Geologia USP. Série Científica (Sep 2014)

Digital imaging and 3D virtual modeling of a block of travertine rock

  • Victor de Albuquerque Silva,
  • David Lopes de Castro,
  • Anderson de Medeiros Souza,
  • Lucila Monte Egito,
  • João Andrade dos Reis Júnior,
  • Francisco Pinheiro Lima-Filho

DOI
https://doi.org/10.5327/Z1519-874X201400030006
Journal volume & issue
Vol. 14, no. 3
pp. 75 – 96

Abstract

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Methodological procedures adopted in the digital imagery process, in a non-conventional scale, of a block of travertine rock from the quaternary age were presented on this paper. The rock, named T-Block, weighting 21.2 ton and measuring 1.60 x 1.60 x 2.70 m, was stored in the courtyard of the Laboratório Experimental de Petróleo “Kelsen Valente” (LabPetro) at the Universidade Estadual de Campinas (UNICAMP). Petrobras, the Brazilian Petroleum Company, had sponsored its shipment from Italy to Brazil in order to perform geological studies and petrophysical essays, mainly by research groups from universities and research centers of Brazil that work in the areas of reservoir characterization and 3D digital imaging. The purpose of this work was to develop a Digital Solid Model involving 3D digital imaging techniques of internal and external surfaces of the T-Block. Light Detection and Range technology and Ground Penetrating Radar were used to capture the imaging of the external and internal surfaces, respectively. Additionally, gamma ray profiles were generated by using a portable gamma-spectrometer. The use of Light Detection and Range technology combined with Ground Penetrating Radar enabled the identification and 3D mapping of three distinct radar facies, which were correlated to the three sedimentary facies already defined: “Travertine in Domes Radarfacies”, “Transitional Travertine Radarfacies” and “Laminated Travertine Radarfacies”. The gamma ray profiles revealed slight variation, in amplitude, of the radioactivity values. This is likely due to the fact that the sedimentary layers have the same mineralogical composition, which is mainly composed of carbonate sediments, with no siliciclastic clay and/or other radioactive mineral elements inside the more pelitic layers.

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