2025-02-23T09:04:53-05:00 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
2025-02-23T09:04:53-05:00 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
2025-02-23T09:04:53-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: <= 200 OK
2025-02-23T09:04:53-05:00 DEBUG: Deserialized SOLR response
EVOLUTIONAL MODEL OF EARLY VENDIAN TRAPPEAN MAGMATISM IN SOUTH-WESTERN PART OF THE EAST-EUROPEAN PLATFORM

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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Bibliographic Details
Main Author: Mel’nichuk, V. G.
Format: Article
Language:Ukrainian
Published: Institute of Geological Sciences, NAS of Ukraine 2010
Online Access:http://geojournal.igs-nas.org.ua/article/view/221184
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2025-02-23T09:04:53-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: Query fl=%2A&rows=40&rows=5&wt=json&json.nl=arrarr&q=id%3A%22mcm-mathkpnueduua-article-221184%22&qt=morelikethis
2025-02-23T09:04:53-05:00 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%22mcm-mathkpnueduua-article-221184%22&qt=morelikethis
2025-02-23T09:04:53-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: <= 200 OK
2025-02-23T09:04:53-05:00 DEBUG: Deserialized SOLR response

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