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  • Articles  (243,064)
  • Data  (187)
  • 1985-1989  (107,535)
  • 1975-1979  (74,109)
  • 1970-1974  (61,607)
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Year
Journal
  • 1
    Publication Date: 1977-01-01
    Print ISSN: 0364-152X
    Electronic ISSN: 1432-1009
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering
    Published by Springer
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  • 2
    ISSN: 1546-1696
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Process Engineering, Biotechnology, Nutrition Technology
    Notes: [Auszug] The goal of the National Laboratory Gene Library Project at the Los Alamos and Lawrence Livermore National Laboratories is the production of chromosome–specific human gene libraries and their distribution to the scientific community for studies of the molecular biology of genes and ...
    Type of Medium: Electronic Resource
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  • 3
    Publication Date: 1986-09-01
    Print ISSN: 0741-3335
    Electronic ISSN: 1361-6587
    Topics: Physics
    Published by Institute of Physics
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  • 4
    Publication Date: 2023-07-09
    Keywords: Archive of Ocean Data; ARCOD; Arctic Ocean; Chaetoceros septentrionalis; Counting, diatoms; Event label; Gomphonema exiguum; Gomphonema septentrionale; Latitude of event; Longitude of event; Melosira arctica; MULT; Multiple investigations; Navicula directa; Navicula kariana; Navicula pennata; Navicula punctulata; Navicula vitrea; Nitzschia polaris; Nitzschia subtilis; Pinnularia quadratarea; SP-22-1980; SP-23-1977; Sum
    Type: Dataset
    Format: text/tab-separated-values, 26 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Bezrukov, Panteleimon L; Skornyakova, Nadezhda S; Murdmaa, Ivar O; Andrushchenko, Polina F; Zenkevich, Nikita L (1976): Ferromanganese Nodules of the Pacific Ocean. P.P. Shirshov Institute of Oceanology of the USSR Academy of Sciences, Transactions, vol. 109. Moscow, Nauka Publ. (P.L. Bezrukov, Ed.), 301 pp
    Publication Date: 2023-08-28
    Description: The monograph highlights extensive materials collected during expeditions of P.P. Shirshov Institute of Oceanology. We consider facial conditions of nodule formation, regularities of their distribution, stratigraphic position, petrography, mineral composition, textures, geochemistry of nodules and hosting sediments. Origin of iron-manganese nodules in the Pacific Ocean is considered as well.
