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  • 2000-2004  (53)
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Year
  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Li, Xian-hua; Wei, Gangjian; Shao, Lei; Liu, Ying; Liang, Xirong; Jian, Zhimin; Sun, Min; Wang, Pinxian (2003): Geochemical and Nd isotopic variations in sediments of the South China Sea: a response to Cenozoic tectonism in SE Asia. Earth and Planetary Science Letters, 211(3-4), 207-220, https://doi.org/10.1016/S0012-821X(03)00229-2
    Publication Date: 2024-01-09
    Description: Secular variations in geochemistry and Nd isotopic data have been documented in sediment samples at ODP Site 1148 in the South China Sea. Major and trace elements show significant changes at ca. 29.5 Ma and 26-23 Ma, whereas epsilon-Nd values show a single change at ca. 26-23 Ma. Increases in Al/Ti, Al/K, Rb/Sr, and La/Lu ratios and a decrease in the Th/La ratio of the sediments beginning at 29.5 Ma are consistent with more intense chemical weathering in the source region. The abrupt change in Nd isotopes and geochemistry at ca. 26-23 Ma coincides with a major discontinuity in the sedimentology and physical properties of the sediments, implying a drastic change in sedimentary provenance and environment at the drill site. Comparison of the Nd isotopes of sediments from major rivers flowing into the South China Sea suggests that pre-27 Ma sediments were dominantly derived from a southwestern provenance (Indochina-Sunda Shelf and possibly northwestern Borneo), whereas post-23 Ma sediments were derived from a northern provenance (South China). This change in provenance from southwest to north was largely caused by ridge jumping during seafloor spreading of the South China Sea, associated with a southwestward expansion of the ocean basin crust and a global rise in sea level. Thus, the geochemical and Nd isotopic changes in the sediments at ODP Site 1148 are interpreted as a response to a major plate reorganization in SE Asia at ca. 25 Ma.
    Keywords: 184-1144A; 184-1148; COMPCORE; Composite Core; DRILL; Drilling/drill rig; Joides Resolution; Leg184; Ocean Drilling Program; ODP; South China Sea
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 2
    Publication Date: 2024-01-09
    Keywords: 184-1148; Age model; Ageprofile Datum Description; COMPCORE; Composite Core; DEPTH, sediment/rock; Joides Resolution; Leg184; Ocean Drilling Program; ODP; South China Sea
    Type: Dataset
    Format: text/tab-separated-values, 54 data points
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  • 3
    Publication Date: 2024-01-09
    Keywords: 184-1144A; Area/locality; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Epoch; Event label; Joides Resolution; LATITUDE; Leg184; LONGITUDE; Neodymium-143/Neodymium-144 ratio; Neodymium-143/Neodymium-144 ratio, error; Ocean Drilling Program; ODP; Sample code/label; South China Sea; ε-Neodymium
    Type: Dataset
    Format: text/tab-separated-values, 150 data points
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  • 4
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Wei, Gangjian; Liu, Ying; Li, Xian-hua; Shao, Lei; Fang, Dianyong (2004): Major and trace element variations of the sediments at ODP Site 1144, South China Sea, during the last 230 ka and their paleoclimate implications. Palaeogeography, Palaeoclimatology, Palaeoecology, 212(3-4), 331-342, https://doi.org/10.1016/j.palaeo.2004.06.011
    Publication Date: 2024-04-16
    Description: We present here the major and trace element data of the sediments at ODP Site 1144 of the last 230 ka with time resolution about 1.5 kyr to investigate their relations to the climate changes. Estimated from TiO2 and CaO contents, over 70% in weight of the sediments are terrestrial materials, and CaCO3 abundance ranges between 7% and 19%. The variation patterns of some of the major elements, such as Al, Fe, K, Mg and Mn, and some of the trace elements, such as the alkali elements (such as Rb and Cs), the alkali earth elements (such as Ba) and most transition metals (such as Sc, V, Co, Cr, Zn), well match that of the oxygen isotopes of the planktonic foraminifer, after normalized with Ti, with higher values during interglacial periods and lower values during glacial periods. Whilst the Na abundance exhibits inverse variation patterns with lower values during interglacial periods and higher values during glacial periods. However, most refractory elements, such as Y, Zr, Nb, Hf, Ta, REEs, Th and U, do not show such patterns. These agree well with the behaviors of these elements during chemical weathering. Therefore, the changes of chemical weathering intensity in South China, the source area of these sediments may account for such variation patterns. During interglacials, wet and warm climate might occur at South China, which resulted in stronger chemical weathering, and dry climate might occur during glacials, which resulted in weaker chemical weathering. Such paleoclimate interpretation agrees with those from other paleoclimate proxies, such as pollen records, indicating that change of the East Asian monsoon, especially change of the winter monsoon is the key for such paleoclimate variation patterns.
