A large number of such data have been produced over the past decades
in paleomagnetic laboratories around the world, so that the amount of available data is getting large enough to allow for global inversion models of the Holocene magnetic field.
Not exact matches
Angrites are igneous rocks, many of which are thought to have erupted onto the surface of asteroids very early
in the solar system's history and then quickly cooled, freezing their original properties — including their composition and
paleomagnetic signals —
in place.
Paleomagnetic dating — matching magnetic properties
in the sediments surrounding a fossil or artifact to ancient reversals
in the Earth's magnetic poles to determine age — later determined the tools had to have been made 3.3 million years ago.
The age of the fossils was corroborated by radiometric dating (using radioactive isotopes), the global
paleomagnetic sequence (signatures of reversals of Earth's magnetic field found
in the samples), and fossil correlations (age of other fossils).
Researchers, led by Yohannes Haile - Selassie co-authored a paper
in the Proceedings of the National Academy of science (PNAS) reporting the discovery, piecing together and analysis of a partially complete male skeleton dated by
paleomagnetic and radiometric methods to 3.6 million years ago.
The researchers say Rising Star Cave was dated using a combination of optically stimulated luminescence of sediments with uranium - thorium dating and
paleomagnetic analyses of flowstones to establish how the cave sediments relate to the geological timescale
in the Dinaledi Chamber.
Joseph L. Kirschvink et al., «
Paleomagnetic Evidence of a Low - Temperature Origin of Carbonate
in the Martian Meteorite ALH84001,» Science, Vol.
Further advances
in understanding the acquisition of magnetisation
in archeo - and
paleomagnetic data, continuing development of improved laboratory procedures and further investigations of suitability and appropriate scaling of sedimentary relative intensity records will help to reduce uncertainties
in the data, and consequently also
in the models.
Information about the magnetic field evolution prior to the times of direct observations is determined
in laboratory procedures from archeo - and
paleomagnetic material.
It's attractive
in that it explains several lines of otherwise problematic evidence (near - ubiquitous glacial sediments, including many
in paleo - low latitudes as indicated by
paleomagnetic studies, overlain by equally ubiquitous «cap carbonates» (resulting from a CO2 insolubility spike at Snowball Earth termination).
Sohl, L.E., N. Christie - Blick, and D.V. Kent, 1999:
Paleomagnetic polarity reversals
in Marinoan (ca. 600 Ma) glacial deposits of Australia: Implications for the duration of low - latitude glaciation
in Neoproterozoic time.