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  • Data  (45)
  • 1950-1954  (45)
Collection
Publisher
Years
Year
  • 1
    Publication Date: 2019-04-30
    Type: Dataset
    Format: text/tab-separated-values, 40 data points
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  • 2
    Publication Date: 2019-04-30
    Type: Dataset
    Format: text/tab-separated-values, 77 data points
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  • 3
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    In:  Supplement to: Lamont-Doherty Earth Observatory (1954): Expedition VEMA 3. Lamont Geological Observatory, Columbia University, New York, unpublished, 11 pp, http://www.ngdc.noaa.gov/mgg/geology/data/vema/vm03/vm03_summary.pdf
    Publication Date: 2018-09-27
    Description: The cores and dredges described in this report were taken during the VEMA 3 Expedition from January 1957 until June 1954 by the Lamont Geological Observatory, Columbia University from the R/V Vema. A total of 160 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Type: Dataset
    Format: text/tab-separated-values, 83 data points
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  • 4
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    In:  Supplement to: Goldberg, Edward D (1954): Marine Geochemistry 1. Chemical Scavengers of the Sea. The Journal of Geology, 62(3), 249-265, http://www.jstor.org/stable/30080120
    Publication Date: 2019-04-16
    Description: The ability of the hydrated oxides of manganese and iron to adsorb ions from solution (scavenging) is considered in relation to some problems in marine geology, chemistry, and biology. In the ferruginous sediments of the Pacific Ocean, iron oxides are accompanied by titanium, cobalt, and zirconium in amounts proportional to the iron content. Similarly, copper and nickel are linearly related to the manganese content. These observations are explained on the basis of scavenging. An electrochemical theory for the formation of manganese nodules is presented. Marine sediments are classified on the basis of the geosphere in which the solid phases originate. The distribution of certain ionic species in sea water between the solid and aqueous phases is considered on the basis of scavenging and co-ordination compound theory. The concentration of minor elements by members of the marine biosphere is explained either by the direct uptake of the element or by the uptake of iron or manganese oxides with the accompanying scavenged element.
    Type: Dataset
    Format: text/tab-separated-values, 118 data points
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  • 5
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    In:  Supplement to: Lamont-Doherty Earth Observatory (1954): Expedition VEMA 5. Lamont Geological Observatory, Columbia University, New York, unpublished, 7 pp, http://www.ngdc.noaa.gov/mgg/curator/data/vema/vm05/vm05_summary.pdf
    Publication Date: 2018-09-27
    Description: The cores and dredges described in this report were taken during the VEMA 5 Expedition from November until December 1954 by the Lamont Geological Observatory, Columbia University from the R/V Vema. A total of 48 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Type: Dataset
    Format: text/tab-separated-values, 83 data points
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  • 6
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    In:  Supplement to: Lamont-Doherty Earth Observatory (1954): Expedition VEMA 4. Lamont Geological Observatory, Columbia University, New York, unpublished, 8 pp, http://www.ngdc.noaa.gov/mgg/geology/data/vema/vm04/vm04_summary.pdf
    Publication Date: 2018-09-27
    Description: The cores and dredges described in this report were taken during the VEMA 4 Expedition from July until September 1954 by the Lamont Geological Observatory, Columbia University from the R/V Vema. A total of 54 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Type: Dataset
    Format: text/tab-separated-values, 45 data points
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  • 7
    Publication Date: 2019-04-30
    Type: Dataset
    Format: text/tab-separated-values, 61 data points
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  • 8
    Publication Date: 2019-04-30
    Type: Dataset
    Format: text/tab-separated-values, 7 data points
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  • 9
    Publication Date: 2019-04-30
    Type: Dataset
    Format: text/tab-separated-values, 42 data points
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  • 10
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    In:  Scripps Institution of Oceanography, UC San Diego
    Publication Date: 2018-09-27
    Type: Dataset
    Format: text/tab-separated-values, 29 data points
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  • 11
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    In:  Supplement to: Emiliani, Cesare (1954): Pleistocene temperature variations in the Mediterranean. Quarternaria, 2, 87-97
    Publication Date: 2019-01-26
    Description: For temperature investigations, a core in the Mediterranean Sea (No 189 of the Swedish Deep-Sea Expedition 1947-1948) was sampled at approximately 10 m intervals. Globigerina dubia, G. inflata and Globigerinoides rubra were seperated from each sample and their test were investigated for stable oxygen isotopic measurement. Oxygen isotopic analysis showed the following: 1) Ten stages are indicated. 2) The temperature minimum of stage 2 corresponds to a racliocarbon age of 17,200 years. 3) Temperature maxima of odd stages are about equal to the modern August mean, except that of stage 5 which is considerably higher and, probably reflects the influx of ice melt water. 4) Temperature minima of even stages are all very low, especially that of stage 2, and reflect conditions similar to those now prevailing around Newfoundland. 5) The temperature record indicates that during most of the time covered by the core, the Mediterranean was cooler than at present and that conditions similar to the present occurred only during comparatively short intervals. 6) Minor temperature fluctuations occur, especially in the warmer stages, which are of doubtful significance. 7) An average rate of sedimentation of 4.3 cm/1000 years is indicated for the whole core.
