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  • 14C uptake; ALOHA_Station; Calculated; Carbon, organic, total per volume; Chlorophyll a; Chlorophyll a, standard deviation; Comment; DEPTH, water; Hawaiian Islands, North Central Pacific; Hawaii Ocean Time-Series; HOT; JGOFS; JGOFS/HOT methods; Joint Global Ocean Flux Study; Moana Wave; OOS; Open ocean station; Phaeopigments; Phaeopigments, standard deviation; Salinity; ST-2
  • Plate tectonics
  • PANGAEA  (11)
  • Springer  (8)
  • American Geophysical Union  (7)
  • 1995-1999  (24)
  • 1985-1989  (2)
  • 1980-1984
  • 1940-1944
Collection
Keywords
Years
Year
  • 1
    Publication Date: 2024-02-01
    Keywords: 14C uptake; ALOHA_Station; Calculated; Carbon, organic, total per volume; Chlorophyll a; Chlorophyll a, standard deviation; Comment; DEPTH, water; Hawaiian Islands, North Central Pacific; Hawaii Ocean Time-Series; HOT; JGOFS; JGOFS/HOT methods; Joint Global Ocean Flux Study; Moana Wave; OOS; Open ocean station; Phaeopigments; Phaeopigments, standard deviation; Salinity; ST-2
    Type: Dataset
    Format: text/tab-separated-values, 96 data points
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  • 2
    Publication Date: 2024-02-01
    Keywords: 14C uptake; ALOHA_Station; Calculated; Carbon, organic, total per volume; Chlorophyll a; Chlorophyll a, standard deviation; Comment; DEPTH, water; Hawaiian Islands, North Central Pacific; Hawaii Ocean Time-Series; HOT; JGOFS; JGOFS/HOT methods; Joint Global Ocean Flux Study; Moana Wave; OOS; Open ocean station; Phaeopigments; Phaeopigments, standard deviation; Salinity; ST-2
    Type: Dataset
    Format: text/tab-separated-values, 94 data points
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  • 3
    Publication Date: 2024-02-01
    Keywords: 14C uptake; ALOHA_Station; Calculated; Carbon, organic, total per volume; Chlorophyll a; Chlorophyll a, standard deviation; Comment; DEPTH, water; Hawaiian Islands, North Central Pacific; Hawaii Ocean Time-Series; HOT; JGOFS; JGOFS/HOT methods; Joint Global Ocean Flux Study; Moana Wave; OOS; Open ocean station; Phaeopigments; Phaeopigments, standard deviation; Salinity; ST-2
    Type: Dataset
    Format: text/tab-separated-values, 96 data points
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  • 4
    Publication Date: 2024-02-01
    Keywords: 14C uptake; ALOHA_Station; Calculated; Carbon, organic, total per volume; Chlorophyll a; Chlorophyll a, standard deviation; Comment; DEPTH, water; Hawaiian Islands, North Central Pacific; Hawaii Ocean Time-Series; HOT; JGOFS; JGOFS/HOT methods; Joint Global Ocean Flux Study; Moana Wave; OOS; Open ocean station; Phaeopigments; Phaeopigments, standard deviation; Salinity; ST-2
    Type: Dataset
    Format: text/tab-separated-values, 96 data points
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  • 5
    Publication Date: 2024-02-01
    Keywords: 14C uptake; ALOHA_Station; Calculated; Carbon, organic, total per volume; Chlorophyll a; Chlorophyll a, standard deviation; Comment; DEPTH, water; Hawaiian Islands, North Central Pacific; Hawaii Ocean Time-Series; HOT; JGOFS; JGOFS/HOT methods; Joint Global Ocean Flux Study; Moana Wave; OOS; Open ocean station; Phaeopigments; Phaeopigments, standard deviation; Salinity; ST-2
    Type: Dataset
    Format: text/tab-separated-values, 96 data points
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  • 6
    Publication Date: 2024-02-01
    Keywords: 14C uptake; ALOHA_Station; Calculated; Carbon, organic, total per volume; Chlorophyll a; Chlorophyll a, standard deviation; Comment; DEPTH, water; Hawaiian Islands, North Central Pacific; Hawaii Ocean Time-Series; HOT; JGOFS; JGOFS/HOT methods; Joint Global Ocean Flux Study; Moana Wave; OOS; Open ocean station; Phaeopigments; Phaeopigments, standard deviation; Salinity; ST-2
    Type: Dataset
    Format: text/tab-separated-values, 90 data points
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  • 7
    Publication Date: 2024-02-01
    Keywords: 14C uptake; ALOHA_Station; Calculated; Carbon, organic, total per volume; Chlorophyll a; Chlorophyll a, standard deviation; Comment; DEPTH, water; Hawaiian Islands, North Central Pacific; Hawaii Ocean Time-Series; HOT; JGOFS; JGOFS/HOT methods; Joint Global Ocean Flux Study; Moana Wave; OOS; Open ocean station; Phaeopigments; Phaeopigments, standard deviation; Salinity; ST-2
