GPR imaging of a turbidite outcrop in Almada Basin (Brazil)

J. M. Travassos, M. Ceia, A. Carrasquilla
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Abstract

Turbidite outcrops of the on shore portion of Almada Basin are made of conglomeratic sandstones and shales of the Urucutuca Formation. Those rocks are the unique Turbidite examples of the marine transgression mega-sequence in the Brazilian passive margin, which were sedimented during late Cretaceous. They are analogues to important Campos Basin reservoirs, offshore of Rio de Janeiro State, which is the largest Brazilian oil producer basin. A combined GPR, resistivity and well log survey was planned in the region to provide information regarding rock properties, such as lithology, geometry and permeability. The survey's goal was to predict the variability on the characteristics normally encountered in this kind of deposits. The GPR survey was done in order to provide a stratigraphic interpretation.
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巴西Almada盆地浊积岩露头GPR成像
阿尔马达盆地滨岸部分浊积岩露头由乌鲁库塔组砾岩砂岩和页岩构成。这些岩石是巴西被动边缘海侵巨型层序中独特的浊积岩实例,沉积于晚白垩世。它们类似于巴西最大的产油盆地——里约热内卢州近海的Campos盆地。该地区计划采用探地雷达、电阻率和测井相结合的测量方法,以提供有关岩石性质的信息,如岩性、几何形状和渗透率。调查的目的是预测在这类矿床中通常遇到的特征的变化。进行探地雷达调查是为了提供地层解释。
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