Quantitative Seismic Interpretation demonstrates how rock physics can be applied to predict reservoir parameters, such as lithologies and pore fluids, from seismically derived attributes. ❋ Unknown (2009)
Nowadays, however, we log chips in detail using a microscope, and our lithologies, mineral percentages, textures, and descriptions go straight into a computer data base. ❋ Silver Fox (2008)
An escarpment over 300 feet (91 m) high marks the juncture between ecoregions 62a and 62b and their respective lithologies. ❋ Unknown (2008)
As different clay types derive from different lithologies via various weathering processes, radiogenic isotopes may also help in these studies not only to track point sources of clays, but also to quantify geochemically the proportions of mixed clays from different sources in the ceramics which may be difficult using other methods. ❋ Unknown (2003)
Additional "bulk" background information will be provided by isotope analysis of snail shells sampled from different bedrock lithologies. ❋ Unknown (2003)
A preliminary comparison between the sediments drilled of the Bereket valley and the weathered rocks of the different lithologies present in the study area indicates that the most likely source of the Quaternary deposits in the valley bottom is the ophiolitic mélange. ❋ Unknown (2003)
The geological map will be compared with the satellite images to specify the reflectance characteristics for the different lithologies. ❋ Unknown (2003)
The dynamic plate tectonics of the area, and the mixing of igneous, metamorphic, and sedimentary geological formations, have resulted in diverse lithologies and soils. ❋ Clinton, Bill, 1946- (2000)
The thermal areas vent through a variety of lithologies, including rhyolites, siltstones and ❋ Unknown (1998)
Among the factors evaluated are bedrock lithologies and structure, fracture patterns, ground-water conditions, soil type and thickness, and topography. ❋ Linda Gale (1998)
Basement lithologies were: quartzite including an 8.5 metre fault zone, followed by pelite, and ending in graphitic pelite.
Primary ore controls are a combination of favourable lithologies and crosscutting structural zones. ❋ Unknown (2011)
Within the primary structural corridors, all lithologies can be pervasively altered and mineralized. ❋ Unknown (2011)
Devonian volcanic rocks and Cretaceous dikes represent the most favourable host lithologies and are pervasively altered and mineralized throughout the deposit. ❋ Unknown (2011)
Boisvert (1989) describes a variety of lithologies in the region, including biotite schists and gneisses, basalts, dacites, quartzites, conglomerates, gabbros, granites and pegmatites. ❋ Unknown (2010)
Geophysical responses from the survey may reflect differing host lithologies, associated alteration assemblages and metal type and content between the different occurrences within theses broader target areas. ❋ Unknown (2010)
* Although it is difficult to determine the actual geometry of a porphyry alteration system, it is very likely that mineralization is controlled by steeply east dipping structures/lithologies. ❋ Unknown (2010)
Sample intervals were selected based on lithologies and intensity of alteration. ❋ Unknown (2010)
