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  • Other Sources  (16)
  • Inst. f. Geophys., Ruhr-Univ. Bochum  (5)
  • Universität Göttingen,Abteilung Bodenphysik  (5)
  • Elsevier  (4)
  • British Antarctic Survey  (2)
  • 2010-2014
  • 1980-1984  (16)
  • 1981  (16)
  • 1
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    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-04-25
    Description: research
    Keywords: Plantagenwirtschaft ; Teakbaumplantage ; Nährstoffhaushalt ; Forstlicher Standort ; Caparo ; Venezuela
    Language: German
    Type: doc-type:book
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  • 2
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    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-04-26
    Description: research
    Keywords: Wasserhaushalt ; Bodenphysik ; Physikochemische Bodeneigenschaft ; Hydrodynamik Hochebene ; Pseudogley ; Waldboden
    Language: German
    Type: doc-type:book
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  • 3
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    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-04-26
    Description: research
    Keywords: Pflanzensoziologie ; Waldgesellschaft ; Ostalpen ; Exkursion Italien ; Waldpflanzen ; Forst Ostalpen ; Vegetation ; Italienische Alpen ; Oberitalien
    Language: German
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  • 4
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    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-05-20
    Description: thesis
    Keywords: Dissertation
    Language: German
    Type: doc-type:book
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  • 5
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    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-05-03
    Description: research
    Keywords: NITROGEN FERTILIZERS ; NEUTRAL SOlLS ; ACID LOESS SOlLS ; BEHAVIOUR OF NITROGEN FERTILIZERS
    Language: English
    Type: doc-type:book
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  • 6
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    Elsevier
    In:  Bull., Polar Proj. OP-O3A4, Computer-aided Seismic Analysis and Discrimination, London, Elsevier, vol. 16, no. 4, pp. 97-109, (ISBN 0080419208)
    Publication Date: 1981
    Keywords: Group veloc. ; Velocity analysis
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  • 7
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    Inst. f. Geophys., Ruhr-Univ. Bochum
    In:  Wissenschaftl. Veröffentl. (Reihe B), Hrsg. H.-P. Harjes, Atlanta, Inst. f. Geophys., Ruhr-Univ. Bochum, vol. 10, no. PL-TR-91-2127, pp. 1219-1222
    Publication Date: 1981
    Keywords: BUG ; ERDSTOSS (see also rockburst and Gebirgsschlag) ; Mining geophysics ; GEBIRGSSCHLAG (see also rockburst and Erdstoss) ; Earthquake catalog ; Rock bursts (see also ERDSTOSS and GEBIRGSSCHLAG) ; Local earthquakes
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  • 8
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    Inst. f. Geophys., Ruhr-Univ. Bochum
    In:  Dissertation, Berichte, Bochum, Inst. f. Geophys., Ruhr-Univ. Bochum, vol. 10, no. 9, pp. 1109-1111
    Publication Date: 1981
    Keywords: Geomagnetics ; Plate tectonics ; Borehole geophys.
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  • 9
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    Inst. f. Geophys., Ruhr-Univ. Bochum
    In:  Diplomarbeit, Rome, Inst. f. Geophys., Ruhr-Univ. Bochum, vol. 10, no. 13, pp. 1431-1434, (ISBN 0 08 042822 3)
    Publication Date: 1981
    Keywords: Velocity ; Physical properties of rocks ; Laboratory measurements ; Instruments ; Wohrl
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  • 10
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    Inst. f. Geophys., Ruhr-Univ. Bochum
    In:  Diplomarbeit, Tokyo, Inst. f. Geophys., Ruhr-Univ. Bochum, vol. C 560, 183 pp., no. 29, pp. 1321-1323, (ISBN 3-933346-037)
    Publication Date: 1981
    Keywords: SEModelling ; Channel waves ; Mining geophysics ; Rayleigh waves ; Kuhbach
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  • 11
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    Inst. f. Geophys., Ruhr-Univ. Bochum
    In:  Dissertation, Berichte, Houston, Inst. f. Geophys., Ruhr-Univ. Bochum, no. 10, pp. 103-155
    Publication Date: 1981
    Keywords: Stress ; cracks and fractures (.NE. fracturing) ; Fracture ; Laboratory measurements
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  • 12
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    British Antarctic Survey
    In:  British Antarctic Survey Butlletin, 54 . pp. 1-7.
    Publication Date: 2020-06-15
    Description: 122 regurgitations by adults and chicks of the small grey-headed and black-browed albatrosses (mollymauks) included, besides flesh remains, 421 upper beaks (mandibles) and 422 lower beaks of cephalopods. The lower beaks and some flesh remains were identified, their lower rostral lengths were measured and the wet weight of squids represented by beaks was estimated. Nine species of squid and one octopod were identified. In both species of albatross, the muscular ommastrephid squid Todarodes is the principal squid in the diet, contributing 88% of the beaks and an estimated 91% of the weight of cephalopods represented by beaks in grey-headed albatrosses and 68% of the beaks and 76% of the weight in black-browed albatrosses. Second in importance in the diet is a cranchiid Mesonychoteuthis sp. A, which contributes 8% and 25% by number and 4% and 12% by weight to the diet of grey-headed and blackbrowed albatrosses, respectively. The eight remaining species are each represented by either one or two lower beaks. These samples are compared with samples from sperm whale stomachs and wandering albatrosses also collected near South Georgia.
