Showing 1,281 - 1,283 results of 1,283 for search '"Ordovician"', query time: 0.08s Refine Results
  1. 1281

    Estratigrafía de las rocas metasedimentarias (Neoproterozoico-Cámbrico) de la Sierra de Mojotoro, Cordillera Oriental Argentina by Pamela A. Aparicio González, María Cristina Moya, Agnes Impiccini

    Published 2010-12-01
    “…<br>The basement of Argentine Eastern Cordillera is an heterogeneous succession of siliciclastic and chemical rocks of Neoproterozoic-Early Cambrian age, identified as the "Precambrian basement" (Keidel, 1910) underlying with angular unconformity the Cambrian and Ordovician deposits of the Mesón and Santa Victoria Groups. …”
    Get full text
    Article
  2. 1282

    Provenance, protolith and metamorphic ages of jadeite-bearing orthogneiss and host paragneiss at Tavagnasco, the Sesia Zone, Lower Aosta Valley, Italy by J. A. Gilotti, W. C. McClelland, S. Schorn, R. Compagnoni, M. A. Coble, M. A. Coble

    Published 2023-08-01
    “…The cores have <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M19" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><mi mathvariant="normal">Th</mi><mo>/</mo><mi mathvariant="normal">U</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="29pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="66336532033b9fae90efac8c3cb90ed2"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-35-645-2023-ie00002.svg" width="29pt" height="14pt" src="ejm-35-645-2023-ie00002.png"/></svg:svg></span></span> <span class="inline-formula">=</span> 0.1 and negative Eu anomalies indicative of an igneous protolith, which we interpret to have crystallized in the Ordovician at 780 <span class="inline-formula"><sup>∘</sup></span>C, based on Ti-in-zircon measurements. …”
    Get full text
    Article
  3. 1283

    Complex <sup>40</sup>Ar&thinsp;∕&thinsp;<sup>39</sup>Ar age spectra from low-grade metamorphic rocks: resolving the input of detrital and metamorphic components in a case study fro... by A. Reid, A. Reid, M. Forster, W. Preiss, W. Preiss, A. Caruso, S. Curtis, S. Curtis, T. Wise, D. Vasegh, N. Goswami, G. Lister

    Published 2022-07-01
    “…<p>In this study, we provide <span class="inline-formula"><sup>40</sup></span>Ar <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M8" display="inline" overflow="scroll" dspmath="mathml"><mo>/</mo></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="fb147fccdcf98a9911cf3d26a8f6dc33"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="gchron-4-471-2022-ie00004.svg" width="8pt" height="14pt" src="gchron-4-471-2022-ie00004.png"/></svg:svg></span></span> <span class="inline-formula"><sup>39</sup></span>Ar geochronology data from a suite of variably deformed rocks from a region of low-grade metamorphism within the Cambro–Ordovician Delamerian Orogen, South Australia. Low-grade metamorphic rocks such as these can contain both detrital minerals and minerals newly grown or partly recrystallised during diagenesis and metamorphism. …”
    Get full text
    Article