    Type: Dataset
    Format: text/tab-separated-values, 121 data points
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  • 12
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    In:  Supplement to: Brockmann, Christoph (1954): Die Diatomeen in den Ablagerungen der ostpreußischen Haffe. Meyniana, 3, 1-95, https://doi.org/10.2312/meyniana.1954.3.1
    Publication Date: 2019-02-13
    Description: Als man nach dem ersten Weltkrieg im verkleinerten Deutschland nach der Möglichkeit von Neulandgewinnung suchte, dachte man auch an eineTrockenlegung der ostpreußischen Haffe. Aus diesem Anlaß wurden umfangreiche Bohrungen ausgeführt, um ein möglichst genaues Bild vom Untergrunde der Haffe zu bekommen. Auf Veranlassung der Preußischen Geologischen Landesanstalt wurde ich mit der Untersuchung der Diatomeen in den Bohrproben beauftragt. Die Arbeit wurde 1934 begonnen und Ende 1937 wurde der letzte Arbeitsbericht abgeliefert. Die beabsichtigte Veröffentlichung ist bisher unterblieben, weil die Druckvorlagen später verloren gegangen sind. Seitdem sind über die Haffuntersuchungen mehrere Teilergebnisse veröffentlicht worden, von denen hier schon wegen der Terminologie die pollenanalytischen Arbeiten von L. HEIN (1941) und HUGO GROSS (1941) erwähnt seien, auf die im Abschnitt Il 2e näher eingegangen wird. Bei der geologischen Auswertung war Zurückhaltung geboten; denn es wäre gewagt, allein aus der Perspektive der Diatomeenforschung endgültige Aussagen machen zu wollen. Darum habe ich mich bemüht, das Material so weit aufzuschließen, daß es Geologen später auch bei veränderter Fragestellung auswerten können. "Die Theorien wechseln, aber die Tatsachen bleiben." Der Initiative des Herrn Prof. Dr. K. GRIPP und der finanziellen Hilfe der Deutschen Forschungsgemeinschaft ist es zu verdanken, daß die vorliegende Arbeit im Druck erscheinen kann. Zusammenfassung 1. Nur in den alluvialen Schichten des Kurischen Haffs wurden Diatomeen gefunden. 2. Die Diatomeenflora des Kurischen Haffs besteht zur Hauptsache aus Süßwasserformen. 3. Salzwasserformen finden sich in allen Schichten verstreut unter der Süßwasserflora. Wenn sie auch nach Zahl der Arten in manchen Proben einen erheblichen Prozentsatz der Flora ausmachen, so ist doch die Zahl der Individuen stets so gering, daß man nirgends von einer Brackwasserflora sprechen kann. 4. Die Süßwasserflora besteht in den unteren Schichten vorwiegend aus Grundformen; und zwar machen die epiphytischen Bewohner flacher Sumpfgewässer einen großen Teil der Flora aus. 5. In einzelnen Bohrungen kommt in den untersten alluvialen Schichten eine Grundflora mit zahlreichen Mastogloien vor. Dies sind die ältesten diatomeenführenden Schichten, entstanden in isolierten Sumpfgewässern. 6. Die übrigen Schichten mit überwiegender Grundflora sind vermutlich Ablagerungen der Ancyluszeit. 7. Die oberen Schichten, in denen die Planktondiatomeen überwiegen, dürften größtenteils der Litorina-Transgressionszeit angehören, jedoch ist der Transgressions-Kontakt nicht klar zu erkennen. 8. Das Ende der Litorinazeit ist noch weniger erkennbar, da eine grundsätzliche Veränderung der Flora nach oben nicht zu beobachten ist. 9. Die ostbaltischen Charakterformen sind in allen Schichten vertreten.
