What Is Sedimentology?

Sedimentology is a discipline that studies the sedimentary processes, sedimentary processes, and geology that form sedimentary strata. Sedimentology evolved and evolved from the sedimentary part of sedimentary rock petrology, and formed a wider research content and application range. It explains the relationship between the vertical and horizontal of the sedimentary stratum, explores the characteristics of the geological records in the sedimentary stratum from multiple aspects, analyzes the cause of formation, and makes it as a theory.

Explore the physical and chemical properties of sedimentary rocks and their movement, sedimentation, and petrification (
Sedimentology is a branch of geology and the content of natural geography. The research results of sedimentology have enriched and promoted
The study of sedimentology will be more combined with the study of structural geology and geotectonics. It focuses on the deposition types and characteristics of active and passive continental margins, studies on plate suture zones and subduction zones, studies of similarities and differences in the separation of separate plates, and studies and confirms the time and trend of plate movements using sedimentology.
In comparative sedimentology, attention will be paid to the quantitative and statistical study of the differences between ancient and modern sediments. In the future development and research of sedimentology, it will be more combined with the study of structural geology and geotectonics. It is necessary to focus on the types and characteristics of the sediments of active and passive continental margins. In comparative sedimentology, attention will be paid to the quantitative and statistical study of the differences between ancient and modern sediments. Pay more attention to the practical significance of sedimentology, especially in aspects related to the genesis and distribution of layered deposits and deep-sea sedimentary deposits.
Pay more attention to the practical significance of sedimentology, especially in the aspects related to the genesis and distribution of layered deposits and deep-sea sedimentary deposits.

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