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  • 1
    Publication Date: 2024-03-31
    Keywords: 40Ar/39Ar geochronology; Age, mineral; Age, standard deviation; Analysis; argon; biotite; calculated, 2 sigma; ELEVATION; Geological sample; GEOS; Himalaya; hornblende; LATITUDE; LONGITUDE; Marsyangdi_Valley; Mineral age, Biotite; muscovite; Sample ID; thermochronology
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 2
    Publication Date: 2024-03-31
    Keywords: 40Ar/39Ar geochronology; Age, mineral; Age, standard deviation; Analysis; argon; biotite; calculated, 2 sigma; ELEVATION; Geological sample; GEOS; Himalaya; hornblende; LATITUDE; LONGITUDE; Marsyangdi_Valley; Mineral age, Biotite; muscovite; Sample ID; thermochronology
    Type: Dataset
    Format: text/tab-separated-values, 160 data points
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  • 3
    Publication Date: 2024-03-31
    Keywords: 40Ar/39Ar geochronology; Age, mineral; Age, standard deviation; Analysis; argon; biotite; calculated, 2 sigma; ELEVATION; Geological sample; GEOS; Himalaya; hornblende; LATITUDE; LONGITUDE; Marsyangdi_Valley; Mineral age, Biotite; muscovite; Sample ID; thermochronology
    Type: Dataset
    Format: text/tab-separated-values, 80 data points
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  • 4
    Publication Date: 2024-04-20
    Keywords: 40Ar/39Ar geochronology; argon; biotite; Geological sample; GEOS; Himalaya; hornblende; Marsyangdi_Valley; muscovite; thermochronology
    Type: Dataset
    Format: application/vnd.openxmlformats-officedocument.spreadsheetml.sheet, 1.2 MBytes
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  • 5
    Publication Date: 2024-04-20
    Description: This dataset contains 40Ar/39Ar bedrock ages measured from 20 hornblende, 9 biotite, and 40 muscovite grains collected from the Marsyangdi valley of central Nepal. The samples were all collected from medium to high-grade metamorphic rocks, to add to already available thermochronometric datasets in the region, and better constrain the exhumation history of the central Himalayas. Measurement of the hornblende and biotite ages were performed using a step-heating method. However, measurement of the muscovite ages was performed using either a step-heating, or a total fusion method.
    Keywords: 40Ar/39Ar geochronology; argon; biotite; Himalaya; hornblende; muscovite; thermochronology
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 6
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillian Magazines Ltd.
    Nature 434 (2005), S. 1008-1011 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Recent convergence between India and Eurasia is commonly assumed to be accommodated mainly along a single fault—the Main Himalayan Thrust (MHT)—which reaches the surface in the Siwalik Hills of southern Nepal. Although this model is consistent with geodetic, geomorphic and ...
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1365-3121
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Determinations of the absolute age of cleavage formation can provide fundamental information about the evolution of orogenic belts. However, when applied to cleavages in slates and phyllites, conventional dating methods are complicated by problems related to mineral separation and the presence of multiple cleavage generations. In situ high-spatial-resolution 40Ar/39Ar laser microprobe geochronology and microstructural observations indicate that the age of cleavage formation in slates and phyllites can be constrained by analysing zones of tightly packed cleavage domains. Three regionally developed cleavages (S2, S3, and S4) are present in the northern Taconic Allochthon of Vermont and New York. Representative samples were studied from a variety of localities where these cleavages, which are defined by white micas, are well developed. In the suite of samples, only S3 and S4 are expressed as domains that are sufficiently wide and spatially isolated in thin section to permit quantitative 40Ar/39Ar geochronology. Mean 40Ar/39Ar laser microprobe ages for these domains are 370.7 ± 1.0 Myr for S3 and 345.5 ± 1.7 Myr for S4. Because estimates of the Ar closure temperature for white micas are substantially higher than the inferred growth temperatures of the micas defining S3 and S4, these values are interpreted as periods since cleavage formation. This interpretation is consistent with independent geochronological constraints on the age of the Acadian orogeny in the region.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 374 (1995), S. 49-52 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The tectonic evolution of the Himalayas and Tibet since the Palaeogene collision between India and Asia has been controlled by three classes of deformational structures. The most obvious features are east-striking, north-dipping thrust fault systems and subordinate folds related to shortening ...
