Lithostratigraphy/Related Articles
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- See also changes related to Lithostratigraphy, or pages that link to Lithostratigraphy or to this page or whose text contains "Lithostratigraphy".
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- Age (geology) [r]: The fundamental chronostratigraphic unit. [e]
- Biostratigraphy [r]: A domain of stratigraphy that involves the identification of fossils and their position relative to their occurrences in space and time. [e]
- Chronostratigraphy [r]: The branch of stratigraphy that studies the relative time relations and ages of rock bodies. [e]
- Earth science [r]: The study of the components and processes of the planet Earth. [e]
- Geochronology [r]: Science of determining the absolute age of rocks, fossils, and sediments, within a certain degree of uncertainty inherent within the method used. [e]
- Geochronometry [r]: A branch of stratigraphy and of geochronology aimed at the quantitative measurement of geologic time. [e]
- Geologic ages of earth history [r]: Measurement of the geologic history of the earth which can be broadly classified into two periods: the Precambrian supereon and the Phanerozoic eon. [e]
- Magnetostratigraphy [r]: Studies of the magnetic characteristics of rocks. [e]
- Sedimentary geology [r]: Science concerned with the physical and chemical properties of sedimentary rocks and the processes involved in their formation, including transportation, deposition, and lithification of sediments. [e]
- Stage (geology) [r]: A unit in the study of soil layers. [e]
- Stratigraphy [r]: The interdisciplinary science field that describes all rock bodies that form the Earth's crust and the manner in which they are organised into distinctive units that are then mapped. [e]
- Universe [r]: The summation of all particles and energy that exist and the space-time in which all events occur. [e]
- Asia [r]: The largest continent in both land area (with 30% of Earth's land area) and population (with 4 billion people, or 60% of Earth's population). [e]
- Stratigraphy [r]: The interdisciplinary science field that describes all rock bodies that form the Earth's crust and the manner in which they are organised into distinctive units that are then mapped. [e]