; ZTES03AR-002D; ZTES03AR-003D; ZTES04AR; ZTES04AR-005D; ZTES04AR-008D; ZTES05AR; ZTES06AR; ZTES06AR-027G-A; ZTES07AR; ZTES-10G; ZTES-11G; ZTES-12G; ZTES-13G; ZTES-15G; ZTES-16G; ZTES-18G; ZTES-1D; ZTES-21G; ZTES-23G; ZTES-27G-A; ZTES-28G; ZTES-2D; ZTES-31G; ZTES-38G; ZTES-3D; ZTES-5D; ZTES-5G; ZTES-6G; ZTES-8D
    Type: Dataset
    Format: text/tab-separated-values, 292 data points
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  • 3
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    PANGAEA
    In:  Supplement to: Heezen, Bruce C; Glass, Bill; Menard, H William (1966): The Manihiki Plateau. Deep Sea Research and Oceanographic Abstracts, 13(3), 445-458, https://doi.org/10.1016/0011-7471(66)91079-5
    Publication Date: 2023-08-28
    Description: The Manihiki Plateau, a 600,000 km2 smooth and nearly flat-topped feature, lies in the west equatorial Pacific. Danger, Nassau, Suvorov and Manihiki Islands rise from the southern part of the plateau. Oceanic depths of about 5500 m surround the 2400-3000 m summit area. The top of the plateau is capped by approximately one kilometer of sediment. The sediment cores to the east and west of the plateau contain red clay but the top of the plateau is covered with foraminiferal ooze. Mineral grains and rock fragments in cores and dredge hauls from the east escarpment indicate that basic igneous rocks underlie a ridge that forms the eastern edge of the plateau north of 13°S. Bottom photographs and dredge hauls below 3000 m on the east scarp of the plateau and in the abyssal hills to the east reveal abundant manganese nodules. Most of the botton photographs show evidence of deep-sea currents. The plateau's shape is apparently controlled by faulting although much evidence of basic vulcanism is present in the cores. The occurrence of Cretaceous fossils on the eastern ridge of the plateau indicates that the bevelling of the plateau must have occurred during or before Cretaceous time. Twenty cores, two dredge hauls, four bottom trawls and fifteen camera stations from the Vema cruise 18.
    Keywords: CAME; Camera; Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; Dredge, rock; DRG; DRG_R; Elevation of event; Event label; File name; Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Piston corer; Position; Quantity of deposit; Sediment type; Size; Substrate type; Uniform resource locator/link to image; V18; V18-024RD; V18-025RD; V18-115SBT; V18-116SBT; V18-197C; V18-199C; V18-200C; V18-201C; V18-202C; V18-204C; V18-205C; V18-206C; V18-207C; V18-209C; V18-258; V18-263; V18-266; V18-267; V18-268; V18-269; V18-270; V18-273; V18-274; V18-275; V18-276; V18-277; V18-278; V18-279; V18-280; Vema; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 728 data points
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  • 4
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    PANGAEA
    In:  Supplement to: Feden, Robert H (1966): Volcanic rock from Caryn Seamount. Journal of Geophysical Research, 71(6), 1761-1763, https://doi.org/10.1029/JZ071i006p01761
    Publication Date: 2023-08-28
    Description: Caryn seamount (36° 42'N, 68° 02'W) was discovered in 1948 during Caryn cruise 1. During the summer of 1963 the Chain (cruise 36) occupied a dredge station on Caryn seamount. Caryn seamount (36° 42'N, 68° 02'W) was discovered in 1948 during Caryn cruise 1. During the summer of 1963 the Chain (cruise 36) occupied a dredge station on Caryn seamount. Manganese nodules, semiconsolidated mud, altered vesicular volcanics, and several glacial erratics were obtained from the western slope of the seamount between depths of about 3950 and 4300 m. The 1963 dredge haul by Chain, the first to obtain volcanic rocks, confirms the volcanic origin of the seamount. Previously, only manganese nodules had been dredged from Caryn, during cruise 21 of Chain.
    Keywords: Atlantic Ocean; CH03601; CH36-11PG; CH36-1PG; CH36-2PC; CH36-6RD; CH36-9PG; Chain; Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; DRG; Event label; GC; Gravity corer; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 114 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Sackett, William M (1966): Manganese Nodules: Thorium-230: Protactinium-231 Ratios. Science, 154(3749), 646-647, https://doi.org/10.1126/science.154.3749.646
    Publication Date: 2023-08-28
    Description: The Th230/Pa231 activity ratio in 7 of 11 manganese nodules is less than 10.8, the theoretical production ratio of activities in the ocean. This finding indicates difierential accumulation of these nuclides in authigenic deposits of manganese-iron oxide.