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 13
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    In:  Supplement to: Young, Edward J (1954): Studies of trace elements in sediments. Massachusetts Intitute of Technology, Boston, Massachusetts, U.S.A., Dissertation, 137 pp, hdl:1721.1/58047
    Publication Date: 2019-06-14
    Description: By means of spectrographic analysis 96 samples of marine sediments were analyzed quantitatively for V, Ti, Zr, Co, Ni, Sc, Cr, and La, and semi-quantitatively for Ba and Sr. Ca has been estimated by visual comparison of spectrographic plates, and several Fe values have also been determined in the same way. Geographically 40 of these samples are from the Pacific Ocean basin, one of which is a manganese nodule, 21 from the Gulf of Mexico, 11 from Atchafalaya Bay, 8 from American Devonian to Miocene sedimentary rocks, 4 from the Mississippi Delta, 3 from the San Diego trough, 3 from off Grand Isle, 3 from Lake Pontchartrain, from Bay Rambour, 1 from Laguna Madre off the Texas coast, and 1 from the Guadalupe River, Texas. The afore-mentioned elements were sought using PdCl2 as an internal standard, after the method developed by Ahrens (1950) and his co-workers. Samples were run in duplicate, and standard deviations varied from 5 to 14 percent. Working curves, from which final values were obtained, were constructed with the use of standard granite, G1, and the standard diabase, W1, as standards. See Fairbairn and others (1951). An experiment was carried out to determine the effect of matrix change, involving CaCO3, on the spectral line intensities of the quantitatively analyzed elements. The distribution of each of the elements is discussed separately, and particular emphasis is given to oceanic "red clay", in which many elements are enriched. A general discussion is given to mineralogy of the sediments, cation exchange in its bearing on this thesis, and a brief recount of the two hypotheses of origin of oceanic "red clay". An application of the findings of this thesis to aid in the choice of the more likely hypothesis is made.
    Type: Dataset
    Format: text/tab-separated-values, 15 data points
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  • 14
    Publication Date: 2019-10-28
    Type: Dataset
    Format: text/tab-separated-values, 1541 data points
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  • 15
    Publication Date: 2019-10-28
    Type: Dataset
    Format: text/tab-separated-values, 17584 data points
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  • 16
    Publication Date: 2019-10-28
    Type: Dataset
    Format: text/tab-separated-values, 2555 data points
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  • 17
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    In:  Supplement to: Kühn, Arthur (1953): Forschungsreise der 'Discovery 11' im Südlichen Eismeer 1950/51. Polarforschung, 23(1/2), 259, hdl:10013/epic.29130.d001
    Publication Date: 2019-04-30
    Description: Die zwei Südwinter und einen Südsommer umspannende Expedition erbrachte so umfangreiche Ergebnisse, daß mit deren Veröffentlichung erst in Jahren gerechnet werden kann. Aus der Fülle der Beobachtungen und Messungen seien herausgegriffen: der wechselnde Verlauf der Packeisgrenze der Antarktis.
    Type: Dataset
    Format: text/tab-separated-values, 9 data points
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  • 18
    Publication Date: 2019-04-30
    Type: Dataset
    Format: text/tab-separated-values, 39 data points
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  • 19
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    In:  Supplement to: Lamont-Doherty Earth Observatory (1953): R/V Atlantis Cruise 185 - Descriptions of Cores. Lamont Geological Observatory, Columbia University, New York, unpublished
    Publication Date: 2019-01-29
    Description: The cores described were taken by the personnel of the Lamont-Doherty Earth Observatory (LDEO) operating as guests scientists during the R/V Atlantis Cruise 185 undertaken by the Woods Hole Oceanographic Institution from April until June 1953. A total of 65 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Type: Dataset
    Format: text/tab-separated-values, 43 data points
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  • 20
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    In:  Supplement to: Kröll, Victor (1953): Vertical Distribution of Radium in Deep-Sea Sediments. Nature, 171(4356), 742-742, https://doi.org/10.1038/171742a0
    Publication Date: 2018-09-27
    Description: The surprisingly high content of radium in certain deep-sea sediments discovered nearly fifty years ago by J. Joly remained unexplained until 1937, when H. Pettersson suggested an ocean-wide precipitation of ionium from sea water on to the ocean bottom as its origin. Extensive radium measurements on deep-sea cores raised by the Swedish Deep-Sea Expedition carried out in this institute by Pettersson, T. Bernert and me did not confirm the regular vertical distribution of radium reported by other workers. An expected rise in radium content from moderate values in the uppermost surface layers to a maximum corresponding to a radioactive equilibrium between precipitated ionium and ionium-supported radium generally occurred; but the maximum was not followed by the theoretical exponential decline downwards governed by the rate of decay of ionium, to 50 per cent in 83,000 years, to 25 per cent in 166,000 years, etc. Instead, a number of secondary maxima of radium content separated by equally pronounced minima were observed (see graph), which could not well be explained as due to intervening changes in the rate of total sedimentation. Another explanation offered was that ionium and radium are not in radioactive equilibrium; that is, the assumption underlying the use of measurements of radium as indicating the concentration in the same layer of its mother element is unjustified.
