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  • Data  (46)
  • 2010-2014
  • 1970-1974  (46)
  • 1945-1949
  • 1974  (14)
  • 1973  (32)
Collection
Source
Keywords
Publisher
Years
  • 2010-2014
  • 1970-1974  (46)
  • 1945-1949
Year
  • 1
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    Unknown
    Analysis of manganes deposits of Leg 23 (1974)
    PANGAEA
    In:  Supplement to: Whitmarsh, Robert B; Weser, Oscar E; Ross, David A; Syed, A; Boudreaux, J E; Coleman, R G; Fleisher, R L; Girdler, R W; Jipa, D; Kidd, Robert B; Mallik, Tapas Kumar; Manheim, Frank T; Matter, A; Nigrini, Catherine A; Siddiquie, H N; Stoffers, Peter; Supko, Peter R (1974): Site 221. In: Whitmarsh, R.B.; Weser, O.E.; Ross, D.A.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXIII, 167-210, https://doi.org/10.2973/dsdp.proc.23.105.1974
    Details
    Publication Date: 2023-08-28
    Description: Located on the Arabian Abyssal Plain near its southernmost termination, this site recorded continuous Middle Eocene through Pleistocene deep-water sedimentation above oceanic basalt. A chert layer is developed at the base of the Eocene strata. The Eocene through Miocene sequence shows the transition from biogenic ooze to brown clay sedimentation which typifies depositional sites as they move from a ridge crest to a deep-ridge flank position. Above this sequence is an undifferentiated Pliocene-Miocene through Pleistocene interval of terrigenous and calcareous turbidites. The former were derived from the Indus Canyon, and the latter from elsewhere.
    Keywords: 23-221; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Indian Ocean/Arabian Sea/PLAIN; Leg23; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 2
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    Unknown
    Annotated record of the detailed examination of Mn deposits from DSDP Leg 23 (Site 221) (1974)
    PANGAEA
    Details
    Publication Date: 2023-08-28
    Keywords: 23-221; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Identification; Indian Ocean/Arabian Sea/PLAIN; Leg23; 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, 16 data points
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  • 3
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    Unknown
    Chemical determinations of iron-manganese rich sediments, Sites 221, DSDP Leg 23 (1974)
    PANGAEA
    Details
    Publication Date: 2023-08-28
    Keywords: 23-221; Chromium; Copper; Deep Sea Drilling Project; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Identification; Indian Ocean/Arabian Sea/PLAIN; Iron; Leg23; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Sample code/label; Vanadium; Visual description; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 20 data points
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  • 4
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    Unknown
    Annotated record of the detailed examination of Mn deposits from DSDP Site 86, Leg 10 (Cores 86-8, 86-9) (1973)
    PANGAEA
    In:  Supplement to: Worzel, J Lamar; Bryant, W R; Beall, A O; Dickinson, K; Laury, R; Smith, L A; McNeely, B; Foreman, H P; Capo, R (1973): Site 86. In: Worzel, J.L.; Bryant, W.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, X, 25-47, https://doi.org/10.2973/dsdp.proc.10.103.1973
    Details
    Publication Date: 2023-08-28
    Description: The origin of the Campeche Escarpment in the Gulf of Mexico has been attributed to several causes. Some suggest that the scarp represents a fault scarp, others suggest that its origin is a function of upbuilding and outbuilding likened, in some cases, to that of delta building. Still others suggest that the scarp represents the detrital accumulation seaward of a barrier or reef complex. In order to clarify these possible interpretations, Site 86 was located on a bench at a depth of 780 fathoms in the vicinity of the Campeche Escarpment.
    Keywords: 10-86; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Gulf of Mexico/BENCH; Identification; Leg10; 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, 32 data points
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  • 5
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    Annotated record of the detailed examination of Mn deposits from DSDP Leg 26 (Sites 250A, 252, 256, 257) (1974)
    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
    Details
    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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  • 6
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    Unknown
    Distribution of diatom species as abundance estimates from vertical multinet hauls from 150 m water depth in the Indian Ocean (1974)
    PANGAEA
    In:  Supplement to: Simonsen, R (1974): The Diatom Plankton of the Indian Ocean Expedition of RV "Meteor" 1964 - 1965. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe D Biologie, Gebrüder Bornträger, Berlin, Stuttgart, D19, 1-107
    Details
    Publication Date: 2023-07-09
    Description: During the Indian Ocean Expedition of R/V METEOR phytoplankton samples were taken with a multiple closing net (Multinet) at 103 stations. In this material the diatoms were investigated. In all 247 taxa could be identified which belong to 242 species and 5 varieties of formae of 80 genera. Of these 1 variety, 15 pecies, and 3 genera are newly described. New combinations were made for 18 species, and a number of old combinations was reinstated.