    Keywords: A-266/D-40; Alpha spectrometry; AT26601; AT266-40; Atlantic Ocean; Atlantis (1931); Blake Plateau, Atlantic Ocean; CH03601; CH36-6RD; Chain; Deposit type; DEPTH, sediment/rock; Description; DNWB0ABD; DOWNWIND-B1; DOWNWIND-H; Dredge; Dredge, chain bag; Dredge, rock; DRG; DRG_C; DRG_R; DWBD1; DWBD4; DWHD47; Event label; FANB01BD; FANBD-20D; FANFARE-B; GOS74; GOS74-2340; Gosnold; Horizon; Identification; MDPC02HO-MP-025F-2; MDPC02HO-MP-026A-3; MIDPAC; MPC-25F-2; MPC-26A-3; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Protactinium-231; Protactinium-231, standard deviation; RC05; RC05-1RD; Robert Conrad; Sample code/label; Spencer F. Baird; Thorium-230; Thorium-230, standard deviation; Thorium-232; Thorium-232, standard deviation; Uranium-238; Uranium-238, standard deviation; V18; V18-32RD; Vema
    Type: Dataset
    Format: text/tab-separated-values, 124 data points
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  • 6
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    PANGAEA
    In:  Supplement to: Jones, E J W; Laughton, Anthony S; Hill, M N; Davies, D (1976): A geophysical study of part of the western boundary of the Madeira-Cape Verde Abyssal plain. Deep Sea Research and Oceanographic Abstracts, 13(5), 889-907, https://doi.org/10.1016/0011-7471(76)90909-8
    Publication Date: 2023-08-28
    Description: The results are discussed of a geophysical survey undertaken by R.R.S. Discovery II early in 1962 in an area centred on 29° 15'N, 25° 5'W at the western extremity of the Madeira-Cape Verde Abyssal Plain. Seismic investigations show that the sediments are underlain by an intermediate layer about 2 km in thickness of velocity 4.1-5.4 km/sec which overlies a deep layer 5.2-km thick of velocity 6.3-6.8 km/sec. Refracted arrivals on the longest seismic line give a depth of 13.2 km to the M discontinuity. Magnetic results indicate that the topography of the abyssal hills in the western part of the area is probably continued eastwards as sub-bottom relief beneath the sediments of the abyssal plain. They also support the hypothesis that the intermediate seismic layer (layer 2) is composed predominantly of volcanic rocks. Examination of a well-defined magnetic anomaly over one topographic feature ("The Madcap Volcano") shows it to be composed of magnetized rocks (I = 8.4 × 10**-3 e.m.u./cm**3) having a direction of magnetization which points upwards at 25° with an azimuth of 305°. Measurements at ten heat flow stations show that the average geothermal flux in this region is 1.20 (±0.11) µcal/cm**2/sec.
    Keywords: Atlantic Ocean; D4810; D4814; Deposit type; DEPTH, sediment/rock; Description; Discovery II (1929); Event label; File name; Identification; MADCAP_62; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Photo/Video; Position; PV; Quantity of deposit; Sediment type; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 26 data points
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  • 7
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    PANGAEA
    In:  Supplement to: Hill, M N; Laughton, Anthony S (1966): RRS DISCOVERY Cruise 4 Report, Feb.-March 1965, Geology and geophysics in the N.E. Atlantic. Cruise Report Series, CR-11, 31 pp, https://store.pangaea.de/Projects/NOAA-MMS/RRSDiscovery_Cruise4_1965.pdf
    Publication Date: 2023-08-28
    Description: A total of 36 coring stations were worked during the cruise of which twenty-five were successful. Both piston and free-fall gravity coring techniques were employed and the cores were extruded and rough logged on board ship as soon as they had been taken. Twelve dredge stations were occupied on the cruise, all of them lying in the Peake Deep area, and nine were successful.