    Type: Dataset
    Format: text/tab-separated-values, 3 data points
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  • 21
    Publication Date: 2018-09-27
    Type: Dataset
    Format: text/tab-separated-values, 17 data points
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  • 22
    Publication Date: 2018-09-27
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 23
    Publication Date: 2019-04-16
    Type: Dataset
    Format: text/tab-separated-values, 20 data points
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  • 24
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    In:  Supplement to: Ljunggren, P (1953): Some Data concerning the Formation of Manganiferous and Ferriferous Bog Ores. Geologiska Föreningens i Stockholm förhandlingar, GFF (The transactions of the Geological Society of Sweden), 75(2), 277-297, https://doi.org/10.1080/11035895309454173
    Publication Date: 2019-02-13
    Description: In connection with a discovery of oxidic manganiferous and ferriferous precipitations in northern Vermland and north-western Dalecarlia, pH measurements of different waters and chemical analyses of waters and bog ores were carried out. The origin of the different bog ores is dealt with in connection with a discussion of some problems of the geochemistry of manganese and iron.
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 25
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    In:  Supplement to: Carsola, A J; Dietz, Robert S (1952): Submarine geology of two flat-topped northeast Pacific seamounts. American Journal of Science, 250(7), 481-497, https://doi.org/10.2475/ajs.250.7.481
    Publication Date: 2018-09-27
    Description: Erben and Fieberling Guyots lie about 800 and 600 miles, respectively, west of San Diego, California. Their tops are largely rocky. The sparse deposits consist of a thin patchy veneer of calcareous and siliceous organic remains and small amounts of clastic mineral grains and basalt fragments derived from the underlying rocks. The rocks of Erben Guyot are encrusted with manganese dioxide. Geomorphic and petrologic evidence indicate the seamounts to be extinct basaltic volcanoes. The drowned summit platforms of Erben Guyot (400 fathoms) and Fieberling Guyot (280 fathoms) are considered to be planes of marine abrasion cut by wave action within a few fathoms of sea level. Possible explanations are discussed for the present deeply drowned position of these truncated surfaces. It is concluded that these extinct submarine volcanoes constitute an uncompensated load on the earth's crust of such magnitude that they tend to subside slowly because of yielding of the earth's crust. Foraminifera of Miocene age have been identified in the calcareous cement of a breccia from the Erben Guyot surface. Thus, this guyot appears to have been truncated in Miocene or earlier time.
    Type: Dataset
    Format: text/tab-separated-values, 17 data points
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  • 26
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    In:  Supplement to: SCRIPPS Institution of Oceanography (1952): USS San Pablo Cruises 10 and 11 - Descriptions of Cores. Scripps Institution of Oceanography, UC San Diego, unpublished, 7 pp, http://www.ngdc.noaa.gov/mgg/curator/data/san_pablo/sp08/sp08-11_descriptions.pdf
    Publication Date: 2018-09-27
    Description: The cores described are taken during the USS San Pablo Cruises 10 and 11 in 1952 by the Scripps Institute of Oceanography. A total of 21 cores were recovered and are available at Scripps Institute of Oceanography for sampling and study.
