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...eys because it is a simple, three-layer stratigraphic package: resistive [[basalt]]s over conductive sediments, which in turn overlie resistive [[Metamorphic * [[Basalt]]s thin to the east

Due to interaction with seawater, magma crystallizes as pillow lava with basalt composition. Oceanic crust is not homogenous structurally. Keary and Vine<r ...ranging from 6.5 – 7.6 km s-1, represents that rocks are more felsic than basalt constructing the lower continental crust. Roberts and Bally<ref>Roberts, D.

...azil, and its role in understanding the Paran_a-Etendeka Continental Flood Basalt Province: J. Volcanol. Geotherm. Res., v. 216, p. 74–82.</ref><ref name=R

...was accommodated in the flexural depression originated by the load of the basalt pile. This was the last significant episode of subsidence in the Paraná Ba ...ltrate and, thus, form the aquifer. The water has first to infiltrate the basalt through the fractures and through the porous until it percolates into the s

* Basalt http://geology.com/rocks/basalt.shtml

...nceandengineering/rocklibrary/viewglossrecord.php?Term=tholeiite tholeitic basalt]s underlying the sedimentary section of the northern Rosario belt and Cifue ...nta Formation]]s. The outpouring of [http://geology.com/rocks/basalt.shtml basalt] continued forming the slightly younger [[Nueva Maria Formation]] in the so

! Element !! Ultrabasic Rock !! Basalt !! Granite !! Shale !! Limestone ...nates from coarse porphyritic granite, biotite granite, Bima Sandstone and basalt.<ref name=Adeyinka /> Arsenic was determined using Inductively Coupled Plas