    Keywords: Atlantic Ocean; D4; D5607; D5608; D5619; D5627; Deposit type; DEPTH, sediment/rock; Description; Discovery (1962); Dredge; DRG; Elevation of event; Event label; Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 24 data points
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  • 8
    Publication Date: 2023-08-28
    Description: Manganese nodules recovered in the Pacific Ocean by the U. S. Bureau of Mines and by DeepSea Ventures Ltd. are studied for their chemical composition using X microprobe and X-ray fluorescence methods.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 9
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    In:  Lamont-Doherty Earth Observatory of Columbia University, New York
    Publication Date: 2023-08-28
    Keywords: Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge, rock; DRG_R; Elevation of event; Event label; Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Photo/Video; Piston corer; Position; PV; Quantity of deposit; RC10; RC10-003RD; RC10-101; RC10-101C1; RC10-101C3; RC10-103C1; RC10-104C4; RC10-11; RC10-110; RC10-123; RC10-123C4; RC10-13; RC10-131; RC10-153; RC10-154; RC10-164; RC10-165; RC10-168; RC10-171; RC10-172; RC10-176; RC10-178; RC10-179; RC10-182; RC10-205; RC10-21C2; RC10-21C3; RC10-233; RC10-239; RC10-244; RC10-26C6; RC10-26C7; RC10-274; RC10-278; RC10-279; RC10-36C1; RC10-36C2; RC10-40C2; RC10-40C4; RC10-41C1; RC10-41C2; RC10-41C4; RC10-44C2; RC10-45C3; RC10-49C2; RC10-49C3; RC10-69C2; RC10-70C1; RC10-76; RC10-77; RC10-78; RC10-79; RC10-7C2; RC10-7C6; RC10-81; RC10-87C7; RC10-88; RC10-8C1; RC10-8C2; RC10-91; RC10-93; RC10-96C2; RC10-96C4; RC10-97C1; RC10-97C4; RC10-97C5; RC10-98C1; RC10-98C3; RC10-98C4; RC10-99C2; Robert Conrad; Sediment type; Size; Substrate type; Uniform resource locator/link to file; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 1142 data points
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  • 10
    Publication Date: 2023-08-28
    Keywords: Baltic Sea; Date/Time of event; DEPTH, sediment/rock; Description; Elevation of event; Event label; Grab; GRAB; Iron oxide, Fe2O3; Latitude of event; Longitude of event; Loss on ignition; Manganese oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Organic matter; Phosphorus pentoxide; Sample ID; Water in rock; Wet chemistry; WNT-A7; WNT-CIII; WNT-S3
    Type: Dataset
    Format: text/tab-separated-values, 32 data points
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  • 11
    Publication Date: 2023-08-28
    Keywords: Baltic Sea; Core; CORE; Date/Time of event; DEPTH, sediment/rock; Description; DIVER; Dredge; DRG; Elevation of event; Event label; Grab; GRAB; Insoluble residue; Iron oxide, Fe2O3; Latitude of event; Longitude of event; Manganese oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Sample ID; Sampling by diver; Wet chemistry; WNT-11A; WNT-12A; WNT-15A; WNT-24; WNT-28B; WNT-2A; WNT-3; WNT-36; WNT-4; WNT-5; WNT-6; WNT-A11; WNT-A18; WNT-A19; WNT-A23; WNT-A3; WNT-A31; WNT-A7; WNT-CIII; WNT-CIV-A; WNT-CIV-B; WNT-F12A; WNT-F23-C; WNT-F58A; WNT-N1; WNT-N2; WNT-N3; WNT-N4; WNT-P20; WNT-P7A; WNT-P9; WNT-R/62; WNT-R6A; WNT-S3; WNT-S4; WNT-Z705
    Type: Dataset
    Format: text/tab-separated-values, 235 data points
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  • 12
    Publication Date: 2023-08-28
    Keywords: Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Description; HRS1; Iron; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Sample ID; Shape; X-ray fluorescence (XRF); Zinc
    Type: Dataset
    Format: text/tab-separated-values, 40 data points
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  • 13
    Publication Date: 2023-08-28
    Keywords: 2P-36; Antimony; Barium; Calcium; Chromium; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Dredge; DRG; Elevation of event; Europium; Event label; Hafnium; HRS1; Iron; Lanthanum; Latitude of event; Longitude of event; Manganese; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Prospector; Prospector-63; Samarium; Sample ID; Scandium; Shape; Sodium; Terbium; Thorium; Titanium; Uranium; Vanadium; X-ray microprobe; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 46 data points
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  • 14
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    PANGAEA
    In:  Supplement to: Winterhalter, Boris (1966): Pohjanlahden ja Suomenlahden rauta-mangaani-saostumista. Summary: Iron-manganese concretions from the gulf of Bothnia and the gulf of Finland. Geoteknillisiä julkaisuja - Geotekniska meddelanden - Geotechnical publications, 69, 77 pp, https://tupa.gtk.fi/julkaisu/geoteknillinen/gt_s_069.pdf
    Publication Date: 2023-08-28
    Description: Iron-manganese concretions, closely related to lacustrine ores and deep sea manganese nodules, are presently forming in different parts of Gulfs of Bothnia and Finland. They can be divided according to physical form into three distinct groups: (1) round pea-shaped concretions, (2) ring-shaped concrections, and (3) flat sheets and crusts of concretionary material. A definite correlation was found to exist between the form i.e. type of concretions and their chemical composition (Mn/Fe ratio). Trace element concentrations were generally rather high, although not as high as in deep sea manganese nodules. X-ray and DTA was used to study the mineralogy and crystal structure of the concretions. Surface concentrations and geographical distribution of the concretions were estimated on the basis of samples, diving observations and echo-grams.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 15
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    In:  Supplement to: Burns, Roger G; Fuerstenau, D W (1966): Electron-probe determination of inter-element relationships in manganese nodules. American Mineralogist, 51, 895-902, http://www.minsocam.org/ammin/AM51/AM51_895.pdf
    Publication Date: 2023-08-28
    Description: Manganese nodules have attracted considerable attention in recent years as a potential source of Mn, Fe, Co, Ni, Cu and other minor elements. These elements are enriched in manganese nodules relative to igneous rocks, sea-water, and deep-sea clays. The present paper describes methods by which element correlations may be determined with the electron-probe, and summarizes the results obtained by electron-beam scanning and specimen traversing. The results obtained in the present electron-probe investigation of manganese nodules may be summarized as follows: (l) The iron concentration fluctuates whereas the manganese concentration is relatively uniform throughout a manganese nodule, hbing slightly higher where iron is low. (2) There is a distinct correlation between Fe, Co, Ti, and Ca. (3) There is pronounced element coherence between Xi, Cu, Zn, and Mg, and between K and Ba. These elements are enriched with Mn and Al in regions of a nodule where the iron concentration is low. (4) The pronounced inter element relationships suggest that isomorphic substitution is an important factor controlling minor element distribution in manganese nodules. The ions Ni2+. Cu2+, Zn2+, Mg2+, K+ and Ba2+ substitute for Mn2+ in the "manganite" phases, Co(III) occurs with Fe(III) in hydrated iron oxide phases and Ti(IV) in delta-MnO2.
