Matches in DBpedia 2014 for { <http://dbpedia.org/resource/Thermoremanent_magnetization> ?p ?o. }
Showing items 1 to 13 of
13
with 100 items per page.
- Thermoremanent_magnetization abstract "When an igneous rock cools, it acquires a thermoremanent magnetization (TRM) from the Earth's field. TRM can be much larger than it would be if exposed to the same field at room temperature (see isothermal remanence). This remanence can also be very stable, lasting without significant change for millions of years. TRM is the main reason that paleomagnetists are able to deduce the direction and magnitude of the ancient Earth's field.".
- Thermoremanent_magnetization wikiPageID "28903728".
- Thermoremanent_magnetization wikiPageRevisionID "591946484".
- Thermoremanent_magnetization hasPhotoCollection Thermoremanent_magnetization.
- Thermoremanent_magnetization subject Category:Magnetic_ordering.
- Thermoremanent_magnetization subject Category:Rock_magnetism.
- Thermoremanent_magnetization comment "When an igneous rock cools, it acquires a thermoremanent magnetization (TRM) from the Earth's field. TRM can be much larger than it would be if exposed to the same field at room temperature (see isothermal remanence). This remanence can also be very stable, lasting without significant change for millions of years. TRM is the main reason that paleomagnetists are able to deduce the direction and magnitude of the ancient Earth's field.".
- Thermoremanent_magnetization label "Thermoremanent magnetization".
- Thermoremanent_magnetization sameAs m.0ddd0l4.
- Thermoremanent_magnetization sameAs Q7783243.
- Thermoremanent_magnetization sameAs Q7783243.
- Thermoremanent_magnetization wasDerivedFrom Thermoremanent_magnetization?oldid=591946484.
- Thermoremanent_magnetization isPrimaryTopicOf Thermoremanent_magnetization.