    Type: Dataset
    Format: text/tab-separated-values, 63 data points
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  • 27
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    In:  Supplement to: Lamont-Doherty Earth Observatory (1952): R/V Atlantis Cruise 179 - Descriptions of Cores. Lamont Geological Observatory, Columbia University, New York, unpublished
    Publication Date: 2019-01-29
    Description: The cores described were taken by the personnel of the Lamont-Doherty Earth Observatory (LDEO) operating as guests scientists during the R/V Atlantis Cruise 179 undertaken by the Woods Hole Oceanographic Institution from April until May 1952. A total of 25 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Type: Dataset
    Format: text/tab-separated-values, 145 data points
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  • 28
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    Publication Date: 2018-09-27
    Description: Gelegentlich einer Diskussion über die Perioden der Polarlichterscheinungen und damit in Zusammenhang stehender Phänomene wurde die Meinung geäußert, daß die in verschiedenen Arbeiten abgeleiteten Perioden (insbesondere der Jahresgang der Nordlichthäufigkeit) möglicherweise nur örtlichen Charakter haben. Ich sah mich daher veranlaßt, bevor ich an eine zusammenfassende Darstellung des aus verschiedenen Gegenden der Nord- und Süd-Halbkugel stammenden Materials gehe, noch die aus Island und den Faer Oern vorliegenden Beobachtungen gesondert zu behandeln. Da die Bearbeitung nach dem gleichen Schema erfolgen kann wie die von mir in der "Polarforschung", Jahrgang 1948, veröffentlichte Arbeit über die in Grönland beobachteten Nordlichter, soll sie hier in stichwortartiger Kürze wiedergegeben werden.
    Type: Dataset
    Format: text/tab-separated-values, 66 data points
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  • 29
    Publication Date: 2019-04-30
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
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  • 30
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    In:  Supplement to: Lamont-Doherty Earth Observatory (1952): R/V Atlantis Cruise 180 - Descriptions of Cores. Lamont Geological Observatory, Columbia University, New York, unpublished
    Publication Date: 2019-01-29
    Description: The cores described were taken by the personnel of the Lamont-Doherty Earth Observatory (LDEO) operating as guests scientists during the R/V Atlantis Cruise 180 undertaken by the Woods Hole Oceanographic Institution from July until October 1952. A total of 118 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Type: Dataset
    Format: text/tab-separated-values, 182 data points
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  • 31
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    In:  Supplement to: SCRIPPS Institution of Oceanography (1952): CASCADIA Expedition 1952, List of cores and dredge samples copied from shipboard logs, Unpublished. (R/V Epce). Scripps Institution of Oceanography, UC San Diego, unpublished, 4 pp, http://www.ngdc.noaa.gov/mgg/curator/data/epce/cascadia/cascadia_ship_log.pdf
    Publication Date: 2018-09-27
    Description: The cores and dredges described in this report were taken on the CASCADIA Expedition in September 1952 by Scripps Institution of Oceanography from, the R/V Epce. A total of 14 cores and dredges were recovered and are available at Scripps for sampling and study. The coring sites are all in the eastern Pacific off the California coast.
    Type: Dataset
    Format: text/tab-separated-values, 22 data points
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  • 32
    Publication Date: 2019-04-30
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    Format: text/tab-separated-values, 20 data points
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  • 33
    Publication Date: 2018-09-27
    Description: The cores described in this report were taken on the NORTHERN HOLIDAY Expedition in August to September 1951 by the Scripps Institution of Oceanography from the R/V Horizon. A total of 19 cores and dredges were recovered and are available at Scripps for sampling and study.
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    Format: text/tab-separated-values, 108 data points
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  • 34
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    In:  Supplement to: Woods Hole Oceanographic Institution (1951): R/V Caryn Cruise 25 - Descriptions of Cores. unpublished, http://www.ngdc.noaa.gov/mgg/curator/data/caryn/c25/
    Publication Date: 2019-01-28
    Description: The cores described are taken during the R/V Caryn Cruise 25 in August-September 1951 by the Woods Hole Oceanographic Institution. A total of 11 cores were recovered and are available at Woods Hole Oceanographic Institution for sampling and study.
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    Format: text/tab-separated-values, 11 data points
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  • 35
    Publication Date: 2018-09-27
    Type: Dataset
    Format: text/tab-separated-values, 15537 data points
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  • 36
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    In:  Supplement to: Nybelin, Orvar (1951): Introduction and Station List. In: Pettersson, H. (Ed.), Jerlov, N. and Kullenberg, B. Reports of the Swedish Deep Sea Expedition, Volume II. Swedish Natural Science Research Council Stockholm 23 - Sweden, 1-28
    Publication Date: 2018-12-16
    Description: The cores and dredges described in this report were taken during the Swedish Deep Sea Expedition from July 1947 until October 1948 aboard the S/S Albatross (Boström). A total of 370 cores and trawls during this World circumnavigation.