    Keywords: Aluminium; Calcium; Cobalt; Copper; DEPTH, sediment/rock; Description; DOWNWIND-H; Dredge; DRG; DWHD16; Electron Probe Microanalysis (EPMA); Horizon; Iron; Magnesium; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Potassium; Sample ID; Silicon; Titanium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 16
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    In:  National Institute of Oceanography, Wormely | Supplement to: National Institute of Oceanography, Wormley (1966): Discovery Cruise 11 Report, April-May 1966, Geology and geophysics in the N.E. Atlantic. National Institute of Oceanography, Wormley, Godalming, Surrey (hdl:10013/epic.47825.d003 pdf 634 kB), 16 pp, https://www.bodc.ac.uk/resources/inventories/cruise_inventory/reports/d11.pdf
    Publication Date: 2023-08-28
    Description: During Discovery Cruise 11, April-May 1966, eleven hauls were made on the crest and on the southern facing slope of Palmer Ridge in the Peake Deep area in order to fill out the information gained last year. Limestones were collected ranging in age from lowest Eocene through to Upper Tertiary, and several hauls successfully sampled the basement beneath these, producing weathered basalts, metamorphosed basalts and dolerites. In Peake Deep on the north slope of Palmer Ridge hard Eocene sediments were core sampled near the base of the slope but no cores could be got near the top.
    Keywords: Atlantic Ocean; D11; D5975; D5978; D5983; Deposit type; DEPTH, sediment/rock; Description; Discovery (1962); Dredge; DRG; Elevation of event; Event label; Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 29 data points
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  • 17
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    In:  Supplement to: SCRIPPS Institution of Oceanography (1966): TRIPOD Expedition, November-December 1966, List of sediment cores and dredge hawls, R/V Argo. Scripps Institution of Oceanography, UC San Diego, unpublished, 7 pp, https://www.ngdc.noaa.gov/mgg/curator/data/argo/tripod/tripod_expedition_report.pdf
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken on the TRIPOD Expedition from November until December 1966 by the Scripps Institution of Oceanography from the R/V Argo. A total of 38 cores and dredges were recovered and are available at Scripps for sampling and study.