    Keywords: Abundance estimate; Actinocyclus curvatulus; Actinocyclus elongatus; Actinocyclus octonarius; Actinocyclus subtilis; Actinoptychus annulatus; Actinoptychus senarius; Actinoptychus splendens; Amphiprora alata; Amphiprora sulcata; Amphora angusta; Amphora bigibba; Amphora crassa; Amphora decussata; Amphora graffeana; Amphora granulata; Amphora robusta; Amphora spectabilis; Amphora wisei; Area/locality; Asterionella glacialis; Asterionella notata; Asterolampra grevillei; Asterolampra marylandica; Asteromphalus arachne; Asteromphalus elegans; Asteromphalus flabellatus; Asteromphalus heptactis; Asteromphalus imbricatus; Asteromphalus ingens; Asteromphalus petterssonii; Asteromphalus roperianus; Asteromphalus sarcophagus; Auricula insecta; Bacillaria paradoxa; Bacteriastrum furcatum; Bacteriastrum furcatum-hispida; Biddulphia pulchella; Biddulphia tuomeyi; Caloneis elongata; Cerataulina bergonii; Cerataulus smithii; Chaetoceros atlanticus; Chaetoceros bacteriastroides; Chaetoceros buceros; Chaetoceros coarctatus; Chaetoceros compressus; Chaetoceros curvisetus; Chaetoceros decipiens; Chaetoceros denticulatus; Chaetoceros didymus; Chaetoceros diversus; Chaetoceros lorenzianus; Chaetoceros messanensis; Chaetoceros peruvianus; Chaetoceros radicans; Chaetoceros rostratus; Chaetoceros seychellarum; Chaetoceros sumatranus; Chaetoceros tetratichon; Climacodium frauenfeldianum; Cocconeis dirupta; Cocconeis dirupta-flexella; Cocconeis distans; Cocconeis placentula; Cocconeis scutellum; Corethron criophilum; Coscinodiscus africanus; Coscinodiscus asteromphalus; Coscinodiscus centralis; Coscinodiscus concinniformis; Coscinodiscus concinnoides; Coscinodiscus crenulatus; Coscinodiscus gigas; Coscinodiscus granii; Coscinodiscus jonesianus; Coscinodiscus lineatus; Coscinodiscus nodulifer; Coscinodiscus oculus-iridis; Coscinodiscus perforatus; Coscinodiscus plicatoides; Coscinodiscus radiatus; Coscinodiscus reniformis; Coscinodiscus stellaris; Coscinodiscus thorii; CT; Cyclotella striata; Cyclotella stylorum; Cymatonitzschia marina; Cymatotheka weissflogii; Dactyliosolen mediterraneus; DEPTH, water; Detonula pumila; Diploneis bomboides; Diploneis didyma; Diploneis papula; Diploneis smithii; Ditylum sol; Ethmodiscus gazellae; Ethmodiscus rex; Ethmodiscus spp. fragments; Eucampia cornuta; Eucampia zodiacus; Fragilaria intermedia; Glyphodesmis rhombica; Gomphonema pseudexiguum; Gossleriella tropica; Grammatophora marina; Guinardia flaccida; Hantzschia amphioxys; Haslea gigantea; Haslea gretharum; Haslea hyalinissima; Haslea wawrikae; Hemiaulus hauckii; Hemiaulus membranaceus; Hemiaulus sinensis; Hemidiscus cuneiformis; Hemidiscus kanayanus; IIOE - International Indian Ocean Expedition; Indian Ocean; Lauderia annulata; Licmophora communis; Licmophora flabellata; M1; M1-track; Mastogloia minuta; Mastogloia rostrata; Mastogloia woodiana; Melosira granulata; Meteor (1964); Navicula abrupta; Navicula comoides; Navicula crucifera; Navicula directa; Navicula distantepunctata; Navicula durandii; Navicula humerosa; Navicula lorenzii; Navicula mutica; Navicula mutica forma cohnii; Navicula nivalis; Navicula protracta; Navicula salinarum; Nitzschia aequatorialis; Nitzschia bicapitata; Nitzschia braarudii; Nitzschia capuluspalae; Nitzschia closterium; Nitzschia constricta; Nitzschia cuspidata; Nitzschia dietrichii; Nitzschia distans; Nitzschia heimii; Nitzschia hybrida; Nitzschia inflatula; Nitzschia inflatula-capitata; Nitzschia interruptestriata; Nitzschia kolaczeckii; Nitzschia lineola; Nitzschia longa; Nitzschia longicollum; Nitzschia longissima; Nitzschia lorenziana; Nitzschia marina; Nitzschia maxima; Nitzschia ossiformis; Nitzschia panduriformis; Nitzschia pungens; Nitzschia pungiformis; Nitzschia sicula; Nitzschia sigma; Nitzschia sigmaformis; Nitzschia socialis; Nitzschia subfraudulenta; Nitzschia subpacifica; Number; Odontella aurita; Odontella mobiliensis; Odontella regia; Odontella rhombus; Odontella sinensis; Oestrupia musca; Pachyneis gerlachii; Palmeria hardmaniana; Paralia sulcata; Pinnularia borealis; Pinnularia cuneatoundulata; Plagiogramma staurophorum; Planktoniella sol; Pleurosigma directum; Pleurosigma indicum; Pleurosigma naviculaceum; Pleurosigma planctonicum; Podocystis spathulata; Podosira stelliger; Porosira denticulata; Protoraphis hustedtiana; Pseudoeunotia doliolus; Pseudohimantidium pacificum; Pseudotriceratium punctatum; Rhabdonema adriaticum; Rhaphoneis amphiceros; Rhaphoneis surirella; Rhaphoneis surirelloides; Rhizosolenia alata; Rhizosolenia alata-indica; Rhizosolenia