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  • Other Sources  (44)
  • AGU  (29)
  • Wiley  (15)
  • 1985-1989  (44)
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Year
  • 1
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    AGU
    In:  Washington D. C., AGU, vol. 4, no. 3, pp. 2-203, (ISBN: 3-540-41598-X)
    Publication Date: 1989
    Keywords: Plate tectonics ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Stress ; Vanicek
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  • 2
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    Wiley
    In:  New York, Wiley, vol. 98, no. ALEX(01)-FR-77-01, AFTAC Contract F08606-76-C-0025, pp. 95-104, (ISBN: 1-4020-1592-5)
    Publication Date: 1989
    Keywords: Rock mechanics ; Laboratory measurements
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  • 3
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    AGU
    In:  Washington D. C., AGU, vol. 3, no. ALEX(01)-FR-77-01, AFTAC Contract F08606-76-C-0025, pp. 329, (ISBN 1-903544-06-8)
    Publication Date: 1989
    Keywords: Textbook of geology ; Volcanology ; Earthquake hazard
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  • 4
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    AGU
    In:  Washington D. C., AGU, vol. 5, no. XVI:, pp. 1-14, (ISBN 0-89871-521-0)
    Publication Date: 1989
    Keywords: Earth model, also for more shallow analyses ! ; Plate tectonics ; Geol. aspects ; Deep seismic sounding (espec. cont. crust)
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  • 5
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    AGU
    In:  Bull., Polar Proj. OP-O3A4, Origin and Evolution of Sedimentary Basins and Their Energy, Washington, D.C., AGU, vol. 48, no. 4, pp. 65-71, (ISBN 0080419208)
    Publication Date: 1989
    Keywords: Geol. aspects ; Modelling ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; 8110 ; Tectonophysics ; Continental ; tectonics ; 8165 ; Structural ; geology ; (crustal ; structure ; and ; mechanics) ; 8194 ; Instruments ; and ; techniques
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  • 6
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    AGU
    In:  Washington D. C., AGU, vol. 8, no. XVI:, pp. 1-14, (ISBN: 0-387-30752-4)
    Publication Date: 1989
    Keywords: Data analysis / ~ processing ; Statistical investigations
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  • 7
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    AGU
    In:  Washington D. C., AGU, vol. 8, no. Publ. No. 12, pp. 9, (3-540-24165-5, XXVI + 228 p.)
    Publication Date: 1989
    Keywords: Earth model, also for more shallow analyses ! ; Plate tectonics
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  • 8
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    AGU
    In:  AGU Spring Meeting, S22A-13, Baltimore, AGU, vol. 11, no. CUED/C/Mats/Tr 51, pp. 1414-1415
    Publication Date: 1989
    Keywords: Seismic networks ; Seismic arrays ; Filter- ; Polarization ; Shear waves
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  • 9
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    Wiley
    In:  In: Marine invertebrate fisheries : their assessment and management. , ed. by Caddy, J. F. A Wiley-interscience publication . Wiley, New York, pp. 559-589. ISBN 0-471-83237-5
    Publication Date: 2020-07-08
    Type: Book chapter , NonPeerReviewed
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  • 10
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    Wiley
    In:  In: Marine invertebrate fisheries : their assessment and management. , ed. by Caddy, J. F. A Wiley-interscience publication . Wiley, New York, pp. 665-700. ISBN 0-471-83237-5
    Publication Date: 2020-07-08
    Type: Book chapter , NonPeerReviewed
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  • 11
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    Wiley
    In:  Aquaculture Research, 20 (1). pp. 1-14.
    Publication Date: 2020-06-11
    Description: Loligo forbesi Steenstrup is a commercially and biomedically important species raneing from Scotland to North Africa and from the Azores Islands in the central Atlantic east through the Mediterranean Sea and Red Sea. Eggs were collected from Plymouth. England and from the Azores and the hatchlings were reared to adult size in recirculating seawater systems. Growth data were obtained primarily from mortalities during the course of three culture experiments which lasted 360, 240 and 480 days. Loligo forbesi hatched at a size of 5–9mg (3.0–4.6mm mantle length, ML) and grew to a maximum size of 124g (155 mm ML) in 413 days. In all experiments, growth was exponential in form for at least the first 3 months at rales of 5.8, 5.1 and 3.6% body weight per day (BW/d) at mean temperatures of 14.1, 14.0 and 13.1°C respectively. In one short-term experiment, month-old squids grew at 8.0% BW/d at 17.4°C. Growth beyond 3 months was slower and either logarithmic (as described by the power function) or exponential in form. Growth rates gradually declined to 1–2% BW/d, Analyses of mantle length growth confirmed the wet weight results. There was no evidence of sexual dimorphism in the laboratory populations, which were of small size, and the length-weight (L-W) relationships were found to be similar to those of field populations. Growth rates during the exponential growth phase appeared very sensitive to temperature, with a 1°C difference changing growth rate by 2% BW/d and producing a three-fold difference in weight at 90 days post-hatching. These dramatic effects of temperature on adult size and lifespan in nature are discussed. It is hypothesized that the small size of mature laboratory-reared squids was due to low culture temperatures during the first 3 months.
