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Preliminary results on the 3D geometric characterisation of a prograding delta-front sandbody with GPR (Rodasandstone, Eocene, Graus-Tremp basin)

机译：探地雷达三角洲前缘砂体的三维几何特征初步结果（Roda 砂岩，始新世，Graus-Tremp盆地）

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A set of GPR profiles have been recorded in order to determine the 3D geometry of a prograding delta-frontsandbody (Roda sandstone formation, Eocene, Graus-Tremp basin). Common Mid Points (CMP) also havebeen recorded to obtain the velocity of the electromagnetic wave in ground. In order to build the topsurface of a 3D prism a set of topographic points have been acquired. Most of the GPR profiles are orientedparallel to the progradation direction (NNE-SSW) and show the expected geometries. The 3D prism hasbeen built from the individual profiles, which shows the three dimensional geometry of the sandy lithosome

机译：记录了一组GPR剖面，以确定渐进的三角洲前缘和地体（Roda砂岩地层，始新世，Graus-Tremp盆地）的3D几何形状。还记录了公共中点（CMP）以获取地面中电磁波的速度。为了构建3D棱镜的顶表面，已获取了一组地形点。大多数GPR剖面的方向平行于渐进方向（NNE-SSW），并显示出预期的几何形状。 3D棱镜是根据单个轮廓构建的，它显示了砂质岩体的三维几何形状

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Coll Miquel; López Blanco M.; Marcuello Alex;
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年度 2006
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正文语种 spa
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Preliminary results on the 3D geometric characterisation of a prograding delta-front sandbody with GPR (Rodasandstone, Eocene, Graus-Tremp basin)

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