bergonii; Rhizosolenia calcar-avis; Rhizosolenia castracanei; Rhizosolenia cochlea; Rhizosolenia cylindrus; Rhizosolenia hebetata; Rhizosolenia imbricata; Rhizosolenia robusta; Rhizosolenia setigera; Rhizosolenia styliformis; Roperia tesselata; Sample code/label; Skeletonema costatum; Stauroneis amphioxys; Stauroneis membranacea; Stephanopyxis palmeriana; Stephanopyxis turris; Stictodiscus californicus; Surirella fastuosa; Synedra hennedyana; Synedra indica; Thalassionema bacillaris; Thalassionema nitzschioides; Thalassiosira diporocyclus; Thalassiosira eccentrica; Thalassiosira lineata; Thalassiosira minuscula; Thalassiosira oestrupii; Thalassiosira punctigera; Thalassiosira spinosa; Thalassiosira subtilis; Thalassiosira symmetrica; Thalassiothrix delicatula; Thalassiothrix frauenfeldii; Thalassiothrix longissima; Thalassiothrix mediterranea; Thalassiothrix vanhoeffenii; Trachyneis antillarum; Trachyneis aspera; Trachyneis debyi; Triceratium broeckii; Triceratium dubium; Triceratium favus; Triceratium pentacrinus; Triceratium robertsianum; Trigonium alternans; Trigonium reticulum; Tropidoneis maxima; Tropidoneis sp.; Tropidoneis subulata; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1337 data points
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  • 7
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    Annotated record of the detailed examination of Mn deposits from DSDP Site 172, Leg 18 (Cores 172-1, 172-2) (1973)
    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
    Details
    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
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  • 8
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    Annotated record of the detailed examination of Mn deposits from DSDP Leg 20 (Sites 195, 196, 198A) (1973)
    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
    Details
    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
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  • 9
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    Unknown
    Observation of manganese deposits in the Gulf of Maine by the ALVIN submersible in 1971-1972 (1974)
    PANGAEA
    Details
    Publication Date: 2023-08-28
    Keywords: AL34200; AL34900; AL42100; AL42300; AL42700; AL43100; AL44500; ALV342; ALV-342; ALV349; ALV-349; ALV421; ALV-421; ALV423; ALV-423; ALV427; ALV-427; ALV431; ALV-431; ALV445; ALV-445; Alvin; Comment; Deposit type; DEPTH, sediment/rock; Description; Event label; Grab; GRAB; Gulf of Maine, Atlantic Ocean; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 55 data points
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  • 10
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    Annotated record of the detailed examination of Mn nodules from the Baja California Seamount Province (1973)
    PANGAEA
    In:  Supplement to: Sorem, Ronald K; Foster, Allan R (1973): Mineralogical, chemical and optical procedures and standards for study of growth features and economic potential of manganese nodules. 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, 23-38, https://store.pangaea.de/Projects/NOAA-MMS/Sorem_1973_IDOE.pdf
    Details
    Publication Date: 2023-08-28
    Description: Internal growth features of manganese nodules reveal that many nodules are structurally, chemically, and mineralogically non-uniform, largely as a result of a complex growth history. If numerous investigators are to study the mineralogical and textural features of manganese nodules, the laboratories concerned must standardize procedures to some extent so that work is not duplicated and so that results can be compared fairly. In particular, we suggest that all investigators, for example, geochemists, mineralogists, and biologists who work with individual nodules, should pay due attention to the internal complexity of nodules while pursuing their individual specialized research. Detailed investigation of the relationships between the internal structure of manganese nodules and the mineralogy and chemical composition is essential to an understanding of nodule origin and of possible problems in economic use of nodules. Research of this kind is best controlled by use of good polished sections of whole manganese nodules.
    Keywords: Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sample code/label; Sample ID; SAN_JUAN_1963; Size; SNJ-DH8; Spencer F. Baird; Substrate type; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 17 data points
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