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  • 12
    Publication Date: 2020-06-12
    Description: First culture results are presented from four major experiments (lasting up to 478 days) on the commercially important squid species, Loligo forbesi Steenstrup, Details are provided on eggs, hatching, feeding, growth, survival, behaviour and sexual maturation. Best survival during the critical first 75 days was 15%. The hatchlings (up to 4.9mm mantle length, ML) are the largest among the genus Loligo, and the largest squid grown was a male 155mm ML and 124g. First schooling was observed only 40–50 days post-hatching. Spawning was not achieved although males reached maturity, females had maturing ova and mating was observed. The largest giant axon measured was 425μm in diameter (from a female 130mm ML), a size suitable for most biomedical applications. Laboratory data suggest a 2-year life cycle compared to fishery data which suggest a 1-year cycle.
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  • 13
    Publication Date: 2018-08-07
    Description: Interrelationships between the morphological and physiological properties of selected cyanobacterial species distinguished in the laboratory are used to simulate their population dynamics against realistic scales of environmental variability. Differences in performances are shown to correlate well with the ambient conditions found in the various types of lakes in which cyanobacteria are typically distributed.
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  • 14
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    The Fisheries Society of the British Isles | Wiley
    In:  Journal of Fish Biology, 35 (SupplementA). pp. 331-333.
    Publication Date: 2019-08-08
    Type: Article , PeerReviewed
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  • 15
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    AGU
    In:  Washington, D.C., AGU, vol. Developments in Petroleum Science vol. 15B, no. Publ. No. 12, pp. 9, (ISBN: 3-540-31080-0)
    Publication Date: 1988
    Keywords: Handbook of physics ; Handbook of mineralogy ; Physical properties of rocks ; Mineralogy
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  • 16
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    Wiley
    In:  In: Methods in Aquatic Bacteriology. , ed. by Austin, B. Wiley, Chichester, UK, pp. 207-240. ISBN 978-0471916512
    Publication Date: 2020-05-05
    Type: Book chapter , NonPeerReviewed
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  • 17
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    AGU (American Geophysical Union) | Wiley
    In:  Journal of Geophysical Research: Solid Earth, 93 (B8). pp. 9027-9057.
    Publication Date: 2021-06-01
    Description: We have determined the centroid depths and source mechanisms of 12 large earthquakes on transform faults of the northern Mid-Atlantic Ridge from an inversion of long-period body waveforms. The earthquakes occurred on the Gibbs, Oceanographer, Hayes, Kane, 15°20′, and Vema transforms. We have also estimated the depth extent of faulting during each earthquake from the centroid depth and the fault width. For five of the transforms, earthquake centroid depths lie in the range 7–10 km beneath the seafloor, and the maximum depth of seismic faulting is 14–20 km. On the basis of a comparison with a simple thermal model for transform faults, this maximum depth of seismic behavior corresponds to a nominal temperature of 900° ± 100°C. In contrast, the nominal temperature limiting the maximum depth of faulting during oceanic intraplate earthquakes with strike-slip mechanisms is 700° ± 100°C. The difference in these limiting temperatures may be attributed to the different strain rates characterizing intraplate and transform fault environments. Three large earthquakes on the 15°20′ transform have shallower centroid depths of 4–5 km and a maximum depth of seismic faulting of 10 km, corresponding to a limiting temperature of 600°C. The shallower extent of seismic behavior along the 15°20′ transform may be related to a recent episode of extension across the transform associated with the northward migration of the triple junction among North American, South American, and African plates to its present position near the transform. The source mechanisms for all events in this study display the strike-slip motion expected for transform fault earthquakes; slip vector azimuths agree to within 2°–3° of the local strike of the zone of active faulting. The only anomalies in mechanism were for two earthquakes near the western end of the Vema transform which occurred on significantly nonvertical fault planes. Secondary faulting, occurring either precursory to or near the end of the main episode of strike-slip rupture, was observed for five of the 12 earthquakes. For three events the secondary faulting was characterized by reverse motion on fault planes striking oblique to the trend of the transform. In all three cases the site of secondary reverse faulting is near a compressional jog in the current trace of the active transform fault zone. We find no evidence to support the conclusions of Engeln, Wiens, and Stein that oceanic transform faults in general are either hotter than expected from simple thermal models or weaker than normal oceanic lithosphere.
