<HashMap><database>biostudies-literature</database><scores/><additional><submitter>Kletetschka G</submitter><funding>Ministry of Education, Youth and Science</funding><funding>Grantová Agentura České Republiky</funding><pagination>22466</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC8599688</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>11(1)</volume><pubmed_abstract>The shock exposure of the Santa Fe's impact structure in New Mexico is evidenced by large human-size shatter cones. We discovered a new magnetic mechanism that allows a magnetic detection of plasma's presence during the impact processes. Rock fragments from the impactites were once magnetized by a geomagnetic field. Our novel approach, based on Neel's theory, revealed more than an order of magnitude lower magnetizations in the rocks that were exposed to the shockwave. Here we present a support for a newly proposed mechanism where the shock wave appearance can generate magnetic shielding that allow keeping the magnetic grains in a superparamagnetic-like state shortly after the shock's exposure, and leaves the individual magnetized grains in random orientations, significantly lowering the ov</pubmed_abstract><journal>Scientific reports</journal><pubmed_title>Plasma shielding removes prior magnetization record from impacted rocks near Santa Fe, New Mexico.</pubmed_title><pmcid>PMC8599688</pmcid><funding_grant_id>LTAUSA 19141</funding_grant_id><funding_grant_id>20-08294S</funding_grant_id><pubmed_authors>Kletetschka G</pubmed_authors><pubmed_authors>Kavkova R</pubmed_authors><pubmed_authors>Ucar H</pubmed_authors></additional><is_claimable>false</is_claimable><name>Plasma shielding removes prior magnetization record from impacted rocks near Santa Fe, New Mexico.</name><description>The shock exposure of the Santa Fe's impact structure in New Mexico is evidenced by large human-size shatter cones. We discovered a new magnetic mechanism that allows a magnetic detection of plasma's presence during the impact processes. Rock fragments from the impactites were once magnetized by a geomagnetic field. Our novel approach, based on Neel's theory, revealed more than an order of magnitude lower magnetizations in the rocks that were exposed to the shockwave. Here we present a support for a newly proposed mechanism where the shock wave appearance can generate magnetic shielding that allow keeping the magnetic grains in a superparamagnetic-like state shortly after the shock's exposure, and leaves the individual magnetized grains in random orientations, significantly lowering the ov</description><dates><release>2021-01-01T00:00:00Z</release><publication>2021 Nov</publication><modification>2026-03-16T15:11:19.351Z</modification><creation>2022-02-11T13:02:08.963Z</creation></dates><accession>S-EPMC8599688</accession><cross_references><pubmed>34789763</pubmed><doi>10.1038/s41598-021-01451-8</doi></cross_references></HashMap>