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  • Wiley-Blackwell  (2,239)
  • Society of Economic Geologists (SEG)
  • PANGAEA
  • 1970-1974  (2,179)
  • 1935-1939  (103)
Collection
Years
Year
  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Doyle, Patricia S; Boltovskoy, Esteban; Herb, Rene C; Thierstein, Hans R; Hyndman, Roy D; Horvath, George J; Leidy, Rosanne D; McKelvey, Barrie C; Kempe, D R C; Rodolfo, Kelvin S; Davies, Thomas A; Luyendyk, Bruce P (1974): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXVI, 1129 pp, https://doi.org/10.2973/dsdp.proc.26.1974
    Publication Date: 2023-08-28
    Description: DSDP Leg 26, is the fifth cruise of D/V Glomar Challenger in the Indian Ocean, and the first cruise of Phase III of the Deep Sea Drilling Project. The Indian Ocean is the smallest of the three major ocean basins but appears to be geologically the most complex. The sites drilled on Leg 26 were selected to try to elucidate a number of specific problems of both local and broad regional significance, as well as to add to the general knowledge of the area. In particular: a) To locate the oldest sediment in the Indian Ocean and thus possibly the date of the initial breakup of Gondwanaland (Sites 250, 256, 257); b) To determine the effects of the initiation of the Circumpolar Current on southern Indian Ocean sedimentation (Sites 250, 252, 256, 257, 258); c) To determine the history of spreading of the Southwest Branch of the Indian Ocean Ridge and the history of the crust and oceanic sedimentation in that general region (Sites 250, 251, 252).
    Keywords: 26-250A; 26-252; 26-256; 26-257; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Indian Ocean//BASIN; Leg26; 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, 42 data points
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  • 2
    ISSN: 0933-5137
    Keywords: Chemistry ; Polymer and Materials Science
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 0018-019X
    Keywords: Chemistry ; Organic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Notes: The structure II of boromycin C45H74BNO15 (cf. [2]) has been established by combination of chemical evidence with X-ray analysis. The antibiotic is a D-valine ester of a Böeseken-complex of boric acid with a macrodiolide of a new type.
    Additional Material: 1 Tab.
    Type of Medium: Electronic Resource
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  • 4
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    PANGAEA
    In:  Supplement to: Andrews, James E; Callender, Edward; Bowser, Carl J; Mero, John L; Gauthier, Michel; Meylan, Maurice A; Craig, James D; Binder, Kenneth; Volk, Patrick; Chave, Alan D; Bachman, Walter (1974): Ferromanganese deposits of the ocean floor. Cruise Report Mn-74-01, R/V Moana Wave, Honolulu to San Diego, 17 July - 10 August 1974. Hawaii Institute of Geophysics, University of Hawaii, Technical Report, 9, 194 pp, https://download.pangaea.de/reference/86495/attachments/08025001_Indexed.pdf
    Publication Date: 2023-08-28
    Description: Cruise MN-74-01 of the R/V Moana Wave was the first part of the field work of the NSF-IDOE Inter-University Ferromanganese Research Program in 1974. This program was designed to investigate the origin, growth, and distribution of copper/nickel-rich manganese nodules in the Pacific Ocean. The field effort was designed to satisfy sample requirements of the 15 principal investigators, while increasing general knowledge of the copper/nickel-rich nodule deposits of the equatorial Pacific. This report is the first of a series of cruise reports designed to assist sample requests for documented nodules, sediment, and water samples so the laboratory results can be realistically compared and related to the environment of nodule growth.