    Keywords: Argo; Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; DRG; East Pacific Ocean; Elevation of event; Event label; GC; Gravity corer; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; TRI-01D; TRI-02D; TRI-02PG; TRI-03D; TRI-04D; TRI-04P; TRI-05D; TRI-06D; TRI-06P; TRI-06PG; TRI-07G; TRI-07P; TRI-08G; TRI-08P; TRI-08PG; TRI-09D; TRI-09G; TRI-09P; TRI-09PG; TRI-10G; TRI-13G; TRI-14G; TRIP02AR; TRIP03AR; TRIPOD_2; TRIPOD_3; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 301 data points
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  • 18
    Publication Date: 2023-08-28
    Keywords: Baltic Sea; Chromium; Cobalt; Copper; Date/Time of event; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; Grab; GRAB; Iron oxide, Fe2O3; Latitude of event; Lead; Longitude of event; Manganese oxide; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Sample ID; Spectrometric analysis; Strontium; Vanadium; WNT-2A; WNT-5; WNT-6; WNT-A31; WNT-A7; WNT-CIV-A; WNT-CIV-B; WNT-F12A; WNT-F23-C; WNT-F58A; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 130 data points
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  • 19
    Publication Date: 2023-08-28
    Keywords: Baltic Sea; Comment; Core; CORE; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; DIVER; Dredge; DRG; Elevation of event; Event label; Grab; GRAB; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Sampling by diver; Sediment type; Shape; Size; Substrate type; Uniform resource locator/link to image; WNT-11A; WNT-12A; WNT-14/61; WNT-14RR4; WNT-15A; WNT-17/61; WNT-19/61; WNT-23/61; WNT-24; WNT-28B; WNT-2A; WNT-3; WNT-36; WNT-4; WNT-4/61; WNT-5; WNT-6; WNT-8; WNT-9/61; WNT-A10; WNT-A11; WNT-A12; WNT-A18; WNT-A19; WNT-A22; WNT-A23; WNT-A24B; WNT-A3; WNT-A31; WNT-A5; WNT-A6; WNT-A7; WNT-A8; WNT-A9; WNT-B5A; WNT-B6; WNT-BII; WNT-BIII; WNT-BIV; WNT-BV; WNT-BVI; WNT-CI; WNT-CIII; WNT-CIV-A; WNT-CIV-B; WNT-CV; WNT-F10; WNT-F10A; WNT-F12A; WNT-F19A; WNT-F23-B; WNT-F23-C; WNT-F23E; WNT-F58A; WNT-L100; WNT-L103; WNT-L110; WNT-L115; WNT-L154; WNT-L162; WNT-L19; WNT-L22; WNT-L24; WNT-L32; WNT-L34; WNT-L36; WNT-L37; WNT-L65-A; WNT-L65-B; WNT-L67; WNT-L68; WNT-L70; WNT-L71; WNT-L73; WNT-L83; WNT-L89; WNT-L91; WNT-L92; WNT-L95; WNT-N1; WNT-N2; WNT-N3; WNT-N4; WNT-P20; WNT-P4; WNT-P7A; WNT-P9; WNT-R/62; WNT-R6A; WNT-S2; WNT-S3; WNT-S4; WNT-To3; WNT-Z705
    Type: Dataset
    Format: text/tab-separated-values, 888 data points
    Location Call Number Expected Availability
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  • 20
    Publication Date: 2024-02-03
    Keywords: Calculated; CTD; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; GIK/IfG; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; Latitude of event; Longitude of event; M1; M1_005; M1_006; M1_CTD005; M1_CTD006; Mediterranean Sea; Meteor (1964); Nitrate; Oxygen; Oxygen, microelectrode, ex-situ; Phosphate; Salinity; Silicate; Temperature, water; Turnover-thermometer
    Type: Dataset
    Format: text/tab-separated-values, 450 data points
    Location Call Number Expected Availability
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  • 21
    Publication Date: 2024-02-03