    Type: Dataset
    Format: text/tab-separated-values, 276 data points
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  • 37
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    In:  Supplement to: Lamont-Doherty Earth Observatory (1951): R/V Atlantis Cruise 172 - Descriptions of Cores. Lamont Geological Observatory, Columbia University, New York, unpublished
    Publication Date: 2019-01-28
    Description: The cores described were taken by the personnel of the Lamont-Doherty Earth Observatory (LDEO) operating as guests scientists during the R/V Atlantis Cruise 172 undertaken by the Woods Hole Oceanographic Institution from April until June 1951. A total of 35 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Type: Dataset
    Format: text/tab-separated-values, 115 data points
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  • 38
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    In:  Supplement to: Lamont-Doherty Earth Observatory (1951): R/V Atlantis Cruise 167 - Descriptions of Cores. Lamont Geological Observatory, Columbia University, New York, unpublished
    Publication Date: 2019-01-28
    Description: The cores described were taken by the personnel of the Lamont-Doherty Earth Observatory (LDEO) operating as guests scientists during the R/V Atlantis Cruise 167 undertaken by the Woods Hole Oceanographic Institution in January 1951. A total of 55 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Type: Dataset
    Format: text/tab-separated-values, 72 data points
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  • 39
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    In:  Supplement to: Lamont-Doherty Earth Observatory (1950): R/V Atlantis Cruise 160 - Descriptions of Cores. Lamont Geological Observatory, Columbia University, New York, unpublished
    Publication Date: 2019-01-28
    Description: The cores described were taken by the personnel of the Lamont-Doherty Earth Observatory (LDEO) operating as guests scientists during the R/V Atlantis Cruise 160 undertaken by the Woods Hole Oceanographic Institution from Januray until April 1950. A total of 23 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Type: Dataset
    Format: text/tab-separated-values, 82 data points
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  • 40
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    In:  Supplement to: Lamont-Doherty Earth Observatory (1950): R/V Atlantis Cruise 164 - Descriptions of Cores. Lamont Geological Observatory, Columbia University, New York, unpublished
    Publication Date: 2019-01-28
    Description: The cores described were taken by the personnel of the Lamont-Doherty Earth Observatory (LDEO) operating as guests scientists during the R/V Atlantis Cruise 164 undertaken by the Woods Hole Oceanographic Institution from July until September 1950. A total of 63 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Type: Dataset
    Format: text/tab-separated-values, 51 data points
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  • 41
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    Unknown
    PANGAEA
    In:  Supplement to: Lamont-Doherty Earth Observatory (1950): RE05 Expedition, R/V Rehoboth, March 1950 - Preliminary Megascopic Descriptions of Split Cores. Lamont Geological Observatory, Columbia University, New York, unpublished, http://www.ngdc.noaa.gov/geosamples/cruise.jsp?cru=RE05&inst=&shp=Rehoboth
    Publication Date: 2019-01-28
    Description: The cores described in this list were taken on the RE05 Expedition in March 1950 by the Lamont-Doherty Earth Observatory from the R/V Rehoboth. A total of 13 cores were recovered and are available at LDEO for sampling and study.
    Type: Dataset
    Format: text/tab-separated-values, 41 data points
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  • 42
    Publication Date: 2019-04-30
    Type: Dataset
    Format: text/tab-separated-values, 18 data points
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  • 43
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Eythòrsson, Jòn (1950): Rückgang der isländischen Gletscher in den Jahren 1930-1947. Polarforschung, 20(1/2), 375, hdl:10013/epic.29052.d001
    Publication Date: 2018-09-27
    Description: Table without abstract.
    Type: Dataset
    Format: text/tab-separated-values, 822 data points
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  • 44
    Publication Date: 2018-12-16
    Description: The cores described in this report were taken on JAPANYON Expedition in June-September 1961 by Scripps Institution of Oceanography from, the R/V Spencer F. Baird. A total of 85 cores and dredges were recovered and are available at Scripps for sampling and study. The coring sites are all in the eastern tropical central Pacific.
    Type: Dataset
    Format: text/tab-separated-values, 250 data points
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  • 45
    Publication Date: 2018-12-16
    Description: The cores described in this report were taken on MIDPAC (Middle Pacific) Expedition in August-September 1950 by Scripps Institution of Oceanography from, the R/V Horizon. A total of 106 cores and dredges were recovered and are available at Scripps for sampling and study. The coring sites, all in the tropical central Pacific.
    Type: Dataset
    Format: text/tab-separated-values, 420 data points
    Location Call Number Expected Availability
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