    Keywords: AK4-225-TR; AK4-227-PH; AK4-230-GR; AK4-231-GR; AK4-232-GR; AK4-232-PH; AK4-233-GR; AK4-233-TR; AK4-259-GR; AK4-259-PH; AK4-260-GR; AK4-261-GR; Akademik Kurchatov; AKU4; Archive of Ocean Data; ARCOD; Central Basin, Pacific Ocean; Central Pacific Seamounts, Pacific Ocean; DM8; DM8-516-GR; DM8-518-GR; DM8-520-GR; DM8-521-TR; DM8-541-GR; DM8-554-GR; DM8-556-GR; DM8-568-GR; DM8-569-GR; DM8-598-GR; DM8-599-GR; DM8-600-GR; DM8-607-GR; DM8-608-GR; Dmitry Mendeleev; Dredge; DRG; Eastern Basin, Pacific Ocean; Eastern Mariana Basin, Pacific Ocean; Equatorial Pacific; GC; Grab; GRAB; Gravity corer; Manihiki Plateau, Pacific Ocean; Marcus-Necker Ridge; Mariana Basin, Pacific Ocean; MULT; Multiple investigations; Northwestern Basin, Pacific Ocean; OKEAN; Okean Grab; Photo/Video; PV; Southeast Pacific; Southern Basin, Pacific Ocean; TRAWL; Trawl net; VITYAZ; Vityaz (ex-Mars); Vityaz-20; Vityaz-25; Vityaz-29; VITYAZ3150-TR; VITYAZ3151-TR; VITYAZ3233-GC-2; Vityaz-34; VITYAZ3630-PH; VITYAZ3631-GR-1; VITYAZ3632-PH; VITYAZ3635-PH; VITYAZ3729-GC-1; VITYAZ3782-PH; VITYAZ3782-TR; VITYAZ3787-TR; VITYAZ3802-TR; VITYAZ3871-GR-1; VITYAZ3899-GR-1; VITYAZ3900-GR-1; VITYAZ3996-TR; VITYAZ4009-TR; VITYAZ4074-TR; VITYAZ4084-GR-1; VITYAZ4090-TR; VITYAZ4104-TR; VITYAZ4191-TR; VITYAZ4199-TR; VITYAZ4217-TR; VITYAZ4221-TR; VITYAZ4239-PH; VITYAZ4239-TR; VITYAZ4245-GR; VITYAZ4249-PH; VITYAZ4249-TR; VITYAZ4261-PH; VITYAZ4265-TR; VITYAZ4273-GR-1; VITYAZ4273-PH; VITYAZ4273-TR; VITYAZ4279-PH; VITYAZ4279-TR; VITYAZ4281-TR; VITYAZ4285-GR-1; VITYAZ4285-PH; VITYAZ4289-GR-1; VITYAZ4289-TR; Vityaz-43; VITYAZ4309-TR; VITYAZ4320-TR; VITYAZ4331-GR-1; VITYAZ4343-GR-1; VITYAZ4347-GR-1; VITYAZ4347-PH; VITYAZ4351-GR; VITYAZ4355-GR; VITYAZ4359-GR-1; VITYAZ4359-PH; VITYAZ4362-GR-1; VITYAZ4370-PH; VITYAZ4370-TR; Vityaz-48; VITYAZ5066-GR; VITYAZ5066-TR; VITYAZ5074-PH; VITYAZ5074-TR; VITYAZ5096-PH; VITYAZ5100-GR-1; VITYAZ5110-GR-1; VITYAZ5112-GR; VITYAZ5114-GR; VITYAZ5124-TR; VITYAZ5126-GR-1; VITYAZ5128-TR; VITYAZ5129-GR-1; VITYAZ5133-TR; VITYAZ5139-GR-1; VITYAZ5159-TR; VITYAZ5163-GR-1; VITYAZ5398-GR-1; VITYAZ5408-GR-1; VITYAZ5409-GR-1; VITYAZ5410-GR-1; VITYAZ5411-GR-1; VITYAZ5412-DR; VITYAZ5414-GR-1; VITYAZ5420-GR-1; VITYAZ5421-GR-1; VITYAZ5422-GR-1; VITYAZ5423-GR-1; VITYAZ5424-GR; VITYAZ5429-GR-1; VITYAZ5432-GR-1; VITYAZ5437-GR; VITYAZ5505-GR; VITYAZ5937A-GR; VITYAZ5937-GR; VITYAZ5955; VITYAZ5958-GR; VITYAZ5959-GR; VITYAZ5960-GR; VITYAZ5960-PH; VITYAZ5962-GR; VITYAZ5962-PH; VITYAZ5963-GC; VITYAZ5964-GR; VITYAZ5965-0-GR; VITYAZ5965-10-GR-1; VITYAZ5965-1-GR; VITYAZ5965-2-GC; VITYAZ5965-3-GR; VITYAZ5965-3-TR; VITYAZ5965-5-GR; VITYAZ5965-6-GC; VITYAZ5966-GR; VITYAZ5966-PH; VITYAZ5968-14-DR; VITYAZ5968-15-DR; VITYAZ5968-18-GC; VITYAZ5968-1-GR; VITYAZ5968-2-GC; VITYAZ5968-3-GR; VITYAZ5968-4-GR; VITYAZ5968-7-TR; VITYAZ5968-9-GR; VITYAZ5970-GR; VITYAZ5971-GR; VITYAZ5972-TR; VITYAZ5975-GR; VITYAZ5975-PH; VITYAZ5977-PH; VITYAZ5982-GR; VITYAZ5982-PH; VITYAZ5983-GR; VITYAZ5983-PH; VITYAZ5