    Type: Dataset
    Format: text/tab-separated-values, 96 data points
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  • 8
    Publication Date: 2024-02-01
    Keywords: 14C uptake; ALOHA_Station; Calculated; Carbon, organic, total per volume; Chlorophyll a; Chlorophyll a, standard deviation; Comment; DEPTH, water; Hawaiian Islands, North Central Pacific; Hawaii Ocean Time-Series; HOT; JGOFS; JGOFS/HOT methods; Joint Global Ocean Flux Study; Moana Wave; OOS; Open ocean station; Phaeopigments; Phaeopigments, standard deviation; Salinity; ST-2
    Type: Dataset
    Format: text/tab-separated-values, 95 data points
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  • 9
    Publication Date: 2024-02-01
    Keywords: 14C uptake; ALOHA_Station; Calculated; Carbon, organic, total per volume; Chlorophyll a; Chlorophyll a, standard deviation; Comment; DEPTH, water; Hawaiian Islands, North Central Pacific; Hawaii Ocean Time-Series; HOT; JGOFS; JGOFS/HOT methods; Joint Global Ocean Flux Study; Moana Wave; OOS; Open ocean station; Phaeopigments; Phaeopigments, standard deviation; Salinity; ST-2
    Type: Dataset
    Format: text/tab-separated-values, 95 data points
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  • 10
    Publication Date: 2024-02-01
    Keywords: 14C uptake; ALOHA_Station; Calculated; Carbon, organic, total per volume; Chlorophyll a; Chlorophyll a, standard deviation; Comment; DEPTH, water; Hawaiian Islands, North Central Pacific; Hawaii Ocean Time-Series; HOT; JGOFS; JGOFS/HOT methods; Joint Global Ocean Flux Study; Moana Wave; OOS; Open ocean station; Phaeopigments; Phaeopigments, standard deviation; Salinity; ST-2
    Type: Dataset
    Format: text/tab-separated-values, 96 data points
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  • 11
    Publication Date: 2024-02-01
    Keywords: 14C uptake; ALOHA_Station; Calculated; Carbon, organic, total per volume; Chlorophyll a; Chlorophyll a, standard deviation; Comment; DEPTH, water; Hawaiian Islands, North Central Pacific; Hawaii Ocean Time-Series; HOT; JGOFS; JGOFS/HOT methods; Joint Global Ocean Flux Study; Moana Wave; OOS; Open ocean station; Phaeopigments; Phaeopigments, standard deviation; Salinity; ST-2
    Type: Dataset
    Format: text/tab-separated-values, 96 data points
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  • 12
    Electronic Resource
    Electronic Resource
    Springer
    International journal of earth sciences 85 (1996), S. 705-722 
    ISSN: 1437-3262
    Keywords: China ; Kunlun ; Kara-Kunlun ; Proto-Tethys ; Paleo-Tethys ; Kudi ophiolite ; Kengxiwar lineament ; Plate tectonics ; Accretion mylonites
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The northern part of the western Kunlun (southern margin of the Tarim basin) represents a Sinian rifted margin. To the south of this margin, the Sinian to Paleozoic Proto-Tethys Ocean formed. South-directed subduction of this ocean, beneath the continental southern Kunlun block during the Paleozoic, resulted in the collision between the northern and southern Kunlun blocks during the Devonian. The northern part of the Paleo-Tethys Ocean, located to the south of the southern Kunlun, was subducted to the north beneath the southern Kunlun during the Late Paleozoic to Early Mesozoic. This caused the formation of a subduction-accretion complex, including a sizeable accretionary wedge to the south of the southern Kunlun. A microcontinent (or oceanic plateau?), which we refer to as “Uygur terrane,” collided with the subduction complex during the Late Triassic. Both elements together represent the Kara-Kunlun. Final closure of the Paleo-Tethys Ocean took place during the Early Jurassic when the next southerly located continental block collided with the Kara-Kunlun area. From at least the Late Paleozoic to the Early Jurassic, the Tarim basin must be considered a back-arc region. The Kengxiwar lineament, which “connects” the Karakorum fault in the west and the Ruogiang-Xingxingxia/Altyn-Tagh fault zone in the east, shows signs of a polyphase strike-slip fault along which dextral and sinistral shearing occurred.