    Type of Medium: Electronic Resource
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  • 9
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2013. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research: Earth Surface 118 (2013): 1333–1341, doi:10.1002/jgrf.20091.
    Description: Detrital mineral thermochronology of modern sediments is a valuable tool for interrogating landscape evolution. Detrital zircon (U-Th)/He thermochronology is of particular interest because zircons are durable and withstand transport in glacial and fluvial systems far better than, for example, apatite. However, because of the time-intensive nature of conventional zircon (U-Th)/He thermochronology, most previous studies of this kind have relied on data for a few tens of grains, even though conventional wisdom holds that a substantially larger number is necessary for a robust characterization of the population of cooling ages in a sample. Here, we introduce a microanalytical approach to detrital zircon (U-Th)/He thermochronology that addresses many factors that can complicate the interpretation of conventional zircon (U-Th)/He data, particularly with respect to alpha ejection and injection and U + Th zoning. In addition, this technique permits the effective dating of naturally abraded and broken grains, and, therefore, lessens the potential for sampling bias. We apply both conventional and laser microprobe techniques to a detrital sample from the Ladakh Range in the northwestern Indian Himalaya, showing that the two yield very similar principal modes of apparent ages. However, the laser microprobe data yield a broader spectrum of ages than that of the conventional data set, which we interpret to be caused by bias related to the selection requirements for zircons used for conventional dating. This method thus provides a time-efficient route to obtaining a higher-resolution distribution of dates from a single sample, which will, in turn, yield higher-fidelity constraints regarding catchment-wide erosion rates for surface process studies.
    Description: Funding for this project was provided by NSF EAR-0642731, awarded to KVH and a Lewis and Clark Grant awarded to AT-L.
    Description: 2014-01-26
    Keywords: Thermochronology ; Zircon ; Laser microprobe
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: text/plain
    Format: application/pdf
    Format: image/tiff
    Format: application/vnd.ms-excel
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  • 10
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2004. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Tectonics 23 (2004): TC5013, doi:10.1029/2003TC001559.
    Description: The Indus River is the only major drainage in the western Himalaya and delivers a long geological record of continental erosion to the Arabian Sea, which may be deciphered and used to reconstruct orogenic growth if the modern bedload can be related to the mountains. In this study we collected thermochronologic data from river sediment collected near the modern delta. U-Pb ages of zircons spanning 3 Gyr show that only ~5% of the eroding crust has been generated since India-Asia collision. The Greater Himalaya are the major source of zircons, with additional contributions from the Karakoram and Lesser Himalaya. The 39Ar/40Ar dating of muscovites gives ages that cluster between 10 and 25 Ma, differing from those recorded in the Bengal Fan. Biotite ages are generally younger, ranging 0–15 Ma. Modern average exhumation rates are estimated at ~0.6 km/m.y. or less, and have slowed progressively since the early Miocene (~20 Ma), although fission track (FT) dating of apatites may indicate a recent moderate acceleration in rates since the Pliocene (~1.0 km/m.y.) driven by climate change. The 39Ar/40Ar and FT techniques emphasize the dominance of high topography in controlling the erosional flux to the ocean. Localized regions of tectonically driven, very rapid exhumation (e.g., Nanga Parbat, S. Karakoram metamorphic domes) do not dominate the erosional record.
    Description: Scottish Universities Environmental Research Centre (SUERC) is supported by the Scottish Universities and the British National Environmental Research Council (NERC). P. C. wishes to thank the Joint Oceanographic Institutions (JOI) for partial support of this work.
    Keywords: Himalaya ; Indus River ; Fission track ; Exhumation ; Erosion ; Thermochronology
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: text/plain
    Format: application/pdf
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