984-GR; VITYAZ5984-PH; VITYAZ5987-GR; VITYAZ5988-11-GR; VITYAZ5988-12-GR; VITYAZ5988-13-GR; VITYAZ5988-14-GC; VITYAZ5988-16-GR; VITYAZ5988-19-TR; VITYAZ5988-20-GR; VITYAZ5988-21-GR; VITYAZ5988-22-GR; VITYAZ5988-24-GR; VITYAZ5988-25-GR; VITYAZ5988-2-GC; VITYAZ5988-4-TR; VITYAZ5988-5-GR; VITYAZ5988-7-GR; VITYAZ5988-9-GR; VITYAZ5993-GR; VITYAZ5995-GR; VITYAZ5996-10-GR; VITYAZ5996-11-TR; VITYAZ5996-13-GR; VITYAZ5996-15-GR; VITYAZ5996-17-GR; VITYAZ5996-18-GR; VITYAZ5996-1-GR; VITYAZ5996-20-GR; VITYAZ5996-22-GR; VITYAZ5996-24-GC; VITYAZ5996-25-GR; VITYAZ5996-2-TR; VITYAZ5996-4-GR; VITYAZ5996-6-GR; VITYAZ6000-GC; VITYAZ6002-11-GC; VITYAZ6002-12-DR; VITYAZ6002-17-GC; VITYAZ6002-20-GC; VITYAZ6002-21-DR; VITYAZ6002-24; VITYAZ6004-GC; VITYAZ6005-GC; VITYAZ6005-GR; VITYAZ6006-GR; VITYAZ6008; VITYAZ6009-GR; VITYAZ6011-GR; VITYAZ6012-GR; VITYAZ6013-GR; VITYAZ6014-GR; VITYAZ6015-GR; VITYAZ6015-PH; VITYAZ6015-TR; VITYAZ6016-GR; VITYAZ6017-DR; VITYAZ6165-GR-1; VITYAZ6167-GR; VITYAZ6168-GR; VITYAZ6172-GR; VITYAZ6174-GR; VITYAZ6177-GR; VITYAZ6243-GR; VITYAZ6255-GR; VITYAZ6256-GR; VITYAZ6257-GR; VITYAZ6264-GR; VITYAZ6265-DR; VITYAZ6267-GR; VITYAZ6270-DR; VITYAZ6272-GR; VITYAZ6273-GR; VITYAZ6275-11-GR; VITYAZ6275-15-TR; VITYAZ6275-2-TR; VITYAZ6275-3-GR; VITYAZ6275-5-GC; VITYAZ6275-8-TR; VITYAZ6277-3-GC; VITYAZ6277-4-TR; VITYAZ6297-TR; VITYAZ6298-10-GC; VITYAZ6298-12-GR; VITYAZ6298-13-TR; VITYAZ6298-14-GC; VITYAZ6298-18-GR; VITYAZ6298-19-GC; VITYAZ6298-1-GC; VITYAZ6298-20-TR; VITYAZ6298-24-TR; VITYAZ6298-26-GR; VITYAZ6298-28-GC; VITYAZ6298-2-GR; VITYAZ6298-30-TR; VITYAZ6298-31-GC; VITYAZ6298-33-GC; VITYAZ6298-34-GR; VITYAZ6298-35-TR; VITYAZ6298-36-GR; VITYAZ6298-37-TR; VITYAZ6298-40-TR; VITYAZ6298-42-GC; VITYAZ6298-43-GR; VITYAZ6298-45-GC; VITYAZ6298-46-GR; VITYAZ6298-47-GC; VITYAZ6298-48-GR; VITYAZ6298-49-GC; VITYAZ6298-50-GR; VITYAZ6298-51-GC; VITYAZ6298-52A-TR; VITYAZ6298-53-TR; VITYAZ6298-56-TR; VITYAZ6298-57-GC; VITYAZ6298-58; VITYAZ6298-62-TR; VITYAZ6298-7-TR; VITYAZ6298-8-GR; VITYAZ6298-9-GR; VITYAZ6299-TR; VITYAZ6300-TR; VITYAZ6307-TR; VITYAZ6331; VITYAZ6332-GR; VITYAZ6333-10-TR; VITYAZ6333-11-GR; VITYAZ6333-13-TR; VITYAZ6333-20; VITYAZ6333-22-GC; VITYAZ6333-23-TR; VITYAZ6333-26-GC; VITYAZ6333-2-TR; VITYAZ6333-3-GC; VITYAZ6333-5-GC; VITYAZ6333-7-GC; VITYAZ6333-8-GC; VITYAZ6334-GR; VITYAZ6335-GC; VITYAZ6339-GC; VITYAZ6343-TR; VITYAZ6344-TR; VITYAZ6348-TR; VITYAZ6352-TR; VITYAZ6356-TR; VITYAZ6358-TR; VITYAZ6359-TR; VITYAZ6360-TR; VITYAZ6364-TR; VITYAZ6365-TR; VITYAZ6366-DR; VITYAZ6367-DR; VITYAZ6368-DR; VITYAZ6369-DR; VITYAZ6405-PH; VITYAZ6408-PH; VITYAZ6704-GC; VITYAZ6706-DR; VITYAZ6817-GR; VITYAZ6818-TR; VITYAZ6819-TR; VITYAZ6821-GR; VITYAZ6822-DR; VITYAZ6824-GR; VITYAZ6825-GR; VITYAZ6826-GR; Vityaz Trench, Pacific Ocean
    Type: Dataset