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  • 13
    Electronic Resource
    Electronic Resource
    Springer
    International journal of earth sciences 84 (1995), S. 319-333 
    ISSN: 1437-3262
    Keywords: Andesites ; Plate tectonics ; Great Caucasus
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract During the Jurassic the major tectonic units of the Great Caucasus (Bechasyn, Front Range, Main Range and Southern Slope zone) were affected by intensive magmatic activity. Magmatism within the Bechasyn zone, the northernmost unit, which represents the southern part of the Variscan-consolidated Skythian platform is considered here. With the beginning of the Early Jurassic this zone was reactivated by subsidence, accompanied by the deposition of epicontinental shallow water sediments. The Lower Jurassic portion of this sedimentary pile was intruded by numerous sills which display a clear temporal and spatial evolution. The older basic rocks are lower in the profile than the younger, more acidic rocks. A set of 75 samples, representing all exposed sills and their feeder-dikes, was analyzed for major and 21 trace elements. All samples appear more or less affected by alteration under lower greenschist facies conditions. However, these alterations essentially took place on local scales and did not affect the overall chemistry. According to their main element composition the rocks constitute a calc-alkaline series ranging from basaltic—andesitic to rhyolitic. Most of the samples are andesites. Chemically, these andesites closely resemble modern orogenic andesites occurring at convergent plate margins. Altogether, the field evidence and the chemical and mineralogical data obtained show the investigated rocks to be comagmatic and derived from basalt—andesitic initial melts by magmatic fractionation processes. Tholeiitic melts have to be considered as parental magmas, which according to the trace element characteristics of the basalt-andesitic rocks, were generated from an enriched peridotitic mantle source. 87Sr/86Sr isotope ratios and σ18O values confirm the mantle origin of this rock series. The observed compositional evolution can be explained as a result of olivine and clinopyroxene fractionation of the tholeitic melts followed by amphibole and plagioclase separation. 40Ar/39Ar measurements on biotite and plagioclase phenocrysts separated from these rocks vary between 190 and 180 Ma and thereby place the magmatic activity in the late Early Jurassic, in good agreement with the stratigraphic observations. Genetically, the calc-alkaline rocks are related to a subduction zone of the Andean type. Their chemical and isotopic compositions and their age setting corroborate the plate tectonic models for the evolution of the Caucasus orogenic belt during the Jurassic.
    Type of Medium: Electronic Resource
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  • 14
    Electronic Resource
    Electronic Resource
    Springer
    International journal of earth sciences 85 (1996), S. 409-437 
    ISSN: 1437-3262
    Keywords: Plate tectonics ; Continental drift ; Paleoclimate ; Numerical climate models ; Gateways ; Orography ; Rain shadow ; Rift valley ; Plateau uplift ; Volcanism
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Tectonics and climate are both directly and indirectly related. The direct connection is between uplift, atmospheric circulation, and the hydrologic cycle. The indirect links are via subduction, volcanism, the introduction of gasses into the atmosphere, and through erosion and consumption of atmospheric gases by chemical weathering. Rifting of continental blocks involves broad upwarping followed by subsidence of a central valley and uplift of marginal shoulders. The result is an evolving regional climate which has been repeated many times in the Phanerozoic: first a vapor-trapping arch, followed by a rift valley with fresh-water lakes, culminating in an arid rift bordered by mountains intercepting incoming precipitation. Convergence tectonics affects climate on a larger scale. A mountain range is a barrier to atmospheric circulation, especially if perpendicular to the circulation. It also traps water vapor converting latent to sensible heat. Broad uplift results in a shorter path for both incoming and outgoing radiation resulting in seasonal climate extremes with reversals of atmospheric pressure and enhanced monsoonal circulation. Volcanism affects climate by introducing ash and aerosols into the atmosphere, but unless these are injected into the stratosphere, they have little effect. Stratospheric injection is most likely to occur at high latitudes, where the thickness of the troposphere is minimal. Volcanoes introduce CO2, a greenhouse gas, into the atmosphere. Geochemical effects of tectonic uplift and unroofing relate to the weathering of silicate rocks, the means by which CO2 is removed from the atmosphere-ocean system on long-term time scales.