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  • 18
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    AGU (American Geophysical Union) | Wiley
    In:  Journal of Geophysical Research: Solid Earth, 93 (B8). pp. 8911-8927.
    Publication Date: 2021-12-13
    Description: High-resolution seismic reflection and Sea Beam bathymetric data provide insights into the processes of sediment offscraping and accretion in the Middle America Trench off southern Mexico. Thick terrigenous sediments that are transported down Ometepec Canyon and accumulate along the trench floor are scraped off the oceanic plate and accreted in thrust packets to the lower trench slope. The packets offscraped represent most of the trench strata. Underlying hemipelagic deposits that accumulate on the seafloor seaward of the trench are subducted landward of the toe of the slope. Horizontal displacement on the thrust is less than 1 km. Leading edge folds are the surface expressions of the thrusts and strike subparallel to the base of the trench slope. The folds are continuous for as much as 10 km and have amplitudes as high as 200 m and wavelengths of 0.5 to 2 km. Folds are best developed along sections of the trench with interbedded silty turbidite and mud deposits. Fold are absent where thick coarse-grained fan deposits occur. Thickening of the thrust packets occurs by large-scale thrust duplication, by layer-parallel shortening, and by deposition of material that slumps off the leading edge of older upslope thrust blocks.
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  • 19
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    AGU
    In:  Bull., Polar Proj. OP-O3A4, Composition, Structure and Dynamics of the Lithosphere-Asthenosphere System, Washington, D.C., AGU, vol. 16, no. Subvol. a, pp. 111-123, (ISBN 0080419208)
    Publication Date: 1987
    Keywords: Review article ; Anisotropy ; Physical properties of rocks
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  • 20
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    Wiley
    In:  New York, 3rd Edition, 538 pp., Wiley, vol. 14, no. 1, pp. 1-40, (ISBN 3-7643-6675-3)
    Publication Date: 1987
    Keywords: Reflection seismics ; Textbook of geophysics ; Applied geophysics
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  • 21
    Publication Date: 2020-06-30
    Description: The diets of adult Macaroni penguins Eudyptes chrysolophus chrysolophus and Southern rockhopper penguins E. chrysocome chrysocome were analysed quantitatively at Marion Island, southern Indian Ocean, throughout two successive chick-rearing seasons. The diets were broadly similar. Crustaceans were the predominant prey type comprising, overall, 90% by mass and 98% by numbers in Macaroni penguins and 96% by mass and 99% by numbers in rockhopper penguins. Nauticaris marionis was the predominant crustacean eaten by both penguin species in 1983–84, but Euphausia vallentini and Thysanoessa vicina predominated in 1984–85. Themisto gaudichaudii was present in appreciable numbers only in Macaroni penguins. Fish was not found in measurable quantities in either species in 1983–84, but contributed 5% and 4% of the mass of the diet in Macaroni and rockhopper penguins, respectively, when calculated in terms of the original biomass of food ingested. In 1984–85, however, fish comprised 10% and 6% of observed mass and c. 25% and 14% of original biomass ingested in Macaroni and rockhopper penguins, respectively. Pelagic myctophids, predominantly Krefftichthys anderssoni, Protomyctophum tenisoni and P. normani between 0·01 and 8·3 g, were the most commonly identified fish prey, but Macaroni penguins took an appreciable number of Electrona carlsbergi in 1983–84. Cephalopods made up between 1 % and 3% of the diet by mass in both penguin species and between 5% and 13% of original biomass ingested. Predominant cephalopods eaten were Kondakovia longimana and an unidentified octopus species. The relative proportions of each prey type change throughout chick-rearing, with pelagic fish and cephalopods comprising a larger proportion later in the season when the penguins were assumed to be foraging farther from their breeding sites. Dietary segregation of the two species appears to be related to the difference in the timing of the breeding season, which begins three to four weeks earlier in Macaroni penguins.