    Type: Article , PeerReviewed
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  • 13
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    British Antarctic Survey
    In:  British Antarctic Survey Butlletin, 54 . pp. 9-21.
    Publication Date: 2020-06-15
    Description: Regurgitations of the chicks of wandering albatrosses near their nests included 762 upper beaks (mandibles) and 532 lower beaks of cephalopods. Twenty-five species of cephalopod are present in the diet. Analysis of the complete samples shows the three most important species in the diet to be Kondakovia longimana (40.0% by number), Taonius pavo (16.9%) and Histioteuthis(?) eltaninae (8.7%). While the large Taningia danae only comprises 1.3% by number, it may contribute over 5% by weight. The species and size ranges of beaks are compared with those occurring in the stomachs of sperm whales killed by whalers in the Southern Hemisphere (Clarke, 1980). The ten complete samples contain an average of 44 beaks which probably represents about 200 days' accumulation. Both Antarctic and warm-water cephalopods are present in the diet. These albatrosses possibly scavenge some of thei food from vomit of sperm whales.
    Type: Article , PeerReviewed
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  • 14
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    Elsevier
    In:  Tectonophysics, 73 (1-3). pp. 151-168.
    Publication Date: 2021-06-08
    Description: The structural setting of the Maltese Islands is governed by two rift systems of different ages and trends and the interference of both. Accompanying faults are exposed at many places along cliffs and belong to the most spectacular phenomena of rift faulting of the world. Malta is part of a wide shelf bridge that connects the Ragusa platform of southern Sicily and the Tripolitanian platform of northern Libya. The archipelago is underlain by a continental crust of African provenance. The older rift generation traversing the islands strikes about 50° to 70° to create a basin-and-range structure on western Malta, Comino and eastern Gozo. This micro-province is framed by two master faults at an average distance of 14 km. Crustal extension started during the Early Miocene, as observed by growth faulting and sedimentary dikes parallel to the future rift. A syndepositional uparching of about 200 m has preceded the physiographical rifting in post-Middle Miocene times. Discrete dip-slip faulting created an external wedge block, split by internal tilt blocks of antithetic character, both compensating an average 15% crustal spreading normal to the rift axis. Shoulder upwarping of approximately 120 m has evolved synchronously with the rifting. Structures of the first generation are crosscut by still active, second-generation rift faults, which on Malta strike about 120°, but on Gozo between 80° and 90°. These faults are associated with the Pantelleria rift, whose deep trough sets immediately south of the islands. Rifting was mainly originated during Late Miocene/Early Pliocene time to continue in parts up to the Present. A set of transform faults runs through the straits on both sides of Comino to form a complicated en echelon or Riedel shear structure on easternmost Gozo and westernmost Malta. Shoulder upwarping related to the Pantelleria rift has considerably tilted the block of Malta NNE-ward and caused the inundated river valleys of the natural harbour of Valletta. The superimposition of two rift structures of different trends has been caused principally by a rotation of the controlling stress regime about 10 m.y. ago. The active Afro—Eurasian collision front is located about 200 km north and northwest of the islands. A contemporary change of plate tectonic stresses is discussed to explain the intraplate rift pattern on Malta as foreland-specific reactions to plate tectonic processes.
    Type: Article , PeerReviewed
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  • 15
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    Elsevier
    In:  Geochimica et Cosmochimica Acta, 45 (4). pp. 577-588.
    Publication Date: 2016-03-01
    Description: Generally, oxidative regeneration of phosphate from anoxic sediments is by microbially mediated sulfate reduction processes. Stoichiometric modelling of such reactions takes into consideration varying proportions of ‘decomposable’ organically bound P to account for the ratios among nutrients in depth-concentration profiles of near-surface sediments. New results of interstitial water composition from sediments underlying the water masses influenced by coastal upwelling of the eastern boundary current system off Peru indicate that dissolution of phosphatic fish debris represents a mechanism for remineralization of phosphate comparable to or larger in magnitude than that by oxidative regeneration of organically bound P. Dissolved interstitial phosphate from fish debris is revealed by an excess amount of phosphate over that predicted from a simple stoichiometric oxidative regeneration model and by anomalously high dissolved interstitial fluoride concentrations. Phosphate flux estimates based on diffusion from the sediment suggest that this mechanism may generate up to 10% of the nutrient pool in the waters of the Peru undercurrent. Partitioning of P among the two sources reveals further that fish debris phosphate is about four times more important than organically bound P in nutrient generation from sediments of the Peru continental margin. Not only does this mechanism of regeneration affect the nutrient cycling but may also control widespread phosphorite formation in this area.
    Type: Article , PeerReviewed
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  • 16
    Publication Date: 2018-07-25
    Description: Investigations of formation-fluid salinities in a transect from western Georgia to the edge of the Blake Plateau off the coast of Georgia show surprisingly similar hydrochemical features offshore and onshore. A fresh-brackish wedge of groundwater (〈25 g/kg total dissolved solids) lies beneath the shelf to a depth of ∼ 900 m. On land, brackish waters extend to a maximum depth of ∼ 1.2 km below sea level in Lowndes County, Georgia. In deeper horizons, hypersaline brines (〉 100 g/kg) occur in Lower Cretaceous (?) strata. These strata have a pronounced evaporitic (anhydritic) character in the offshore segment. Strong salinity gradients in interstitial waters signify buried evaporite deposits at drill sites beneath the Blake Plateau.
    Type: Article , PeerReviewed
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