    Keywords: BC; Box corer; Comment; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; Event label; FFC; FFGR; Free fall corer; Free-fall grab; Latitude of event; Longitude of event; Mass; Mn-74-01-001-FFG-001; Mn-74-01-001-FFG-002; Mn-74-01-001-FFG-003; Mn-74-01-002-FFG-004; Mn-74-01-002-FFG-005; Mn-74-01-002-FFG-006; Mn-74-01-003-FFG-007; Mn-74-01-003-FFG-009; Mn-74-01-004-FFG-010; Mn-74-01-004-FFG-011; Mn-74-01-004-FFG-012; Mn-74-01-005-B2; Mn-74-01-005-FFG-014; Mn-74-01-005-FFG-015; Mn-74-01-006-C5; Mn-74-01-006-FFC-027; Mn-74-01-006-FFG-016; Mn-74-01-006-FFG-017; Mn-74-01-006-FFG-018; Mn-74-01-006-FFG-019; Mn-74-01-006-FFG-020; Mn-74-01-006-FFG-021; Mn-74-01-006-FFG-022; Mn-74-01-006-FFG-023; Mn-74-01-006-FFG-024; Mn-74-01-006-FFG-025; Mn-74-01-006-FFG-026; Mn-74-01-006-FFG-027; Mn-74-01-007-FFG-028; Mn-74-01-007-FFG-029; Mn-74-01-007-FFG-030; Mn-74-01-008-D1; Mn-74-01-008-FFG-032; Mn-74-01-008-FFG-033; Mn-74-01-009-FFG-034; Mn-74-01-009-FFG-036; Mn-74-01-010-FFG-037; Mn-74-01-010-FFG-038; Mn-74-01-010-FFG-039; Mn-74-01-010-FFG-040; Mn-74-01-010-FFG-042; Mn-74-01-010-FFG-043; Mn-74-01-011-FFG-045; Mn-74-01-011-FFG-046; Mn-74-01-011-FFG-047; Mn-74-01 IODE; Moana Wave; MW7401; MW7401-01G01; MW7401-01G02; MW7401-01G03; MW7401-02G04; MW7401-02G05; MW7401-02G06; MW7401-03G07; MW7401-03G09; MW7401-04G10; MW7401-04G11; MW7401-04G12; MW7401-05B02; MW7401-05G14; MW7401-05G15; MW7401-06C05; MW7401-06C07; MW7401-06G16; MW7401-06G17; MW7401-06G18; MW7401-06G19; MW7401-06G20; MW7401-06G21; MW7401-06G22; MW7401-06G23; MW7401-06G24; MW7401-06G25; MW7401-06G26; MW7401-06G27; MW7401-07G28; MW7401-07G29; MW7401-07G30; MW7401-08D01; MW7401-08G32; MW7401-08G33; MW7401-09G34; MW7401-09G36; MW7401-10G37; MW7401-10G38; MW7401-10G39; MW7401-10G40; MW7401-10G42; MW7401-10G43; MW7401-11G45; MW7401-11G46; MW7401-11G47; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Nodules, mass abundance; Number; Pacific Ocean; Position; Quantity of deposit; Sample ID; Sediment type; Shape; Substrate type; Surface description
    Type: Dataset
    Format: text/tab-separated-values, 845 data points
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  • 5
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    Unknown
    PANGAEA
    In:  Supplement to: Hays, J D; Cook, Harry E III; Jenkins, D Graham; Cook, F M; Fuller, J T; Goll, Robert M; Milow, E Dean; Orr, W N (1972): Site 76. In: Hays, J.D.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, 9, U.S. Government Printing Office, IX, 21-41, https://doi.org/10.2973/dsdp.proc.9.102.1972
    Publication Date: 2023-08-28
    Description: Site 76 was selected in order to core a thick sequence of sediments north of the Tuamotu ridge that had been crossed by Glomar Challenger justprior to the termination of Leg 8 in Tahiti. Two holes at this site continuously cored 27 meters of lower Pliocene to Recent phillipsitic clay and calcareous nannofossil ooze interbedded with calcareous turbidites. The drill bit was stopped by a silicified calcareous turbidite of Early Pliocene age.
    Keywords: 9-76; 9-76A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg9; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; South Pacific/PLAIN; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 16 data points
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  • 6
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    Unknown
    PANGAEA
    In:  Supplement to: Hays, J D; Cook, Harry E III; Jenkins, D Graham; Cook, F M; Fuller, J T; Goll, Robert M; Milow, E Dean; Orr, W N (1972): Site 79. In: Hays, J.D.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, 9, U.S. Government Printing Office, IX, 317-400, https://doi.org/10.2973/dsdp.proc.9.105.1972
    Publication Date: 2023-08-28
    Description: Site 79 is located on the crest of the equatorial Pacific sediment belt (Ewing and others, 1968) and is the westernmost of a series of sites (79, 81, 82 and 83) that follow the crest of this belt eastward to and across the crest of the oceanic ridge, locally known as the East Pacific Rise. The purpose of these sites is two-fold: 1) to study variations in biostratigraphy and sediment type from west to east across the Pacific and 2) to paleontologically date basement and determine the rate of spreading of the Pacific plate since the time of deposition of the oldest sediments at Site 77.
