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  • PANGAEA
  • 1975-1979
  • 1970-1974  (16)
  • 1945-1949
  • 1935-1939
  • 1973  (16)
Collection
Keywords
Years
  • 1975-1979
  • 1970-1974  (16)
  • 1945-1949
  • 1935-1939
Year
  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: Ryan, William B F; Hsü, Kenneth J; Cita, Maria Bianca; Dumitrica, Paulian; Llort, Jennifer; Maync, Wolf; Nesteroff, Wladimir D; Pautot, Guy; Stradner, Herbert; Wezel, Forese C (1973): Sites 133 and 134. In: Ryan, W.B.F.; Hsu, K.J.; et al., Initial Reports of the Deep Sea Drilling Project, 13, Initial Reports of the Deep Sea Drilling Project, 13, U.S. Government Printing Office, XIII, 465-514, https://doi.org/10.2973/dsdp.proc.13.114.1973
    Publication Date: 2023-08-28
    Description: The western margin of Sardinia (had been explored in the Spring of 1970 by the R/V Jean Charcot of CNEXO. It showed that the basement ridge west of Sardinia lies at the very distal edge of the continental slope and has effectively dammed an upslope sedimentary basin which is presently isolated from the Balearic Abyssal Plain. Consequently a series of holes was contemplated along an east to west transverse of the Charcot profile.
    Keywords: 13-134E; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Identification; Leg13; Mediterranean Sea/PLAIN; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 9 data points
    Location Call Number Expected Availability
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  • 2
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    PANGAEA
    In:  Supplement to: Ryan, William B F; Hsü, Kenneth J; Cita, Maria Bianca; Dumitrica, Paulian; Llort, Jennifer; Maync, Wolf; Nesteroff, Wladimir D; Pautot, Guy; Stradner, Herbert; Wezel, Forese C (1973): Site 126. In: Ryan, W.B.F.; Hsu, K.J.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XIII, 219-241, https://doi.org/10.2973/dsdp.proc.13.108.1973
    Publication Date: 2023-08-28
    Description: The single "raison d'être" for selecting Site 126 was to explore the pre-evaporite history of the eastern Mediterranean and hopefully to establish the paleoenvironment which preceded the Late Miocene salinity crisis. The selcetd site is in a deep cleft in the Mediterranean Ridge in the central Ionian Sea, a cleft that cuts more than 250 meters below the level of Horizon M and at the same time is floored by flat-lying sediments. A secondary objective of the cleft site-selection was to ascertain what kind of sediment makes up the horizontal fill and hopefully to determine some details of the history and mechanics of the depression-filling process.
    Keywords: 13-126; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Identification; Leg13; Mediterranean Sea/RIDGE; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
    Location Call Number Expected Availability
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  • 3
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    PANGAEA
    In:  Supplement to: Kulm, LaVerne D; von Huene, Roland; Duncan, John R; Ingle, James C; Kling, S A; Musich, L F; Piper, David J W; Pratt, Richard M; Schrader, Hans-Jürgen; Weser, Oscar E; Wise, Sherwood W (1973): Site 172. In: Kulm, L.D.; von Huene, R.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XVIII, 15-30, https://doi.org/10.2973/dsdp.proc.18.103.1973
    Publication Date: 2023-08-28
    Description: Site 172 was continuously cored to a depth of 24 meters in a sediment pond 140 kilometers south of the Murray fracture zone. The upper 9 meters consist of a moderate brown pelagic clay which changes to a zeolite-rich brown clay, brown clay zeolitite and zeolitite in the lower 9 to 24 meters. An Early Oligocene (35 to 38 my) nannofossil horizon occurs near an extrusive basalt encountered at 24 meters. These sediments are older than the 29 my age indicated by a recent identification of magnetic anomaly 8 in the "disturbed" zone. The age discrepancy suggests that the magnetic anomalies in the "disturbed" zone are still not identified correctly.
    Keywords: 18-172; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Identification; Leg18; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 25 data points
    Location Call Number Expected Availability
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  • 4
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    PANGAEA
    In:  Supplement to: Winterer, Edward L; Ewing, John I; Douglas, Robert G; Jarrard, Richard D; Lancelot, Yves; Moberly, Ralph; Moore, Theodore C; Roth, P H; Schlanger, Seymour O (1973): Initial Reports of the Deep Sea Drilling Project 17. U. S. Government Printing Office, XVII, https://doi.org/10.2973/dsdp.proc.17.1973
    Publication Date: 2023-08-28
    Description: The main objectives of Leg 17 were to establish the regional pattern of oceanic crustal ages in the central Pacific, to obtain cores of the entire stratigraphic succession, especially from pre-Middle Eocene strata, To document the history of growth and subsidence of seamounts located along seamount chains, by drilling on the archipelagic apron of sediments near the foot of individual seamounts and to sample acoustic reflectors seen on seismic reflection profiles and to establish their physical properties and their ages.
