";s:4:"text";s:13296:"Stratigraphy definition is - geology that deals with the origin, composition, distribution, and succession of strata. While the basic rule is that the lowest strata are the oldest, it's important to understand how they are formed and how they relate. Van Wagoner et al. This is very useful in archaeological science as buried soils represent former land surfaces, and their recognition can help locate archaeological sites. Examining the fossils in the rock layers can show what kinds of ancient creatures lived together at the same time. The stratigraphy of an area provides the basis for putting together the geologic history of an area. In a sequence of strata any stratum is younger than the sequence of strata on which it rests and is … stratigraphy (stră-tig -ră-fee) The study of rock layers (strata).Younger geological units overlie, embay, or intrude older units. For example, studying layers of rock can show when an area changed from a sandy seabed to a muddy swamp. define sequence stratigraphy as “… the study of rock relationships within a chronostratigraphic framework of repetitive, genetically related strata bounded by surfaces of erosion or nondeposition, or their correlative unconformities.” Paleogeographic reconstruction of facies belts at precise moments in time is the goal of the … Stratified … Lithologic Stratigraphy Or Lithostratigraphy The basic law of stratigraphy, the law of superposition, states that lower layers are older than upper layers, unless the sequence has been overturned. Stratigraphy is a branch of geology concerned with the study of rock layers and layering (stratification).It is primarily used in the study of sedimentary and layered volcanic rocks.Stratigraphy has two related subfields: lithostratigraphy (lithologic stratigraphy) and biostratigraphy (biologic stratigraphy). It is a discipline that correlates rocks and time, helping us understand how, why, and when a certain configuration of strata came to be. Stratigraphy is the study of rock layers and reconstruction of the original sequence in which they were deposited. Pedo-stratigraphy is the study of the stratigraphic and spatial relationships between surface soils and buried soils (palaeosols). Stratigraphy is the study of layered materials (strata) that were deposited over time. Concerned with Physical Stratigraphy- the study of the relationships of strata in time and space (superposition, cross-cutting, etc) Principle of Superposition. It is therefore possible to produce geological maps of the surface of a planet or satellite, and to form a stratigraphic classification to help to understand its history. Two type related subfields. Definition. 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