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  • 1
    Online Resource
    Online Resource
    Cham :Springer International Publishing :
    Keywords: Geochemistry. ; Geology. ; Mineralogy. ; Geophysics. ; Cosmology. ; Geochemistry. ; Geology. ; Mineralogy. ; Geophysics. ; Cosmology.
    Description / Table of Contents: Why Hadean?- Thermal evolution models -- Radionuclide produced isotopic variations in mantle rocks -- The Lunar surface and Late Heavy Bombardment concept -- Models of continental growth and destruction -- Plate boundary interactions through geologic history -- Hadean Jack Hills zircon geochemistry -- Hadean zircons elsewhere in the Solar System -- Proposed sources of Hadean zircons -- Could the Hadean eon have been habitable?- Morpho- and chemo-fossil evidence for the appearance of life -- Collectanea.
    Abstract: This book consolidates the latest research on the Hadean Eon - the first 500 million years of Earth history - which has permitted hypotheses of early Earth evolution to be tested, including geophysical models that include the possibility of plate tectonic-like behavior. These new observations challenge the longstanding Hadean paradigm – based on no observational evidence - of a desiccated, lifeless, continent-free wasteland in which surface petrogenesis was largely due to extraterrestrial impacts. The eon was termed “Hadean” to reflect such a hellish environment. That view began to be challenged in 2001 as results of geochemical analyses of greater than 4 billion year old zircons from Australia emerged. These data were consistent with the zircons forming in a world much more similar to today than long thought and interpreted to indicate that sediment cycling was occurring in the presence of liquid water. This new view leaves open the possibility that life could have emerged shortly after Earth accretion. The epistemic limitations under which the old paradigm persisted are closely examined. The book is principally designed as a monograph but has the potential to be used as a text for advanced graduate courses on early Earth evolution.
    Type of Medium: Online Resource
    Pages: XVI, 291 p. 65 illus., 52 illus. in color. , online resource.
    Edition: 1st ed. 2020.
    ISBN: 9783030466879
    DDC: 551.9
    Language: English
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  • 2
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Oxford Univ. Press
    Call number: M 00.0405
    Type of Medium: Monograph available for loan
    Pages: 269 S.
    Edition: 2nd ed.
    ISBN: 0195109201
    Classification:
    Stratigraphy
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 3
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    Unknown
    PANGAEA
    In:  Supplement to: Copeland, Peter; Harrison, T Mark; Heizler, Matthew T (1990): 40Ar/39Ar single-crystal dating of detrital muscovite and K-feldspar from Leg 116, southern Bengal Fan: implications for the uplift and erosion of the Himalayas. In: Cochran, JR; Stow, DAV; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 116, 93-114, https://doi.org/10.2973/odp.proc.sr.116.119.1990
    Publication Date: 2024-01-09
    Description: Detrital K-feldspars and muscovites from Ocean Drilling Program Leg 116 cores that have depositional ages from 0 to 18 Ma have been dated by the 40Ar/39Ar technique. Four to thirteen individual K-feldspars have been dated from seven stratigraphic levels, each of which have a very large range, up to 1660 Ma. At each level investigated, at least one K-feldspar yielded an age minimum which is, within uncertainty, identical to the age of deposition. One to twelve single muscovite crystals from each of six levels have also been studied. The range of muscovite ages is less than that of the K-feldspars and, with one exception, reveal only a 20-Ma spread in ages. As with the K-feldspars, each level investigated contains muscovites with mineral ages essentially identical to depositional ages. These results indicate that a significant portion of the material in the Bengal Fan is first-cycle detritus derived from the Himalayas. Therefore, the significant proportion of sediment deposited in the distal fan in the early to mid Miocene can be ascribed to a significant pulse of uplift and erosion in the collision zone. Moreover, these data indicate that during the entire Neogene, some portion of the Himalayan orogen was experiencing rapid erosion (〈= uplift). The lack of granulite facies rocks in the eastern Himalayas and Tibetan Plateau suggests that very rapid uplift must have been distributed in brief pulses in different places in the mountain belt. We suggest that the great majority of the crystals with young apparent ages have been derived from the southern slope of the Himalayas, predominantly from near the main central thrust zone. These data provide further evidence against tectonic models in which the Himalayas and Tibetan plateaus are uplifted either uniformly during the past 40 m.y. or mostly within the last 2 to 5 m.y.