    Format: application/zip, 14 datasets
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  • 6
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    PANGAEA
    In:  Supplement to: Winterer, Edward L; Riedel, William R; Moberly, Ralph; Resig, Johanna M; Kroenke, Loren W; Gealy, E L; Heath, G Ross; Bronnimann, P; Martini, E; Worsley, Thomas R (1971): Site 61. In: Winterer, E.L.; et al., Initial Reports of the Deep Sea Drilling Project, 7, Initial Reports of the Deep Sea Drilling Project, 7, U.S. Government Printing Office, VII, 27-47, https://doi.org/10.2973/dsdp.proc.7.103.1971
    Publication Date: 2023-08-28
    Description: The results at Site 59 suggested that Mesozoic sediments are present beneath a thin Tertiary cover in the region north of the Caroline Ridge near the Mariana Trench. Since one of the principal objectives of the drilling program was to find old Pacific crust, and since the section at Site 59 was not fully penetrated, it seemed worth a determined effort to go beyond the level reached at Site 59, somewhere in the same general area, in an attempt to reach basement. As the reflection profile taken by Argo (SCAN Leg V) through Site 59 shows the section above thesmooth basement reflector (Horizon B?) thinning northwestward from about 0.3 to 0.15 second, by loss of part of the lower "transparent" layer, this is were Site 61 was located.
    Keywords: 7-61; Comment; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; Glomar Challenger; Identification; Leg7; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 9 data points
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  • 7
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Winterer, Edward L; Riedel, William R; Moberly, Ralph; Resig, Johanna M; Kroenke, Loren W; Gealy, E L; Heath, G Ross; Bronnimann, P; Martini, E; Worsley, Thomas R (1971): Site 63. In: Winterer, E.L.; et al., Initial Reports of the Deep Sea Drilling Project, 7, Initial Reports of the Deep Sea Drilling Project, 7, U.S. Government Printing Office, VII, 323-472, https://doi.org/10.2973/dsdp.proc.7.105.1971
    Publication Date: 2023-08-28
    Description: The sedimentary section at Site 62 on Eauripik Ridge can be traced eastward into the East Caroline Basin. It was decided to drill a hole to basement in the eastern part of East Caroline Basin to determine the age of the upper strong reflectors and to test the hypothesis that sediments older than any at Site 62 are present. A nearly complete section was obtained from middle Oligocene to Quaternary, unconformably overlying basalt containing middle Oligocene chalk xenoliths. The sediments consist of chalk and chalk ooze in the Oligocene and Miocene, and of marl ooze and calcareous clay in the Pliocene and Quaternary.