    Keywords: Alkalinity, total; Ammonia; Calcium; Calculated; CTD; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Eastern Arabian Sea; Elevation of event; Event label; Fluoride; GIK/IfG; Golf of Aden, Arabian Sea; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; Latitude of event; Longitude of event; M1; M1_023; M1_026; M1_028; M1_029; M1_039; M1_042; M1_043; M1_045; M1_049; M1_053; M1_055; M1_056; M1_062; M1_066; M1_069; M1_071; M1_072; M1_090; M1_091; M1_092; M1_093; M1_094; M1_095; M1_096; M1_099; M1_100; M1_101; M1_102; M1_103; M1_104; M1_105; M1_106; M1_107; M1_108; M1_109; M1_111; M1_112; M1_113; M1_114; M1_115; M1_116; M1_117; M1_118; M1_124; M1_125B; M1_126; M1_127; M1_128; M1_129; M1_130; M1_131; M1_132; M1_133; M1_134; M1_135; M1_136; M1_137; M1_138; M1_139; M1_142; M1_143; M1_144; M1_145; M1_146; M1_147; M1_148; M1_149; M1_150; M1_151; M1_152; M1_153; M1_154; M1_155; M1_156; M1_157; M1_158; M1_160; M1_161; M1_162; M1_163; M1_164; M1_165; M1_166; M1_167; M1_168; M1_169; M1_170; M1_171; M1_172; M1_173; M1_174; M1_175; M1_176; M1_177; M1_178; M1_179; M1_180; M1_181; M1_182; M1_183; M1_184; M1_185; M1_186; M1_187; M1_188; M1_189; M1_190; M1_194; M1_195; M1_196; M1_197; M1_198; M1_199; M1_200; M1_201; M1_202; M1_205; M1_206; M1_207; M1_208; M1_209; M1_210; M1_211; M1_215; M1_217; M1_218; M1_219; M1_221; M1_222; M1_223; M1_224; M1_225; M1_226; M1_227; M1_228; M1_229; M1_232; M1_233; M1_234; M1_235; M1_236; M1_237; M1_238; M1_239; M1_240; M1_241; M1_CTD023; M1_CTD026; M1_CTD028; M1_CTD029; M1_CTD039; M1_CTD042; M1_CTD043; M1_CTD045; M1_CTD049; M1_CTD053; M1_CTD055; M1_CTD056; M1_CTD062; M1_CTD066; M1_CTD069; M1_CTD071; M1_CTD072; M1_CTD090; M1_CTD091; M1_CTD092; M1_CTD093; M1_CTD094; M1_CTD095; M1_CTD096; M1_CTD099; M1_CTD100; M1_CTD101; M1_CTD102; M1_CTD103; M1_CTD104; M1_CTD105; M1_CTD106; M1_CTD107; M1_CTD108; M1_CTD109; M1_CTD111; M1_CTD112; M1_CTD113; M1_CTD114; M1_CTD115; M1_CTD116; M1_CTD117; M1_CTD118; M1_CTD124; M1_CTD125; M1_CTD126; M1_CTD127; M1_CTD128; M1_CTD129; M1_CTD130; M1_CTD131; M1_CTD132; M1_CTD133; M1_CTD134; M1_CTD135; M1_CTD136; M1_CTD137; M1_CTD138; M1_CTD139; M1_CTD142; M1_CTD143; M1_CTD144; M1_CTD145; M1_CTD146; M1_CTD147; M1_CTD148; M1_CTD149; M1_CTD150; M1_CTD151; M1_CTD152; M1_CTD153; M1_CTD154; M1_CTD155; M1_CTD156; M1_CTD157; M1_CTD158; M1_CTD160; M1_CTD161; M1_CTD162; M1_CTD163; M1_CTD164; M1_CTD165; M1_CTD166; M1_CTD167; M1_CTD168; M1_CTD169; M1_CTD170; M1_CTD171; M1_CTD172; M1_CTD173; M1_CTD174; M1_CTD175; M1_CTD176; M1_CTD177; M1_CTD178; M1_CTD179; M1_CTD180; M1_CTD181; M1_CTD182; M1_CTD183; M1_CTD184; M1_CTD185; M1_CTD186; M1_CTD187; M1_CTD188; M1_CTD189; M1_CTD190; M1_CTD194; M1_CTD195; M1_CTD196; M1_CTD197; M1_CTD198; M1_CTD199; M1_CTD200; M1_CTD201; M1_CTD202; M1_CTD205; M1_CTD206; M1_CTD207; M1_CTD208; M1_CTD209; M1_CTD210; M1_CTD211; M1_CTD215; M1_CTD217; M1_CTD218; M1_CTD219; M1_CTD221; M1_CTD222; M1_CTD223; M1_CTD224; M1_CTD225; M1_CTD226; M1_CTD227; M1_CTD228; M1_CTD229; M1_CTD232; M1_CTD233; M1_CTD234; M1_CTD235; M1_CTD236; M1_CTD237; M1_CTD238; M1_CTD239; M1_CTD240; M1_CTD241; Meteor (1964); Nitrate; Nitrite; Oxygen; Oxygen, microelectrode, ex-situ; pH; Phosphate; Phosphorus, total; Red Sea; Salinity; Silicate; Temperature, water; Turnover-thermometer; Western Arabian Sea
    Type: Dataset
    Format: text/tab-separated-values, 38537 data points
    Location Call Number Expected Availability
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  • 22
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Dietrich, Günter; Düing, Walter; Grasshoff, Klaus; Koske, Peter H (1966): Physikalische und chemische Daten nach Beobachtungen des Forschungsschiffes Meteor im Indischen Ozean 1964/65. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe A Allgemeines, Physik und Chemie des Meeres, Gebrüder Bornträger, Berlin, Stuttgart, A2, 1-155
    Publication Date: 2024-02-03
    Description: The present volume gives the observed physical and chemical data obtained by R.V. "Meteor" in the Indian Ocean during cruise 1964/65. The tables are based on the computations made by the National Oceanographic Data Center (NODC) in Washington. In addition to the normally communicated data, the tables contain four chemical parameters: alkalinity, ammonia, fluoride, and calcium.