    Keywords: 17-164; 17-165A; 17-168; 17-169; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg17; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific; North Pacific/BASIN; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 103 data points
    Location Call Number Expected Availability
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  • 5
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    PANGAEA
    In:  Supplement to: Heezen, Bruce C; MacGregor, Ian D; Foreman, H P; Forristall, G; Hekel, H; Jones, E J W; Kaneps, Ansis G; Krasheninnikov, Valery A; Okada, H; Ruef, Michael R (1973): The Post-Jurassic Sedimentary Sequence on the Pacific Plate; a Kinematic Interpretation Of Diachronous Deposits. In: Heezen, B.C.; MacGregor, I.D., Initial Reports of the Deep Sea Drilling Project, 20, Initial Reports of the Deep Sea Drilling Project, 20, U.S. Government Printing Office, XX, 725-738, https://doi.org/10.2973/dsdp.proc.20.133.1973
    Publication Date: 2023-08-28
    Description: The sea floor of the western Pacific is covered by five stratigraphic units: (l)an eastward thinning wedge of late Tertiary silty clay, primarily of volcanic origin, (2) a Cretaceous to Tertiary zeolitic red clay, (3) a Late Cretaceous to Tertiary chalk/chert sequence, (4) a Cretaceous clay, and (5) a basal chalk/chert sequence. The basal chalk was deposited on the young crust at the crest of the mid-oceanic ridge, while the upper chalk was deposited beneath the equator, and the abyssal clays were deposited in abyssal depths in mid latitudes. A kinematic model has been constructed that outlines the deposition of these units on growing crust, which not only was displaced westward away from the accretion center of the mid-oceanic ridge, but northward under the equator. The average northward component of motion for the Pacific plate has been 2 cm per year from 0 to 30 m.y. and 4.4 cm per year from 30 to 100 m.y. The deep-sea deposits of the Pacific are basically and systematically time transgressive. Claims of general synchroneity for either lithostratigraphy or acoustostratigraphy are rejected as inconsistent with both the drilling data and the kinematic model of Pacific pelagic stratigraphy. A few more well sampled holes in the ancient Pacific plate combined with an appropriately refined kinematic model should yield a 'rather detailed history of the Pacific plate since the Jurassic.
    Keywords: 20-195; 20-196; 20-198A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg20; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/ABYSSAL FLOOR; North Pacific/BASIN; Position; Quantity of deposit; Sample code/label; Sediment type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 128 data points
    Location Call Number Expected Availability
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  • 6
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    PANGAEA
    In:  Supplement to: Fein, Charles D; Morgenstein, Maury (1973): Microprobe analysis of manganese crusts from the Hawaiian Archipelago. In: Phase I Report - Inter-University Program of Research on Ferromanganese Deposits of the Ocean Floor. Seabed Assessment Program, IDOE, NSF, Washington D.C., USA - http://catalog.hathitrust.org/Record/005761114 (pdf 733 kB), 85-92, https://store.pangaea.de/Projects/NOAA-MMS/Fein_1973_IDOE.pdf
    Publication Date: 2023-08-28
    Description: Quantitative and qualitative chemical analyses were performed on fourteen manganese nodules and crusts from the Waho Shelf. The analyses showed that submarine weathering has leached several elements, notably Si02, A1203, Na20, CaO and MnO from the hydrated glass surrounding the basaltic seeds of the nodules. The altered glass was enriched in Ti02, MgO, K2O and total Fe. The manganese bands formed on the altered glass were further depleted in Si02, Al203, and similar to the hydrated glass in Na2O and CaO content. The manganese-enriched zones also showed higher TiO2 and NiO than the basaltic seeds, and higher total Fe than pelagic nodules from the North Pacific. Qualitative measurement of Cu, Ni, and Co, showed relative enrichment in the manganese bands. A proposed model for manganese accretion in the Waho Shelf incorporates local submarine weathering of basalts, redistribution of Mn in marine sediments, and an influx of Mn "rain" on the sea floor.