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  • 22
    Publication Date: 2021-05-05
    Description: Maturing females of the octopod Japetella diaphana (Hoyle) develop a luminous oral ring. Studies of specimens of different size show that this structure develops from a muscular ring which undergoes great cellular proliferation, associated with gradual degeneration of the original muscle. The light‐producing cells (photocytes) have a relatively uniform cytoplasm whose most characteristic components are small mitochondria, granular aggregates and microtubular or microfibrillar bundles. It is concluded that the original muscle tissue is not transformed directly into luminous tissue. Possible uses of the luminescence are discussed, based on the postures adopted by live specimens in shipboard aquaria.
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  • 23
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    AGU
    In:  Washington D. C., AGU, vol. 1, pp. 6322, (ISBN 0-521-79203-7)
    Publication Date: 1986
    Keywords: Textbook of geophysics ; Seismics (controlled source seismology) ; Earth model, also for more shallow analyses !
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  • 24
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    AGU
    In:  Washington D. C., AGU, vol. 14, pp. 6322, (ISBN 0-521-79203-7)
    Publication Date: 1986
    Keywords: Textbook of geophysics ; Seismics (controlled source seismology) ; Earth model, also for more shallow analyses ! ; Reflection seismics
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  • 25
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    AGU
    In:  Washington D.C., AGU, vol. 6, no. XVI:, pp. 227-235, (ISBN 3-342-00685-4)
    Publication Date: 1986
    Keywords: Stress ; Earthquake precursor: statistical anal. of seismicity ; Source parameters ; Stress drop
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  • 26
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    AGU
    In:  Washington D.C., AGU, vol. 6, no. Publ. No. 12, pp. 81-89, (ISBN 0-444-50971-2)
    Publication Date: 1986
    Keywords: Rock mechanics ; Fluids ; Source
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  • 27
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    AGU
    In:  Professional Paper, Earthquake Source Mechanics, Washington, D.C., AGU, vol. 6, no. 16, pp. 91-96, (ISBN 1-4020-1729-4)
    Publication Date: 1986
    Keywords: Earthquake precursor: prediction research
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  • 28
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    AGU
    In:  Bull., Open-File Rept., Earthquake Source Mechanics, Maurice Ewing Ser., Washington D.C., AGU, vol. 6, no. 16, pp. 209-216, (ISBN 1-86239-165-3, vi + 330 pp.)
    Publication Date: 1986
    Keywords: Seismicity ; Subduction zone ; scaling ; Magnitude ; seismic Moment ; nokms
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  • 29
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    AGU
    In:  Bull., Open-File Rept., Earthquake Source Mechanics, Maurice Ewing Ser., Washington D.C., AGU, vol. 6, no. 16, pp. 157-167, (ISBN 1-86239-165-3, vi + 330 pp.)
    Publication Date: 1986
    Keywords: Fracture ; Fault zone ; Source
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  • 30
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    AGU
    In:  Washington, D.C., 341 pp., AGU, vol. 231, no. 3, pp. 2-203, (ISBN 0-470-02298-1)
    Publication Date: 1986
    Keywords: Earthquake precursor: prediction research
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  • 31
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    Wiley
    In:  New York, Wiley, vol. 2, no. XVI:, pp. 1-14, (ISBN 0-08-043751-6)
    Publication Date: 1986
    Keywords: Data analysis / ~ processing
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  • 32
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    AGU
    In:  Washington D.C., AGU, vol. 6, no. XVI:, pp. 65-70, (ISBN: 3486274473, 2. Auflage 2004, xxiv, 244 Seiten)
    Publication Date: 1986
    Keywords: Friction ; Fault zone ; Elasticity
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  • 33
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    AGU
    In:  Washington D.C., AGU, vol. 6, no. 22, pp. 71-80, (ISBN 0-87590-422-X)
    Publication Date: 1986
    Keywords: Fracture ; Inelastic ; Fault zone ; Source mechanics
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  • 34
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    AGU
    In:  Professional Paper, Earthquake Source Mechanics, Washington, D.C., AGU, vol. 6, no. 16, pp. 237-245, (ISBN 1-86239-165-3, vi + 330 pp.)
    Publication Date: 1986
    Keywords: Earthquake precursor: prediction research ; Stress drop ; Seismic arrays ; Source parameters
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  • 35
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    AGU
    In:  Bull., Polar Proj. OP-O3A4, Reflection Seismology: A Global Perspective, Washington, D.C., AGU, vol. 13, no. Subvol. a, pp. 167-182, (ISBN 0080419208)
    Publication Date: 1986
    Keywords: Review article ; Deep seismic sounding (espec. cont. crust) ; Refraction seismics ; Muller
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  • 36
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    AGU
    In:  Bull., Open-File Rept., Earthquake Source Mechanics, Washington D. C., AGU, vol. 6, no. 16, pp. 147-155, (ISBN 1-86239-165-3, vi + 330 pp.)
