lithologic unit

The relationship to the term "Pottsville" and actual lithologic units is complex.

We have subdivided the tunnel route into a number of broad lithologic units.

Coring at Site 1210 recovered three lithologic units that have been separated based on composition.

Five lithologic units were delineated at Site 1126.

Coring at Site 1213 recovered four lithologic units.

Bulk sediment concentrations, measured every 1.5 m, outline the major lithologic units described above.

Correlation of the computed models with the wells drilled in the region shows that the main gross lithologic units were detected.

One lithologic unit was identified.

Four informal lithologic units were recognized.

No pore fluids were recovered from lithologic Unit II.

Chemostratigraphy studies the changes in the relative proportions of trace elements and isotopes within and between lithologic units.

Six lithologic units, including two newly named formations, were mapped on Randall, Dunira, and nearby islands.

One chert layer was penetrated in lithologic Unit III.

These pools are accumulations of oil in permeable sand lenses within less permeable lithologic units.

Analyses of texture, mineralogy, paleontology, and sedimentary structures enable definition of eight lithologic units.

Provisional structural map of the area west of Corner Brook, showing major lithologic units and structural features.

Lithologic units in close surrundings of the cave are of autochthonous blocks and allochthonous blocks.

Fluid focussing into the highly deformed regions occurs as a function of the ability of the different lithologic units to undergo volume change with deformation.

Tetrapod fossils have been found only in the lower lithologic unit of the Chañares Formation, where they are preserved almost exclusively within carbonate concretions.

The logs provide good resolution of various lithologic units and provide data required to estimate the salinity of water in sand beds prior to constructing a well.

No calcareous nannofossils or foraminifers were found in lithologic Units III or IV.

The stratigraphy of Klappa, Opalinski, and James is here revised to reflect better understanding of lithologic units within this complex tectono-stratigraphic assemblage.

A coastal cliff section near Codroy, Newfoundland exposes five distinctive lithologic units, which are defined lithologically and structurally as colluvial, lacustrine, or glacial in origin.

An unconformity from lower Miocene to upper Oligocene separates lithologic Unit I from Unit II.

Between the lithologic units UA, UB and UC, there exist contrasts in seismic wave velocities and densities.