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Dictionnaire français - anglais

llandovérien

Llandoverian

sciences naturelles et appliquées - iate.europa.eu

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Classification of chitinozoa (llandoverian, canada) using image analysis

Des Chitinozoaires (Llandovérien, Canada) ont étéétudiés par analyse d'images....

...Chitinozoa (Llandoverian, Canada) were studied usingimage analysis....

général - core.ac.uk -

Publications scientifiques

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Conodonts of the estill shale and bisher formation (silurian, southern ohio): biostratigraphy and distribution... The Estill belongs in the amorphognathoides Zone and is late Llandoverian to early Wenlockian....

général - core.ac.uk - PDF: kb.osu.edu

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Trilobite taphonomy of a silurian reef: attawapiskat formation,Trilobites of exhumed reefs of the Late Llandoverian Atta-wapiskat Formation of northern Ontario occur in accumu-lations that have undergone extensive taphonomic sorting....

général - core.ac.uk - PDF: palaios.geoscienceworld.org

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Tem and aem constraints on he origin and significance of chlorite-mica stacks in slates: an example from central... The stacks occur in a weakly cleaved Llandoverian mudstone, central Wales, which has a white mica (illite) crystallinity index of 0.35...

général - core.ac.uk - PDF: deepblue.lib.umich.edu

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Early silurian paleogeography and source-reservoir-cap rocks of the middle-upper yangtze region in south chinaThe lithofacies paleogeography for the three successive ages (Rhuddanian, Aeronian and Telychian) in the Middle-Upper Yangtze region of South China in the Early Silurian (Llandoverian Epoch) is reconstructed according to the concept that structures control a basin, a basin controls facies, which, in turn, control the basic geology of oil and gas....

général - core.ac.uk - PDF: www.sciencedirect.com

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Tem and aem constraints on the origin and significance of chlorite-mica stacks in slates: an example from central wales, u.k.... The stacks occur in a weakly cleaved Llandoverian mudstone, central Wales, which has a white mica (illite) crystallinity index of 0.35[deg]...

général - core.ac.uk - PDF: dx.doi.org

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