    Keywords: 116-717; 116-717A; 116-718C; COMPCORE; Composite Core; DRILL; Drilling/drill rig; Joides Resolution; Leg116; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 4
    Publication Date: 2024-01-09
    Keywords: 116-717A; 116-718C; Age, maximum/old; Age, minimum/young; Age model; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Joides Resolution; Leg116; Ocean Drilling Program; ODP; Sample code/label; South Indian Ridge, South Indian Ocean
    Type: Dataset
    Format: text/tab-separated-values, 44 data points
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  • 5
    Publication Date: 2024-01-09
    Keywords: 116-717A; 116-718C; Age, dated; Age, dated standard deviation; Argon-36/Argon-39; Argon-37/Argon-39; Argon-39; Argon-40; Argon-40/Argon-39; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Joides Resolution; Laser power; Leg116; Number; Ocean Drilling Program; ODP; Sample code/label; Sample comment; South Indian Ridge, South Indian Ocean
    Type: Dataset
    Format: text/tab-separated-values, 3178 data points
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  • 6
    Publication Date: 2024-01-09
    Keywords: 116-717A; 116-718C; Age, dated; Age, dated standard deviation; Argon-36/Argon-39; Argon-37/Argon-39; Argon-39; Argon-40; Argon-40/Argon-39; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Joides Resolution; Leg116; Ocean Drilling Program; ODP; Sample code/label; Sample comment; South Indian Ridge, South Indian Ocean; Temperature, technical
    Type: Dataset
    Format: text/tab-separated-values, 1320 data points
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  • 7
    Publication Date: 2024-01-09
    Keywords: 116-717A; 116-718C; Age, dated; Age, dated standard deviation; Argon-36/Argon-39; Argon-37/Argon-39; Argon-39; Argon-40; Argon-40/Argon-39; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Joides Resolution; Leg116; Ocean Drilling Program; ODP; Sample code/label; Sample comment; South Indian Ridge, South Indian Ocean; Temperature, technical
    Type: Dataset
    Format: text/tab-separated-values, 72 data points
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  • 8
    Publication Date: 2024-01-09
    Keywords: 116-717A; 116-718C; Age, minimum/young; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Joides Resolution; Leg116; Mass; Mineral name; Ocean Drilling Program; ODP; Sample code/label; South Indian Ridge, South Indian Ocean
    Type: Dataset
    Format: text/tab-separated-values, 86 data points
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  • 9
    Electronic Resource
    Electronic Resource
    Palo Alto, Calif. : Annual Reviews
    Annual Review of Earth and Planetary Sciences 28 (2000), S. 211-280 
    ISSN: 0084-6597
    Source: Annual Reviews Electronic Back Volume Collection 1932-2001ff
    Topics: Geosciences , Physics
    Notes: Abstract A review of the geologic history of the Himalayan-Tibetan orogen suggests that at least 1400 km of north-south shortening has been absorbed by the orogen since the onset of the Indo-Asian collision at about 70 Ma. Significant crustal shortening, which leads to eventual construction of the Cenozoic Tibetan plateau, began more or less synchronously in the Eocene (50-40 Ma) in the Tethyan Himalaya in the south, and in the Kunlun Shan and the Qilian Shan some 1000-1400 km in the north. The Paleozoic and Mesozoic tectonic histories in the Himalayan-Tibetan orogen exerted a strong control over the Cenozoic strain history and strain distribution. The presence of widespread Triassic flysch complex in the Songpan-Ganzi-Hoh Xil and the Qiangtang terranes can be spatially correlated with Cenozoic volcanism and thrusting in central Tibet. The marked difference in seismic properties of the crust and the upper mantle between southern and central Tibet is a manifestation of both Mesozoic and Cenozoic tectonics. The former, however, has played a decisive role in localizing Tertiary contractional deformation, which in turn leads to the release of free water into the upper mantle and the lower crust of central Tibet, causing partial melting in the mantle lithosphere and the crust.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillian Magazines Ltd.
    Nature 409 (2001), S. 178-181 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Granitoid gneisses and supracrustal rocks that are 3,800–4,000 Myr old are the oldest recognized exposures of continental crust. To obtain insight into conditions at the Earth's surface more than 4 Gyr ago requires the analysis of yet older rocks or their mineral ...
    Type of Medium: Electronic Resource
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