Search Results - "Pernambuco"

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  1. 1
    Different types of bowing technique for violin in the baroque and romantic eras / Izzat Syazwan Ab Halim

    Different types of bowing technique for violin in the baroque and romantic eras / Izzat Syazwan Ab Halim by Ab Halim, Izzat Syazwan

    Published 2013
    “…Historically, western bow have been made from pernambuco wood from brazil. However, pernambuco is now an endangered species which people export it regularly by international treaty. …”
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  2. 2
    Age, composition, and source of continental arc- and syn-collision granites of the Neoproterozoic Sergipano Belt, Southern Borborema Province, Brazil

    Age, composition, and source of continental arc- and syn-collision granites of the Neoproterozoic Sergipano Belt, Southern Borborema Province, Brazil by Oliveira, E., Bueno, J., McNaughton, Neal, Silva Filho, A., Nascimento, R., Donatti-Filho, J.

    Published 2015
    “…The Sergipano belt is the outcome of collision between the Pernambuco-Alagoas Domain (Massif) and the São Francisco Craton during Neoproterozoic assembly of West Gondwana. …”
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  3. 3
    Three most widely used gnss-based shoreline monitoring methods to support integrated coastal zone management policies

    Three most widely used gnss-based shoreline monitoring methods to support integrated coastal zone management policies by Goncalves, R., Awange, Joseph

    Published 2017
    “…Using a case study of the Pernambuco State ICZM in Brazil, this study evaluates three of the most commonly used GNSS-based shoreline monitoring methods, that is, relative kinematic (RK), real-time kinematic (RTK), and precise point positioning (PPP) methods. …”
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  4. 4
    Detrital zircon U-Pb geochronology and whole-rock Nd-isotope constraints on sediment provenance in the Neoproterozoic Sergipano orogen, Brazil: From early passive margins to late foreland basins

    Detrital zircon U-Pb geochronology and whole-rock Nd-isotope constraints on sediment provenance in the Neoproterozoic Sergipano orogen, Brazil: From early passive margins to late f... by Oliveira, E., McNaughton, Neal, Windley, B., Carvalho, M., Nascimento, R.

    Published 2014
    “…Our preliminary results support a model in which sediments of the Marancó and Macururé domains were deposited on a continental margin of the ancient Borborema plate before its collision with the São Francisco Craton; the Canindé domain is likely to be an aborted Neoproterozoic rift assemblage within the southern part of the Borborema plate (Pernambuco-Alagoas massif). The basal units of the Vaza Barris and Estância domains have clast sources from the São Francisco Craton and are best interpreted as passive margin sediments. …”
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