तलछट-संबंधी इसके अंग्रेजी अर्थ का उदाहरण

The Narryer Gneiss Terrane is adjacent to the northernmost margin of the Yilgarn Craton and is abutted on the north by the Gascoyne Complex metasedimentary and metagranite orogen.

ZX Spectrum Plutonism (or volcanism) is the geologic theory that the igneous rocks forming the Earth originated from intrusive magmatic activity, with a continuing gradual process of weathering and erosion wearing away rocks, which were then deposited on the sea bed, re-formed into layers of sedimentary rock by heat and pressure, and raised again.

It is three miles west of Flagler Beach on CR 2001, south of SR 100, and contains the ruins of an ante-bellum plantation and its sugar mill, built of coquina, a fossiliferous sedimentary rock composed of shells.

These fossils may be studied while still partially entombed in the sedimentary rock matrix where they are preserved, or once lifted out of the matrix by a peel or transfer technique.

Erosion occurring between the eruptions deposited deep layers of sediment between the lava flows, which eventually lithified into sedimentary rock.

This happens, for example, where animal burrows penetrate into pre-existing sedimentary deposits.

It occurs in rocks which have undergone low to medium grade regional metamorphism and in contact metamorphism of high calcium sedimentary rocks.

Between the crater wall and lake is a northern margin/beach consisting of sedimentary, with little vegetation.

The Yilgarn Craton is bounded on the east-southeast by the ~1,300 Ma Albany-Fraser Orogen, composed primarily of amphibolite to greenschist facies sedimentary protolith gneisses, migmatites and granites.

The Bovey Formation is the major source in England for ball clay – a highly plastic fine-grained kaolinitic sedimentary clay typically used by the pottery industry.

To the east and northeast rocks of the complex are overlain unconformably by fine-grained Mesoproterozoic sedimentary rocks of the Edmund Basin and Collier Basin (formerly known as the Bangemall Basin).

Sedimentary microstructures, specifically, may include microscopic analogs of larger sedimentary structural features such as cross-bedding, syn-sedimentary faults, sediment slumping, cross-stratification, etc.

Metamorphism resulted in the generation of S-type and I-type granites which intruded this Palaeozoic sedimentary sequence in the New England Fold Belt.