2025-02-23T13:30:26-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: Query fl=%2A&wt=json&json.nl=arrarr&q=id%3A%22irk-123456789-3170%22&qt=morelikethis&rows=5
2025-02-23T13:30:26-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: => GET http://localhost:8983/solr/biblio/select?fl=%2A&wt=json&json.nl=arrarr&q=id%3A%22irk-123456789-3170%22&qt=morelikethis&rows=5
2025-02-23T13:30:26-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: <= 200 OK
2025-02-23T13:30:26-05:00 DEBUG: Deserialized SOLR response
О температуре солидуса пород мантии
The accordance of the solidus temperature (Ts) of mantle rocks to a complex of petrological and geophysical data is considered. It is proved that the relation Ts = 1013 + 3.914H − 0.0037H2 , where H is the depth in km, corresponds to this information and can be used for the construction of model...
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| Main Authors: | , |
|---|---|
| Format: | Article |
| Language: | Russian |
| Published: |
Видавничий дім "Академперіодика" НАН України
2007
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| Subjects: | |
| Online Access: | http://dspace.nbuv.gov.ua/handle/123456789/3170 |
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2025-02-23T13:30:26-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: Query fl=%2A&rows=40&rows=5&wt=json&json.nl=arrarr&q=id%3A%22irk-123456789-3170%22&qt=morelikethis
2025-02-23T13:30:26-05:00 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-123456789-3170%22&qt=morelikethis
2025-02-23T13:30:26-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: <= 200 OK
2025-02-23T13:30:26-05:00 DEBUG: Deserialized SOLR response