Seismic stratigraphy is a geologic approach to the interpretation of seismic data, allowing their application based on physical stratigraphy. Primary seismic reflections parallel the surface and nonconforming surface of the strata.
Nicholas Steno, a Danish scientist, is often credited as the founder of stratigraphy. He developed the fundamental principles of stratigraphy in the 17th century, which are still used in geology and archaeology today to study the layers of the Earth's crust.
William (Strata) Smith
Stratigraphy is the study of rock layers and layering. There are two different principles of stratigraphy. The first principle is the principle of the original horizontality. The second is the principle of lateral continuity.
STRATIGRAPHY also called historical geology , is that branch of geology which deals with the history of the rocks of earth crust with special emphasis on their approximate time of formation and the changes they have undergone since their formation.
Stratigraphy, or formation, refers to the study of strata, or rock layers. Stratigraphy is often used for geologic time markers, and it serves many uses in the scientific world.
seismic stratigraphy is very useful for interpretation of depositional environment in one hand and subsequent analysis of depositional environment, tectonic realm, and associated seismic markers (reflectors) indirectly indicate the presence fo hydrocarbons.
The termination of shallowly dipping, younger strata against more steeply dipping, older strata, or the termination of low-angle reflections in seismic data against steeper reflectionThe termination of shallowly dipping, younger strata against more steeply dipping, older strata, or the termination of low-angle reflections in seismic data against steeper reflections. Onlap is a particular pattern of reflections in seismic data that, according to principles of sequence stratigraphy, occurs during periods of transgression. s. Onlap is a particular pattern of reflections in seismic data that, according to principles of sequence stratigraphy, occurs during periods of transgression.
any two principles you think are well suitable, use them.... because this is how we make it in life baby
William (Strata) Smith
Nicholas Steno, a Danish scientist, is often credited as the founder of stratigraphy. He developed the fundamental principles of stratigraphy in the 17th century, which are still used in geology and archaeology today to study the layers of the Earth's crust.
Elizabeth L. Coward has written: 'Seismic stratigraphy of Santaren Channel, Bahamas'
Stratigraphy is the study of rock layers and layering. There are two different principles of stratigraphy. The first principle is the principle of the original horizontality. The second is the principle of lateral continuity.
Carl O. Dunbar has written: 'Principles of stratigraphy' -- subject(s): Stratigraphic Geology
Carl Owen Dunbar has written: 'Stratigraphy and correlation of the Devonian of western Tennessee' -- subject(s): Stratigraphic Geology, Geology 'Principles of stratigraphy' -- subject(s): Geology, Stratigraphic, Stratigraphic Geology
law of original horizontaly. law of superposition. law of gravity and oppositional force. law of cross-cutting relationships.
Stratigraphy is the study of the order and position of layers of archaeological remains. Its four principles are: law of original horizontality, law of superposition, law of original lateral continuity and law of cross-cutting relationships.
law of original horizontaly. law of superposition. law of gravity and oppositional force. law of cross-cutting relationships.