    Keywords: 9-79; 9-79A; Comment; Deep Sea Drilling Project; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg9; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/VALLEY; Position; Quantity of deposit; Sample code/label; Sediment type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 7
    ISSN: 0360-6376
    Keywords: Physics ; Polymer and Materials Science
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Notes: Polyperfluorobut-2-yne is prepared by a fluoride ion-induced polymerization of hexafluorobut-2-yne. The mass spectrum indicates a regular fragmentation pattern but the ESCA spectrum establishes the structure as a polyene, rather than a crosslinked system, and the occurrence of a shake-up peak assists in this assignment.
    Additional Material: 3 Ill.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    New York, NY [u.a.] : Wiley-Blackwell
    Journal of Applied Polymer Science 18 (1974), S. 3543-3553 
    ISSN: 0021-8995
    Keywords: Chemistry ; Polymer and Materials Science
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics , Physics
    Notes: An analytical procedure for determining the antioxidant (i.e., Akroflex CD) content in neoprene rubber has been developed. The method is based on the infrared absorption analyses of chloroform extractables from the cured rubber at 1600 cm-1 and 1300 cm-1. Good agreement is found between these two independent sets of measurements. In an attempt to elucidate the antioxidant loss mechanism found with neoprene, thermal aging studies were carried out over the temperature range of 80°-200°C. Using the infrared analytical procedure, antioxidant loss rates at the different temperatures were established. The activation energy value (5.1 kcal/mole) for the loss rate as well as other aging data suggest that the antioxidant is lost by a diffusion mechanism.
    Additional Material: 9 Ill.
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  • 9
    Electronic Resource
    Electronic Resource
    New York, NY [u.a.] : Wiley-Blackwell
    Journal of Applied Polymer Science 16 (1972), S. 3353-3360 
    ISSN: 0021-8995
    Keywords: Chemistry ; Polymer and Materials Science
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics , Physics
    Notes: Two independently derived distribution function methods validate both the calibration curve and the dispersion correction of the “effective linear calibration” method used in gel permeation chromatography (GPC). Experimental conditions are specified for making the method more useful by permitting linear extrapolation of the calibration line, \documentclass{article}\pagestyle{empty}\begin{document}$ V_R = C_1 + C_2 \log M, $\end{document} and for using a minimum number of standards. The independent methods quantitatively relate known differential of integral distribution functions for standard samples to their respective chromatograms. As such, they are useful calibration methods also, but are limited in scope and range.
    Additional Material: 5 Ill.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    New York, NY [u.a.] : Wiley-Blackwell
    Journal of Applied Polymer Science 17 (1973), S. 269-282 
    ISSN: 0021-8995
    Keywords: Chemistry ; Polymer and Materials Science
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics , Physics
    Notes: The development of gel permeation chromatography (GPC) has provided a convenient tool for the rapid determination of molecular weight distribution. The question has arisen as to the suitability of the method for specification purposes. The present work, suggested by the Naval Air Systems Command, represents an attempt to assess the precision of the method through a series of tests carried out by a number of laboratories using identical procedures on the same samples. Ten laboratories agreed to take part. Naval Ordnance Station, Indian Head, worked out standard conditions for operation of the chromatograph, for calibration of the columns, and for analysis of the GPC curves. Two samples of polystyrene were used by the various organizations for calibration of their instruments. Number-average molecular weight, heterogeneity index, and cumulative molecular weight distribution curves were determined on four samples of carboxyl-terminated polybutadiene (CTPB) and two samples of hydroxyl-terminated polybutadiene (HTPB), all unidentified except by letter code. All laboratories used identical directions for setting up CTPB and HTPB calibration curves which were based on curves determined from vapor-pressure osmometer molecular weights and GPC count numbers of fractionated material. Variation among the different laboratories was 0.15 in heterogeneity index, and a maximum of 1200 in molecular weight provided one aberrant set of values was eliminated. The six samples had heterogeneity indices from 1.15 to 1.54, while molecular weight varied from approximately 3000 to 6000. The average coefficient of variation of the molecular weight values was 6.2 ± 0.7%, which is quite acceptable. Variation in heterogeneity index was too great for specification purposes when considered among the different laboratories, but may be sufficiently good when measured by any one laboratory.
    Additional Material: 7 Ill.
    Type of Medium: Electronic Resource
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