2025-02-23T09:01:38-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: Query fl=%2A&wt=json&json.nl=arrarr&q=id%3A%22mcm-mathkpnueduua-article-221184%22&qt=morelikethis&rows=5
2025-02-23T09:01:38-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: => GET http://localhost:8983/solr/biblio/select?fl=%2A&wt=json&json.nl=arrarr&q=id%3A%22mcm-mathkpnueduua-article-221184%22&qt=morelikethis&rows=5
2025-02-23T09:01:38-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: <= 200 OK
2025-02-23T09:01:38-05:00 DEBUG: Deserialized SOLR response
EVOLUTIONAL MODEL OF EARLY VENDIAN TRAPPEAN MAGMATISM IN SOUTH-WESTERN PART OF THE EAST-EUROPEAN PLATFORM
Stages of pericraton trappean magmatism, what showed up in south-western part of the East-European platform in connection with dissidence of supermainland of Rhodiniya and opening of paleoocean of Yapetus (Galycka geosyncline) in early Vend, are considered. Eruption of picrite and olivine basalts of...
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| Main Author: | |
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| Format: | Article |
| Language: | Ukrainian |
| Published: |
Institute of Geological Sciences, NAS of Ukraine
2010
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| Online Access: | http://geojournal.igs-nas.org.ua/article/view/221184 |
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