Review of Survey activities 2014: Observed melt-season snowpack evolution on the Greenland ice sheet

In the central portion of the study area, we have defined the occurrence of two alkali-feldspar granite bodies (Serra Alkali Feldspar Granite, Guimarães et al.. Figure 8 -

The transition zone between the Pernambuco-Alagoas Domain and the Sergipano Belt (Borborema Province, NE Brazil): Geochronological constraints on the ages of deposition,

Geological mapping using remote sensing data: a comparison of five machine learning algorithms, their response to variations in the spatial distribution of training data and the

The HAND model, which in turn, defines the terrain height thresholds that fall into the susceptibility classes, was cut from the susceptible relief vectors, i.e., areas of the

The Central compartment is separated from the East compartment by the Central granite, which forms an interbasinal high between the two compartments (Figure 5). This

Figure 12 - Map demonstrating the location of microbialites of Lagoa Salgada and the area of the Lagoa do Açu State Park (Adapted from Silva

Gold is present in the matrix of the metaconglomerates and we have observed three different forms of occurrence (Fig. 10): (1) within detrital quartz grains, (2) as intergranular

m), shallow drillings (<100 m), and field data from the surroundings of the Saquinho iron mine in the Rio-Piranhas- Seridó domain of the Borborema Province, northeastern