    Keywords: Biscaya; CTD/Rosette; CTD-RO; Eastern Arabian Sea; GIK/IfG; Golf of Aden, Arabian Sea; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; M1; M1_001; M1_005; M1_006; M1_023; M1_026; M1_028; M1_029; M1_039; M1_042; M1_043; M1_045; M1_049; M1_053; M1_055; M1_056; M1_062; M1_066; M1_069; M1_071; M1_072; M1_090; M1_091; M1_092; M1_093; M1_094; M1_095; M1_096; M1_099; M1_100; M1_101; M1_102; M1_103; M1_104; M1_105; M1_106; M1_107; M1_108; M1_109; M1_111; M1_112; M1_113; M1_114; M1_115; M1_116; M1_117; M1_118; M1_124; M1_125B; M1_126; M1_127; M1_128; M1_129; M1_130; M1_131; M1_132; M1_133; M1_134; M1_135; M1_136; M1_137; M1_138; M1_139; M1_142; M1_143; M1_144; M1_145; M1_146; M1_147; M1_148; M1_149; M1_150; M1_151; M1_152; M1_153; M1_154; M1_155; M1_156; M1_157; M1_158; M1_160; M1_161; M1_162; M1_163; M1_164; M1_165; M1_166; M1_167; M1_168; M1_169; M1_170; M1_171; M1_172; M1_173; M1_174; M1_175; M1_176; M1_177; M1_178; M1_179; M1_180; M1_181; M1_182; M1_183; M1_184; M1_185; M1_186; M1_187; M1_188; M1_189; M1_190; M1_194; M1_195; M1_196; M1_197; M1_198; M1_199; M1_200; M1_201; M1_202; M1_205; M1_206; M1_207; M1_208; M1_209; M1_210; M1_211; M1_215; M1_217; M1_218; M1_219; M1_221; M1_222; M1_223; M1_224; M1_225; M1_226; M1_227; M1_228; M1_229; M1_232; M1_233; M1_234; M1_235; M1_236; M1_237; M1_238; M1_239; M1_240; M1_241; M1_CTD001; M1_CTD005; M1_CTD006; M1_CTD023; M1_CTD026; M1_CTD028; M1_CTD029; M1_CTD039; M1_CTD042; M1_CTD043; M1_CTD045; M1_CTD049; M1_CTD053; M1_CTD055; M1_CTD056; M1_CTD062; M1_CTD066; M1_CTD069; M1_CTD071; M1_CTD072; M1_CTD090; M1_CTD091; M1_CTD092; M1_CTD093; M1_CTD094; M1_CTD095; M1_CTD096; M1_CTD099; M1_CTD100; M1_CTD101; M1_CTD102; M1_CTD103; M1_CTD104; M1_CTD105; M1_CTD106; M1_CTD107; M1_CTD108; M1_CTD109; M1_CTD111; M1_CTD112; M1_CTD113; M1_CTD114; M1_CTD115; M1_CTD116; M1_CTD117; M1_CTD118; M1_CTD124; M1_CTD125; M1_CTD126; M1_CTD127; M1_CTD128; M1_CTD129; M1_CTD130; M1_CTD131; M1_CTD132; M1_CTD133; M1_CTD134; M1_CTD135; M1_CTD136; M1_CTD137; M1_CTD138; M1_CTD139; M1_CTD142; M1_CTD143; M1_CTD144; M1_CTD145; M1_CTD146; M1_CTD147; M1_CTD148; M1_CTD149; M1_CTD150; M1_CTD151; M1_CTD152; M1_CTD153; M1_CTD154; M1_CTD155; M1_CTD156; M1_CTD157; M1_CTD158; M1_CTD160; M1_CTD161; M1_CTD162; M1_CTD163; M1_CTD164; M1_CTD165; M1_CTD166; M1_CTD167; M1_CTD168; M1_CTD169; M1_CTD170; M1_CTD171; M1_CTD172; M1_CTD173; M1_CTD174; M1_CTD175; M1_CTD176; M1_CTD177; M1_CTD178; M1_CTD179; M1_CTD180; M1_CTD181; M1_CTD182; M1_CTD183; M1_CTD184; M1_CTD185; M1_CTD186; M1_CTD187; M1_CTD188; M1_CTD189; M1_CTD190; M1_CTD194; M1_CTD195; M1_CTD196; M1_CTD197; M1_CTD198; M1_CTD199; M1_CTD200; M1_CTD201; M1_CTD202; M1_CTD205; M1_CTD206; M1_CTD207; M1_CTD208; M1_CTD209; M1_CTD210; M1_CTD211; M1_CTD215; M1_CTD217; M1_CTD218; M1_CTD219; M1_CTD221; M1_CTD222; M1_CTD223; M1_CTD224; M1_CTD225; M1_CTD226; M1_CTD227; M1_CTD228; M1_CTD229; M1_CTD232; M1_CTD233; M1_CTD234; M1_CTD235; M1_CTD236; M1_CTD237; M1_CTD238; M1_CTD239; M1_CTD240; M1_CTD241; Mediterranean Sea; Meteor (1964); Red Sea; Western Arabian Sea
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
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  • 23
    Publication Date: 2024-02-03
    Keywords: Biscaya; Calculated; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; GIK/IfG; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; Latitude of event; Longitude of event; M1; M1_001; M1_CTD001; Meteor (1964); Oxygen; Oxygen, microelectrode, ex-situ; Salinity; Temperature, water; Turnover-thermometer
    Type: Dataset
    Format: text/tab-separated-values, 176 data points
    Location Call Number Expected Availability
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  • 24
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Cordes, Eilhard (1966): Aufbau und Bildungsbedingungen der Schwermineralseifen bei Skagen (Dänemark). Meyniana, 16, 1-35, https://doi.org/10.2312/meyniana.1966.16.1
    Publication Date: 2024-04-19