    Keywords: 184-1144A; Barium; Caesium; Calcium oxide; Cerium; Chromium; Cobalt; Copper; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Dysprosium; Erbium; Europium; Gadolinium; Gallium; Germanium; Hafnium; Holmium; Inductively coupled plasma atomic emission spectroscope (ICP-AES); Inductively coupled plasma - mass spectrometry (ICP-MS); Iron oxide, FeO; Joides Resolution; Lanthanum; Lead; Leg184; Lutetium; Magnesium oxide; Manganese oxide; Neodymium; Niobium; Ocean Drilling Program; ODP; Phosphorus pentoxide; Praseodymium; Rubidium; Samarium; Sodium oxide; South China Sea; Strontium; Tantalum; Terbium; Thorium; Thulium; Uranium; Vanadium; Ytterbium; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 4719 data points
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  • 5
    Publication Date: 2024-04-16
    Keywords: 184-1148; AGE; Aluminium oxide; Barium; Caesium; Calcium oxide; Cerium; Chromium; Cobalt; COMPCORE; Composite Core; Copper; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Dysprosium; Erbium; Europium; Gadolinium; Gallium; Hafnium; Holmium; Inductively coupled plasma atomic emission spectroscope (ICP-AES); Iron oxide, FeO; Isotope ratio mass spectrometry; Joides Resolution; Lanthanum; Lead; Leg184; Lutetium; Magnesium oxide; Neodymium; Neodymium-143/Neodymium-144 ratio; Neodymium-143/Neodymium-144 ratio, error; Nickel; Niobium; Ocean Drilling Program; ODP; Phosphorus pentoxide; Potassium oxide; Praseodymium; Rubidium; Samarium; Sample code/label; Scandium; Silicon dioxide; Sodium oxide; South China Sea; Strontium; Tantalum; Terbium; Thorium; Thulium; Titanium dioxide; Uranium; Vanadium; Ytterbium; Yttrium; Zinc; Zirconium; ε-Neodymium
    Type: Dataset
    Format: text/tab-separated-values, 7837 data points
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  • 6
    ISSN: 1440-1738
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Abstract  Major and trace elements and Sm–Nd isotopic data are presented for metabasites that are present as lenses within Paleozoic metasediments in the Chenxing and Bangxi regions, central Hainan Island, Southeast (SE) China. Most metabasites are metamorphosed cumulated gabbroic rocks tholeiitic in nature, and characterized by varying degrees of depletion in Th, Nb, Ta and light rare earth elements (LREE). Moreover, they show high positive ∈Nd(T) values of approximately +7, similar to those of mid-ocean ridge basalts (MORB). A Sm–Nd isochron age of 333 ± 12 Ma obtained for the metabasites is interpreted as their crystallization age. The combined geochemical and Sm–Nd isotopic data suggest that the metabasites were generated by dynamic partial melting from a MORB-like mantle source in an oceanic regime. These rocks probably represent remnants of fragmented oceanic crust of the eastern part of Paleo-Tethys. They were obducted onto the continental crust as part of the ‘Shilu Mélange’ in earliest Mesozoic time when southern Hainan (part of the Indochina block) collided with northern Hainan (part of South China). Alternatively, they could be formed in a volcanic rifted passive margin at the sea-floor spreading stage as part of MORB-like seaward-dipping reflector break-up packages.
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1546-170X
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Medicine
    Notes: [Auszug] Interleukin (IL)-2 and IL-15 are redundant in stimulating T-cell proliferation in vitro. Their precise role in vivo in governing T-cell expansion and T-cell homeostasis is less clear. Each may have distinct functions and regulate distinct aspects of T-cell activation. The functional receptors for ...
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature America Inc.
    Nature medicine 6 (2000), S. 866-867 
    ISSN: 1546-170X
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Medicine
    Notes: [Auszug] THE SUCCESS of allogeneic hematopoietic stem cell engraftment across major histocompatibility complex barriers can be promoted by passenger cells that are carried along in the donor bone marrow. Determination of the precise identity of these facilitating cells is a central issue in bone marrow ...
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Meccanica 35 (2000), S. 383-392 
    ISSN: 1572-9648
    Keywords: Piezoelectric material ; Rigid inclusion ; Dynamic response ; Electroelastic field ; Mechanics of Solid
    Source: Springer Online Journal Archives 1860-2000
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics , Physics
    Notes: Abstract The problem of a conducting rigid inclusion embedded in an infinite piezoelectric matrix is considered under the action of combined electromechanical impact loads. By using integral transform techniques, the mixed initial-boundary value problem for the case of anti-plane shear load and in-plane electric field is transformed into two systems of dual integral equations, the solutions of which give the singularity coefficients of electroelastic field near the inclusion tips in closed-form in the Laplace transform domain. Numerical results for the stress singularity coefficient in the physical space are presented graphically by numerically solving the resulting Fredholm integral equation and carrying out the numerical inversion of Laplace transform for a PZT-5H material with a conducting rigid line inclusion.
    Type of Medium: Electronic Resource
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  • 10
    Publication Date: 2001-04-30
    Print ISSN: 0003-6951
    Electronic ISSN: 1077-3118
    Topics: Physics
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