    Keywords: Aluminium oxide; Calcium oxide; Calculated; Chromium(III) oxide; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Electron microprobe (EMP); Elevation of event; Event label; Hawaii islands; Identification; Iron oxide, FeO; Kauai_Sediments-Exped; Latitude of event; Longitude of event; Magnesium oxide; Manganese oxide; Nickel oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Potassium oxide; Silicon dioxide; Sodium oxide; TE6-1RD; TE7-3RD; TE7-4RD; TE8-1RD; TE8-5RD; TE8-7RD; Teritu; Titanium dioxide; Water in rock; Zone
    Type: Dataset
    Format: text/tab-separated-values, 176 data points
    Location Call Number Expected Availability
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  • 7
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    PANGAEA
    In:  Supplement to: Amos, A F; Garside, Christopher; Gerard, Robert D; Levitus, Sydney; Malone, T C; Paul, Allen Z; Roels, Oswald A (1973): Study of the impact of manganese nodule mining on the seabed and water column. In: Phase I Report - Inter-University Program of Research on Ferromanganese Deposits of the Ocean Floor. Seabed Assessment Program, International Decade of Ocean Exploration, National Science Foundation, Washington D.C., USA, 221-264, hdl:2027/wu.89033915380
    Publication Date: 2023-08-28
    Description: he proposed mining of ferromanganese deposits from the deep sea will affect benthic and pelagic environments depending to a great extent on the method of nodule retrieval and separation. Three basic deep-ocean mining systems have been proposed, each of which will effect the removal under varying conditions of water, sediment and nodules from the ocean floor. This report summarizes existing oceanographhic information on potential manganese nodule mining areas at the date of publication and presents the results of field observations in a manganese nodule area of the North Atlantic Ocean surveyed during Cruise 15 of the R/V Robert Conrad.
    Keywords: Atlantic Ocean; Comment; Deposit type; DEPTH, sediment/rock; Description; File name; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Photo/Video; Position; PV; Quantity of deposit; RC15; RC15-180C; Robert Conrad; Sediment type; Station 222; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 9 data points
    Location Call Number Expected Availability
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  • 8
    Publication Date: 2023-08-28
    Keywords: Barium; Calcium; Carbon, total; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Elevation of event; Event label; Identification; Iron; Latitude of event; Lead; Longitude of event; Magnesium; Manganese; Method/Device of event; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Phosphorus; Piston corer; Potassium; RC13; RC13-66; RC13-70; Robert Conrad; Shape; Sodium; Sulfur, total; Titanium; X-ray emission spectroscopy (XES); Zinc
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
    Location Call Number Expected Availability
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  • 9
    Publication Date: 2023-08-28
    Keywords: Aluminium; Atlantic Ocean; Barium; Calcium; Carbon, total; Chromium; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Dredge; DRG; Elevation of event; Event label; Identification; Indian Ocean; Iron; Latitude of event; Lead; Longitude of event; Magnesium; Manganese; Method/Device of event; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Phosphorus; Potassium; Shape; Silicon; Sodium; Strontium; Titanium; TRAWL; Trawl net; V15; V15-135SBT; V16; V16-19SBT; V16-29SBT; V18; V18-11RD; Vema; Water in rock; X-ray fluorescence (XRF); Zinc
    Type: Dataset
    Format: text/tab-separated-values, 71 data points
    Location Call Number Expected Availability
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  • 10
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    PANGAEA
    In:  Supplement to: MNHN (1973): OSIRIS I Cruise - MD00, R/V Marion Dufresne, Core list. Muséum National d'Histoire Naturelle, Paris, unpublished, https://geocores.mnhn.fr/index.php?catid=7&blogid=1
    Publication Date: 2023-08-28
    Description: The cores and dredges described at this site were taken on the OSIRIS I cruise from 29 april until 7 june 1973 by the Muséum National d'Histoire Naturelle from the R/V Marion Dufresne. A total of 54 cores and dredges were recovered and are available at MNHN for sampling and study.
    Keywords: Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; DRG; Elevation of event; Event label; Indian Ocean; Latitude of event; Longitude of event; Marion Dufresne (1972); MD00; MD 00-09-DR; MD 00-12-PS; MD 00-42-PS; MD 00-43-PS; MD 00-44-PS; MD 00-45-DR; MD 00-47-DR; MD 00-47-PS; MD 00-54-PS; MD-DR730001; MD-DR730004; MD-DR730005; MD-PS730008; MD-PS730031; MD-PS730032; MD-PS730033; MD-PS730034; MD-PS730040; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; OSIRIS I; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 262 data points
    Location Call Number Expected Availability
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