    Publication Date: 1986
    Keywords: FractureT ; Fault zone ; Geol. aspects
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  • 37
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    AGU
    In:  Bull., Open-File Rept., Earthquake Source Mechanics, Washington, D.C., AGU, vol. 6, no. 1, pp. 131-145, (ISBN 1-86239-165-3, vi + 330 pp.)
    Publication Date: 1986
    Keywords: Earthquake ; Stress ; Geothermics ; CRUST ; Inelastic ; HGROSSER ; FROTH
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  • 38
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    Wiley
    In:  In: Handbook of Holocene palaeoecology and palaeohydrology. , ed. by Berglund, B. E. Wiley, Chichester, pp. 527-570. ISBN 0-471-90691-3
    Publication Date: 2018-04-18
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  • 39
    Publication Date: 2020-07-23
    Description: A high-resolution near-bottom survey has been conducted of the Clipperton transform fault and adjoining segments of the East Pacific Rise (EPR), using the Sea MARC I side-looking sonar system and the Lamont-Doherty Geological Observatory Olympus-based camera system. The transform fault zone (TFZ) is a narrow, well-defined belt of transform-parallel lineaments, which varies along strike from a single, sharp-edged notch to a complex band of subparallel lineaments up to 1 km wide. The TFZ is set within a 5-km-wide band of unusually fine-grained side scan texture, which could indicate nonbasaltic seafloor and/or pervasively sheared and mass-wasted basaltic crust The fine-grained swath is surrounded by constructional volcanic terrain with no hint of strike-slip motion; this observation puts an upper limit of 5 km on the extent of lateral migration of the TFZ in the last 1.5 m.y. Both ridge transform intersections (RTIs) are dominated by bathymetric highs located on the old plate opposite the spreading center. A mantling of fresh-looking constructional volcanic terrain on side scan images suggests that the highs are built in part by recent extrusive and intrusive volcanism; thermal expansion may also play a part. The EPR south of Clipperton has recently experienced extrusion of high effusion rate basalts, burial of faults and fissures by lava flows, and development of vigorous hydrothermal circulation. On the EPR north of Clipperton, the axial zone of faults and fissures tapers toward the transform fault; this may reflect a change in the shape or size of the underlying shallow level magma feeders as a function of distance from the site of magma upwelling or distance toward the transform fault.
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  • 40
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    AGU
    In:  Journal of Geophysical Research: Oceans, 91 (C12). pp. 14192-14206.
    Publication Date: 2020-07-23
    Description: In the western tropical Atlantic, seasonal variations in the surface winds and in the ocean are dominated by an annual harmonic. A simulation with a general circulation model indicates that the response in the western side of the basin is an equilibrium one practically in phase with the local winds. It includes the following: large vertical excursions of the thermocline that have a 180° change in phase across 8°N approximately; a change in the direction of the North Brazilian Coastal Current, which flows continuously along the coast between December and May but which veers offshore near 5°N to feed the North Equatorial Countercurrent during the other months; and a seasonal reversal of the countercurrent. To the east of 30°W, seasonal changes in the model have a prominent semiannual harmonic in phase with the local winds but only partially attributable to forcing at that frequency. The transients excited by the abrupt intensification of the southeast tradewinds in May happen to have a phase essentially the same as that of the semiannual forcing. These transients decay by the end of the calendar year, so that the seasonal cycle that starts with the intensification of the winds in May can be treated as an initial value problem as far as the upper ocean, above the thermocline, is concerned. The winds along the equator determine the response of the surface equatorial layer in the Gulf of Guinea but play a minor role in the seasonal upwelling along the coast near 5°N. That upwelling is strongly influenced by changes in both components of the wind, and in the curl of the wind, over the Gulf of Guinea.
