2025-02-22T21:29:38-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: Query fl=%2A&wt=json&json.nl=arrarr&q=id%3A%22irk-123456789-128262%22&qt=morelikethis&rows=5
2025-02-22T21:29:38-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: => GET http://localhost:8983/solr/biblio/select?fl=%2A&wt=json&json.nl=arrarr&q=id%3A%22irk-123456789-128262%22&qt=morelikethis&rows=5
2025-02-22T21:29:38-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: <= 200 OK
2025-02-22T21:29:38-05:00 DEBUG: Deserialized SOLR response
The peculiarities of cross-correlation between two secondary precursors – radon and magnetic field variations, induced by tectonic activity

The peculiarities of cross-correlation between two secondary precursors – radon and magnetic field variations, induced by tectonic activity

A model of precursor manifestation mechanisms, stimulated by tectonic activity and some peculiarities of observer strategy, whose main task is the effective measurement of precursors in the spatial area of their occurrence on the Earth’s daylight, are considered. In particular, the applicability of...

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Bibliographic Details
Main Authors: Rusov, V.D., Maksymchuk, V.Yu., Ilić, R., Pavlovych, V.M., Bakhmutov, V.G., Saranuk, D.N., Vaschenko, V.M., Skvarč, J., Hanžič, L., Kosenko, S.I.
Format: Article
Language:English
Published: Національний антарктичний науковий центр МОН України 2006
Series:Український антарктичний журнал
Subjects:
Ядерно-фізичні дослідження Землі та атмосфери
Online Access:http://dspace.nbuv.gov.ua/handle/123456789/128262
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2025-02-22T21:29:38-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: Query fl=%2A&rows=40&rows=5&wt=json&json.nl=arrarr&q=id%3A%22irk-123456789-128262%22&qt=morelikethis
2025-02-22T21:29:38-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: => GET http://localhost:8983/solr/biblio/select?fl=%2A&rows=40&rows=5&wt=json&json.nl=arrarr&q=id%3A%22irk-123456789-128262%22&qt=morelikethis
2025-02-22T21:29:38-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: <= 200 OK
2025-02-22T21:29:38-05:00 DEBUG: Deserialized SOLR response

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