lithologically

Lithologically, sediments consist of clay, silt and fine to coarse sand.

Physically and lithologically it resembles the lunar highlands megaregolith.

The reservoir is a lithologically capped hydrothermal system with three layers of reservoirs underlying one another.

The Karadon formation is lithologically similar to the Kozlu Fm.

Lithologically, a variety of rock types have been discerned namely, igneous, metamorphic and sedimentary.

This member is lithologically similar to the older Wadhurst Clay and also has weathered red mottled clays at its top.

The formation is a lithologically distinctive stratigraphic unit that is large enough to be mappable and traceable.

The Haynesville Shale is a lithologically heterogeneous, often organic-rich, mudstone.

Lithologically, its stones are siliceous sandstone which probably come from Illumbe, the slope of Usoteguieta mountain.

Lithologically, the formation is dominated by red and grey shales with thin siltstone, limestone and sandstone interlayers.

Stratigraphically equivalent and lithologically similar sandstone extends across the international border into Canada, although stratigraphic boundaries and nomenclature can differ.

The Moine is lithologically monotonous, being dominated by psammites (metamorphosed sandstones), making lithostratigraphic correlation extremely difficult.

They have been tentatively correlated with the Moine, which they resemble lithologically and with which they share a metamorphic history.

Beds are the smallest formal unit in the hierarchy of sedimentary lithostratigraphic units, e.g. a single stratum lithologically distinguishable from other layers above and below.

A possible correlation with the lithologically similar Torridon Group, an unmetamorphosed sequence of similar age found beneath the Moine Thrust, remains unproven.

The formation is lithologically similar to the Ashdown Formation and comprises complex cyclic sequences of siltstones with sandstones and clays, typically fining upwards.

The Moine Supergroup is overlain to the south-east by the more lithologically diverse late Proterozoic to early Palaeozoic Dalradian Supergroup.

Lithologically the up to 50 meter thick Ruhpolding Formation consists of black-green to red radiolarites grading into cherty limestones, cherty marls and cherty shales.

Geologically, the city is settled in a Tertiary-Quaternary formation lithologically composed by little-consolidated lutites, with remains of flora or fauna, and numerous white-sand lenses of abundant silicon.

This site comprises a section of river just east of Netherfield in East Sussex which cuts through a lithologically varied sequence of Purbeck Beds, including marine horizons.

The Mazerolles Unit (MU), also of lower metamorphic grade and lithologically comparable to the TPU, overrides the paragneisses of the Lower Gneiss Unit from the southwest.

The hummocky deposits on Augustine's lower flanks resemble both topographically and lithologically those of the great landslide or debris avalanche that initiated the spectacular May 18, 1980 eruption of Mount St. Helens.

The timing of the tectonic movements is based mainly on comparisons with lithologically and structurally similar terranes in the Armorican Massif (Chantonnay Syncline in the Vendée) and in the Rouergue.

The Adirondack and New England Provinces include sedimentary, metasedimentary, and plutonic igneous rocks, mainly of Cambrian and Ordovician age, similar lithologically to rocks in the Blue Ridge and Piedmont Provinces to the south.