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  • 41
    Publication Date: 2020-07-23
    Description: Eddy correlation measurements over the ocean give CO2 fluxes an order of magnitude or more larger than expected from mass balance measurements using radiocarbon and radon 222. In particular, Smith and Jones (1985) reported large upward and downward fluxes in a surf zone at supersaturations of 15% and attributed them to the equilibration of bubbles at elevated pressures. They argue that even on the open ocean such bubble injection may create steady state CO2 supersaturations and that inferences of fluxes based on air-sea pCO2 differences and radon exchange velocities must be made with caution. We defend the global average CO2 exchange rate determined by three independent radioisotopic means: prebomb radiocarbon inventories; global surveys of mixed layer radon deficits; and oceanic uptake of bomb-produced radiocarbon. We argue that laboratory and lake data do not lead one to expect fluxes as large as reported from the eddy correlation technique; that the radon method of determining exchange velocities is indeed useful for estimating CO2 fluxes; that supersaturations of CO2 due to bubble injection on the open ocean are negligible; that the hypothesis that Smith and Jones advance cannot account for the fluxes that they report; and that the pCO2 values reported by Smith and Jones are likely to be systematically much too high. The CO2 fluxes for the ocean measured to date by the micrometeorological method can be reconciled with neither the observed concentrations of radioisotopes of radon and carbon in the oceans nor the tracer experiments carried out in lakes and in wind/wave tunnels.
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  • 42
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    AGU
    In:  Journal of Geophysical Research: Solid Earth, 90 (B8). p. 6709.
    Publication Date: 2020-07-23
    Description: Heat flow in the Imperial Valley and adjacent crystalline rocks is very high (∼140 mW m−2). Gravity and seismic studies suggest the crust is about 23.5 km thick with the lower half composed of gabbro and the upper fourth composed of low-density sediments. Conduction through such a crust resting directly on asthenosphere would give the observed heat flow if there were no extension or sedimentation. However, both processes must have been active, as the Imperial Valley is part of the Salton Trough, a pull-apart sedimentary basin that evolved over the past 4 or 5 m.y. To investigate the interrelations of these factors, we consider a one-dimensional model of basin formation in which the lower crustal gabbro and upper crustal sediments accumulated simultaneously as the crust extended and sedimentation kept pace with isostatic subsidence. For parameters appropriate for the Salton Trough, increasing the extension rate has little effect on surface heat flow because it increases effects of heating by intrusion and cooling by sedimentation in a compensating manner; it does, however, result in progressively increasing lower crustal temperatures. Analytical results suggest that the average extensional strain rate during formation of the trough was ∼20–50%/m.y. (∼1014 s−1); slower rates are inadequate to account for the present composition of the crust, and faster rates would probably cause massive crustal melting. To achieve the differential velocities of the Pacific plate at one end of the trough and North American plate at the other with this strain rate, extension must have, on the average, been distributed (or shifted about) over a spreading region ∼150 km wide. This is about 10 times wider than the present zone of active seismicity, suggesting that the seismic pattern is ephemeral on the time scale for the trough's formation. Narrow spreading zones are typical where sustained spreading is compensated by basaltic intrusion to form the thin oceanic crust, but where such spreading occurs in thicker continental crust, broader zones of distributed extension (with smaller strain rates) may be required for heat balance. The Salton Trough model suggests that distributed extension can be associated with substantial magmatic additions to the crust; their effect on crustal buoyancy has important implications for the relation between crustal extension and subsidence.
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  • 43
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    AGU
    In:  Journal of Geophysical Research: Oceans, 90 (C4). pp. 6953-6970.
    Publication Date: 2020-07-23
    Description: Water column inventories are calculated for bomb radiocarbon at all the stations occupied during the GEOSECS and NORPAX expeditions and for the available TTO stations. The pattern of global inventories obtained in this way suggests that a sizable portion of the bomb radiocarbon that entered the Antarctic, the northern Pacific, and the tropical ocean has been transported to the adjacent temperate zones. A strategy for utilizing these inventory anomalies as constraints on global ocean circulation models is presented. Essential to this strategy are the improvement of our knowledge of the pattern of wind speed over the ocean, the establishment of the wind speed dependence of the rate of gas exchange between the atmosphere and sea, and the continued mapping of the distribution of bomb-produced radiocarbon in the sea.
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  • 44
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    AGU
    In:  Journal of Geophysical Research: Oceans, 90 (C4). pp. 6940-6944.
    Publication Date: 2020-07-23
    Description: Comparison of the 1973 GEOSECS expedition results from the deep eastern basin of the North Atlantic with those for 1981 TTO expedition reveal no firm evidence for change in NO3, PO4, or a H4SiO4. concentration. While a 2–3 μmol/kg difference is seen for O2, it is more likely experimental than temporal in origin. The combined TTO-GEOSECS data sets reveal no evidence for ventilation of the bottom waters of the eastern basin by waters from the north.
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