Search Results - "Oyhantçabal, P."

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  1. 1

    Structural evolution of the Sarandí del Yí Shear Zone, Uruguay: kinematics, deformation conditions and tectonic significance by Oriolo, S., Oyhantçabal, P., Heidelbach, F., Wemmer, K., Siegesmund, S.

    “…The Sarandí del Yí Shear Zone is a crustal-scale shear zone that separates the Piedra Alta Terrane from the Nico Pérez Terrane and the Dom Feliciano Belt in…”
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    Journal Article
  2. 2

    Reassessing the polyphase Neoproterozoic evolution of the Punta del Este Terrane, Dom Feliciano Belt, Uruguay by Silva Lara, Hernan, Siegesmund, S., Oriolo, S., Hueck, M., Wemmer, K., Basei, M. A. S., Oyhantçabal, P.

    “…Some recent models challenge the position and extension of the assumed oceanic basins formed through the break-up of Rodinia, and the tectonic processes…”
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  3. 3

    Provenance of metasedimentary rocks of the western Dom Feliciano Belt in Uruguay: Insights from U–Pb detrital zircon geochronology, Hf and Nd model ages, and geochemical data by Oyhantçabal, P., Oriolo, S., Wemmer, K., Basei, M.A.S., Frei, D., Siegesmund, S.

    Published in Journal of South American earth sciences (01-06-2021)
    “…New isotopic and geochemical data for the Paleo- Meso- and Neoproterozoic metasedimentary cover of the southern Dom Feliciano Belt (Brasiliano/Pan-African) are…”
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    effect of air pollution on stone decay: the decay of the Drachenfels trachyte in industrial, urban, and rural environments—a case study of the Cologne, Altenberg and Xanten cathedrals by Graue, B, Siegesmund, S, Oyhantcabal, P, Naumann, R, Licha, T, Simon, K

    Published in Environmental earth sciences (01-06-2013)
    “…Severe stone deterioration is evident at the Cologne cathedral. In particular, the “Drachenfels” trachyte, which was the building material of the medieval…”
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  6. 6

    Mineralizations of the Lavalleja Group (Uruguay), a Probable Neoproterozoic Volcano-sedimentary Sequence by Sánchez-Bettucci, L., Oyhantçabal, P., Loureiro, J., Ramos, V.A., Preciozzi, F., Basei, M.A.S.

    Published in Gondwana research (01-07-2004)
    “…The Lavalleja Group is located in the southern extreme of the Dom Feliciano Belt, being tentatively correlated with the Porongos and Brusque Groups of Brazil…”
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  7. 7

    The Soca intrusion: a rapakivi granite of Uruguay by Oyhantçabal, P., Derrégibus, M.T., Muzio, R., Nardi, L.V.S.

    Published in Journal of South American earth sciences (01-03-1998)
    “…The Soca granite, emplaced in the Rı́o de la Plata Craton, is located 65 km east of Montevideo. It is a homogeneous porphyritic leucogranite, with almost 75 km…”
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    Petrography and Geochemistry of the Carapé Granitic Complex (Southeastern Uruguay) by Sánchez-Bettucci, Leda, Oyhantçabal, Pedro, Page, Stella, Ramos, Víctor A.

    Published in Gondwana research (2003)
    “…The southern sector of Uruguay was intruded by numerous granitic plutons during the Brasiliano Cycle. The granites and granodiorites of the Carapé Complex…”
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