    Keywords: 7-63; 7-63A; 7-63B; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg7; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/BASIN; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 33 data points
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  • 8
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    Unknown
    PANGAEA
    In:  Supplement to: Winterer, Edward L; Riedel, William R; Moberly, Ralph; Resig, Johanna M; Kroenke, Loren W; Gealy, E L; Heath, G Ross; Bronnimann, P; Martini, E; Worsley, Thomas R (1971): Site 67. In: Winterer, E.L.; et al., Initial Reports of the Deep Sea Drilling Project, 7, Initial Reports of the Deep Sea Drilling Project, 7, U.S. Government Printing Office, VII, 821-841, https://doi.org/10.2973/dsdp.proc.7.109.1971
    Publication Date: 2023-08-28
    Description: Site 67 is on the Hawaiian Arch, in the general region selected for one of the Mohole Project sites. Therefore, intensive geophysical surveys have been made in the area. The objectives were to penetrate the entire sedimentary sequence to basement in order to learn the petrology and ages of the sediments and of the seismic reflectors, and to obtain samples of the underlying basement rocks. Well consolidated and bedded volcanic sandstone and mudstone, and claystone were found to extend from the sea floor to a depth of 60 meters, where a layer of hard brown porcelanite stopped the bit. Displaced radiolarians in mud from a core at 60 meters indicate sediments of early Eocene or late Paleocene age are present somewhere above that depth.
    Keywords: 7-67; 7-67A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg7; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific; Position; Quantity of deposit; Sample code/label; Sediment type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 15 data points
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  • 9
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    Unknown
    PANGAEA
    In:  Supplement to: Winterer, Edward L; Riedel, William R; Moberly, Ralph; Resig, Johanna M; Kroenke, Loren W; Gealy, E L; Heath, G Ross; Bronnimann, P; Martini, E; Worsley, Thomas R (1971): Site 65. In: Winterer, E.L.; et al., Initial Reports of the Deep Sea Drilling Project, 7, Initial Reports of the Deep Sea Drilling Project, 7, U.S. Government Printing Office, VII, 607-723, https://doi.org/10.2973/dsdp.proc.7.107.1971
    Publication Date: 2023-08-28
    Description: An acoustically very transparent layer is present over much of the deep basin—here termed the Central Basin—between the Gilbert and Marshall Islands on the west and the Line Islands on the east. The Pacific Panel recommended drilling in this region to sample at least the upper transparent layer, and the first opaque layer beneath. Several possible sites were considered by the panel and by the shipboard party. Of paramount importance in choosing a particular site was a concern that sufficient sediments be present to bury the bottom-hole assembly (the drill collars and bumper subs) before the bit struck hard rock. A set of nearly continuous cores of an apparently uninterrupted section of radiolarian ooze ranging in age from middle Eocene to Recent was obtained, but the bit did not reach the deepest seismic reflector. Below depths of 127 meters, in the Oligocene and Eocene, thin chert and turbidite beds are sparsely interbedded with ooze.
    Keywords: 7-65; 7-65A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg7; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/BASIN; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 41 data points
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  • 10
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Winterer, Edward L; Riedel, William R; Moberly, Ralph; Resig, Johanna M; Kroenke, Loren W; Gealy, E L; Heath, G Ross; Bronnimann, P; Martini, E; Worsley, Thomas R (1971): Site 66. In: Winterer, E.L.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, VII, 725-819, https://doi.org/10.2973/dsdp.proc.7.108.1971
    Publication Date: 2023-08-28
    Description: One of the principal objectives in the Central Pacific Basin was to elucidate the Paleobathymetric history of the region, which is located amidst groups of atolls and guyots that have subsided as much as 2 kilometers since mid-Cretaceous times. After failure to penetrate the entire sedimentary section and to sample basement at Site 65, on the west side of the Central Basin another site in the Basin where basement rocks might be sampled was searched. Likely places were known from unpublished reflection profiles on the east side of the Basin near the Line Islands by the Hawaii Institute of Geophysics. Finally it was decided to drill a transparent section once again in this area acoiding turbidites formations.
    Keywords: 7-66; 7-66A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg7; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/BASIN; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 67 data points
    Location Call Number Expected Availability
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