    Type of Medium: Electronic Resource
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  • 15
    Electronic Resource
    Electronic Resource
    Springer
    Studia geophysica et geodaetica 39 (1995), S. 375-388 
    ISSN: 1573-1626
    Keywords: Plate tectonics ; convergent plate margins ; Wadati-Benioff zones ; calc-alkaline volcanism ; fossil plate boundaries
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying , Geosciences , Physics
    Notes: Summary The discovery of paleoplates buried in the upper mantle leads to an interpretation of the subduction as a discontinuous process running in cycles and shifting the place of its operation in or against the direction of ocean floor spreading. This mechanism explains the distribution of calc-alkaline volcanism of different age in fossil convergent plate boundaries. The establishment of regular spatial correlation of the aseismic gap in the Wadati-Benioff zones with the distribution of calc-alkaline volcanism enables to reconstruct fossil plate boundaries and to define allochtonous terranes in apparently homogeneous continental plates. The hampering effect of the ocean floor morphology and of the fragments of continental plates approaching the trench, which substantially influences the rates of subduction and the geodynamic history of active continental margins in different domains along the trench, allows us to understand the complicated geological development of continental wedges in fossil convergent plate margins. The establishment of the segmented nature of active subduction zones and the dramatic morphology of the lower limit of the active subducted slab along the trench help us to interpret extensive lateral gaps in volcanic chains overlying active as well as fossil subduction zones.
    Type of Medium: Electronic Resource
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  • 16
    Electronic Resource
    Electronic Resource
    Springer
    Geologische Rundschau 84 (1995), S. 319-333 
    ISSN: 0016-7835
    Keywords: Key words Andesites ; Plate tectonics ; Great Caucasus
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract. During the Jurassic the major tectonic units of the Great Caucasus (Bechasyn, Front Range, Main Range and Southern Slope zone) were affected by intensive magmatic activity. Magmatism within the Bechasyn zone, the northernmost unit, which represents the southern part of the Variscan-consolidated Skythian platform is considered here. With the beginning of the Early Jurassic this zone was reactivated by subsidence, accompanied by the deposition of epicontinental shallow water sediments. The Lower Jurassic portion of this sedimentary pile was intruded by numerous sills which display a clear temporal and spatial evolution. The older basic rocks are lower in the profile than the younger, more acidic rocks. A set of 75 samples, representing all exposed sills and their feeder-dikes, was analyzed for major and 21 trace elements. All samples appear more or less affected by alteration under low greenschist facies conditions. However, these alterations essentially took place on local scales and did not affect the overall chemistry. According to their main element composition the rocks constitute a calc-alkaline series ranging from basaltic--andesitic to rhyolitic. Most of the samples are andesites. Chemically, these andesites closely resemble modern orogenic andesites occurring at convergent plate margins. Altogether, the field evidence and the chemical and mineralogical data obtained show the investigated rocks to be comagmatic and derived from basalt--andesitic initial melts by magmatic fractionation processes. Tholeiitic melts have to be considered as parental magmas, which according to the trace element characteristics of the basalt-andesitic rocks, were generated from an enriched peridotitic mantle source. 87Sr/86Sr isotope ratios and δ18O values confirm the mantle origin of this rock series. The observed compositional evolution can be explained as a result of olivine and clinopyroxene fractionation of the tholeiitic melts followed by amphibole and plagioclase separation. 40Ar/39Ar measurements on biotite and plagioclase phenocrysts separated from these rocks vary between 190 and 180 Ma and thereby place the magmatic activity in the late Early Jurassic, in good agreement with the stratigraphic observations. Genetically, the calc-alkaline rocks are related to a subduction zone of the Andean type. Their chemical and isotopic compositions and their age setting corroborate the plate tectonic models for the evolution of the Caucasus orogenic belt during the Jurassic.
    Type of Medium: Electronic Resource
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  • 17
    ISSN: 0016-7835
    Keywords: Key words China ; Kunlun ; Kara-Kunlun ; Proto-Tethys ; Paleo-Tethys ; Kudi ophiolite ; Kengxiwar lineament ; Plate tectonics ; Accretion mylonites
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  The northern part of the western Kunlun (southern margin of the Tarim basin) represents a Sinian rifted margin. To the south of this margin, the Sinian to Paleozoic Proto-Tethys Ocean formed. South-directed subduction of this ocean, beneath the continental southern Kunlun block during the Paleozoic, resulted in the collision between the northern and southern Kunlun blocks during the Devonian. The northern part of the Paleo-Tethys Ocean, located to the south of the southern Kunlun, was subducted to the north beneath the southern Kunlun during the Late Paleozoic to Early Mesozoic. This caused the formation of a subduction-accretion complex, including a sizeable accretionary wedge to the south of the southern Kunlun. A microcontinent (or oceanic plateau?), which we refer to as "Uygur terrane," collided with the subduction complex during the Late Triassic. Both elements together represent the Kara-Kunlun. Final closure of the Paleo-Tethys Ocean took place during the Early Jurassic when the next southerly located continental block collided with the Kara-Kunlun area. From at least the Late Paleozoic to the Early Jurassic, the Tarim basin must be considered a back-arc region. The Kengxiwar lineament, which "connects" the Karakorum fault in the west and the Ruoqiang-Xingxingxia/Altyn-Tagh fault zone in the east, shows signs of a polyphase strike-slip fault along which dextral and sinistral shearing occurred.