    Description: Aufbau und Ausdehnung der Schwermineral-Anreicherungen (Ilmenit, Granat, Amphibol) am Strand südlich Skagens wurden in langen Schürfgräben untersucht. Die Seifenlagen ziehen durchgehend vom Kliff-Fuß bis zur mittleren Meereshöhe hin und liegen meist diskordant auf der alten Strandschichtung. Ihre strandparallele Ausdehnung beträgt bis zu 100 m. Aufgebaut werden sie aus dünnen Schwermineral-Lamellen, die in kleinerem Umfang überall in den Strandablagerungen zu finden sind und hier das Gefüge nachzeichnen (Rippeln, Strandwallschichtung, Schichtstörungen). Die Seifenbildung geht in einem Gebiet mit verstärktem Küstenabtrag vor sich (Lee-Erosion südlich der Hafenmolen von Skagen). Dieses deutet darauf hin, daß die Schwerminerale bei Aufarbeitung bereits vorhandener Sedimente infolge ihres unterschiedlichen hydraulischen Verhaltens Zurückbleiben und schließlich angereichert werden. Die Korngrößenverteilung der Minerale in verschiedenen Sedimentproben zeigen, daß mit steigender Schwermineral-Anreicherung eine Kornverfeinerung und Zunahme der spezifisch schwersten Minerale (opake Erzminerale und Zirkon) auftritt. In ähnlicher Weise werden die Sortierungswerte besser. Die Aufbereitung des Sedimentes wird, in Anlehnung an v. ENGELHARDT (1939), mit einem doppelten Sortierungsvorgang durch die Wasserbewegung am Strand erklärt. Beim Absinken des Sandes nach dem Brecherschwall tritt eine Vorsortierung ein, die den Abtransport der leichteren und größeren Minerale im Sog begünstigt. Verbindungen zu Vorstellungen der Aufbereitungstechnik (Rundherdverfahren) und Hydrodynamik ('laminare Unterschicht') werden hergestellt. Die Dünensande Skagens sind infolge ihres hohen Schwermineralgehaltes und günstiger Äquivalentgrößen der einzelnen Minerale besonders bedeutsam für die Seifenbildung am Strand.
    Keywords: Europe, Denmark; HAND; Sampling by hand; Skagen1964
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
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  • 25
    Publication Date: 2024-04-19
    Keywords: Amphibole; Area/locality; Distance; Europe, Denmark; Garnet; HAND; Heavy minerals; Median, grain size; Opaque minerals; Sample ID; Sampling by hand; Skagen1964
    Type: Dataset
    Format: text/tab-separated-values, 77 data points
    Location Call Number Expected Availability
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  • 26
    Publication Date: 2024-04-19
    Keywords: Amphibole; Area/locality; Epidote; Europe, Denmark; Garnet; HAND; Heavy minerals; Median, grain size; Minerals, other; Opaque minerals; Sample ID; Sampling by hand; Skagen1964; Sorting; Zircon
    Type: Dataset
    Format: text/tab-separated-values, 300 data points
    Location Call Number Expected Availability
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  • 27
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Bonatti, Enrico; Joensuu, Oiva (1966): Deep-Sea Iron Deposit from the South Pacific. Science, 154(3749), 643-645, https://doi.org/10.1126/science.154.3749.643
    Publication Date: 2024-04-20
    Description: Along with specimens of manganese oxides and basalt, rocks containing more than 30 percent iron by weight and consisting mainly of poorly crystallized goethite have been dredged from the flanks of a seamount located on the East Pacific Rise. The Fe-Mn ratio varies widely among the various oxide rocks deposited at this locality and at another seamount in the same area. The deposit was probably formed by fractional precipitation of iron and manganese which had been introduced locally into the bottom water by hydrothermal solutions of volcanic origin, and by leaching from deep-sea basaltic lavas.
    Keywords: Aluminium oxide; AMPH-002D; AMPH01AR; AMPH01AR-002D; AMPHITRITE; Argo; Barium; Boron; Calcium oxide; Chromium; Cobalt; Copper; DEPTH, sediment/rock; Dredge; DRG; Iron; Loss on drying; Magnesium oxide; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Optical spectrographic analysis; Pacific Ocean; Potassium oxide; Sample ID; Silicon dioxide; Strontium
    Type: Dataset
    Format: text/tab-separated-values, 46 data points
    Location Call Number Expected Availability
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