    Type of Medium: Electronic Resource
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  • 18
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    Springer
    In:  Houston, Springer, vol. Developments in Petroleum Science vol. 15B, no. Publ. No. 12, pp. 9, (ISBN: 3-540-31080-0)
    Publication Date: 1987
    Keywords: Textbook of geology ; Structural geology ; Plate tectonics
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  • 19
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    American Geophysical Union
    In:  U.S. National Report to International Union of Geodesy and Geophysics 1991 - 1994. Contributions in Dynamics of the Solid Earth and Other Planets, ed. by R. A. Pielke, Washington, D.C., American Geophysical Union, vol. 10, no. 28, pp. 309-314
    Publication Date: 1995
    Keywords: Seismics (controlled source seismology) ; Deep seismic sounding (espec. cont. crust) ; Plate tectonics ; Review article
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  • 20
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    Unknown
    American Geophysical Union
    In:  U.S. National Report to International Union of Geodesy and Geophysics 1991 - 1994. Contributions in Dynamics of the Solid Earth and Other Planets, ed. by, Washington, D.C., American Geophysical Union, vol. 10, no. 302, pp. 365-369
    Publication Date: 1995
    Keywords: Plate tectonics ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Seismicity ; Geodesy ; Review article
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  • 21
    Publication Date: 1989
    Keywords: Proceedings of a conference ; Geodesy ; Plate tectonics ; Muller
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  • 22
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    Unknown
    American Geophysical Union
    In:  Bull., Open-File Rept., U.S. National Report to International Union of Geodesy and Geophysics 1991 - 1994, Washington, D.C., American Geophysical Union, vol. 65, no. 1, pp. 23-40, (ISBN 0080419208)
    Publication Date: 1995
    Keywords: Review article ; Seismology ; Tectonics ; Plate tectonics ; Volcanology ; Earthquake hazard ; Earthquake precursor: prediction research ; Earth rotation ; Geochemistry ; Nuclear explosion ; Source ; Deep seismic sounding (espec. cont. crust) ; GeodesyY ; Chaotic behaviour ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Rock mechanics ; remote ; sensing ; Mineralogy ; Geodesy ; Global Positioning System ; Very Long Baseline Interferometry ; Satellite Laser Ranging ; Gravimetry, Gravitation ; Planetology
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  • 23
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    American Geophysical Union
    In:  Washington, American Geophysical Union, vol. 1, (ISBN 0-521-81734-X)
    Publication Date: 1995
    Keywords: Handbook of geophysics ; Plate tectonics ; TIDES ; Geomagnetics ; Geothermics ; Seismology ; Geoelectrics ; Earth model, also for more shallow analyses ! ; Gravimetry, Gravitation ; Paleomagnetism ; isotopes ; Geochemistry ; Oceanography ; Volcanology ; physical ; constants
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  • 24
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    Unknown
    American Geophysical Union
    In:  Professional Paper, Global Earth Physics: A Handbook of Physical Constants, Washington, American Geophysical Union, vol. 1, no. 16, pp. 66-87, (ISBN: 3-540-23712-7)
    Publication Date: 1995
    Keywords: Plate tectonics ; Modelling ; Review article ; Geodesy ; Paleomagnetism
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  • 25
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    Unknown
    American Geophysical Union
    In:  U.S. National Report to International Union of Geodesy and Geophysics 1991 - 1994. Contributions in Dynamics of the Solid Earth and Other Planets, ed. by R. A. Pielke, Washington, D.C., American Geophysical Union, vol. C 560, 183 pp., no. PL-TR-91-2097, pp. 371-377, (ISBN 3-933346-037)
    Publication Date: 1995
    Keywords: Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Geodesy ; Very Long Baseline Interferometry ; Satellite Laser Ranging ; Global Positioning System ; Plate tectonics ; Review article
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  • 26
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    American Geophysical Union
    In:  U.S. National Report to International Union of Geodesy and Geophysics 1991 - 1994. Contributions in Dynamics of the Solid Earth and Other Planets, ed. by R. A. Pielke, Washington, D.C., American Geophysical Union, vol. C 560, 183 pp., no. AFGL-TR-88-0314, pp. 413-418, (ISBN 3-933346-037)
    Publication Date: 1995
    Keywords: Plate tectonics ; evolution ; GeodesyY ; Review article
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