2025-02-23T05:18:07-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: Query fl=%2A&wt=json&json.nl=arrarr&q=id%3A%22journalsuranua-geofizicheskiy-article-111022%22&qt=morelikethis&rows=5
2025-02-23T05:18:07-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: => GET http://localhost:8983/solr/biblio/select?fl=%2A&wt=json&json.nl=arrarr&q=id%3A%22journalsuranua-geofizicheskiy-article-111022%22&qt=morelikethis&rows=5
2025-02-23T05:18:07-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: <= 200 OK
2025-02-23T05:18:07-05:00 DEBUG: Deserialized SOLR response
About PT conditions in magma chambers in the Earth's mantle
The investigation of the PT-parameters of magma in the mantle of this and other oceans is conducted. They are about 25 km and 1150 °С, 55—60 km and 1200 °С, 95 km and 1300 °С, 145 km and 1500 °С, 210 km and 1700 °С. The results are consistent with the advection-polymorphic hypothesis of deep process...
Saved in:
| Main Author: | |
|---|---|
| Format: | Article |
| Language: | rus |
| Published: |
Subbotin Institute of Geophysics of the NAS of Ukraine
2014
|
| Subjects: | |
| Online Access: | https://journals.uran.ua/geofizicheskiy/article/view/111022 |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
| id |
journalsuranua-geofizicheskiy-article-111022 |
|---|---|
| record_format |
ojs |
| spelling |
journalsuranua-geofizicheskiy-article-1110222020-10-07T11:45:12Z About PT conditions in magma chambers in the Earth's mantle Gordienko, V.V. mantle of the oceans and continents deep processes magma sources PT-parameters The investigation of the PT-parameters of magma in the mantle of this and other oceans is conducted. They are about 25 km and 1150 °С, 55—60 km and 1200 °С, 95 km and 1300 °С, 145 km and 1500 °С, 210 km and 1700 °С. The results are consistent with the advection-polymorphic hypothesis of deep processes. Subbotin Institute of Geophysics of the NAS of Ukraine 2014-12-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/111022 10.24028/gzh.0203-3100.v36i6.2014.111022 Geofizicheskiy Zhurnal; Vol. 36 No. 6 (2014); 28-57 Геофизический журнал; Том 36 № 6 (2014); 28-57 Геофізичний журнал; Том 36 № 6 (2014); 28-57 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/111022/105944 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| institution |
Geofizicheskiy Zhurnal |
| collection |
OJS |
| language |
rus |
| topic |
mantle of the oceans and continents deep processes magma sources PT-parameters |
| spellingShingle |
mantle of the oceans and continents deep processes magma sources PT-parameters Gordienko, V.V. About PT conditions in magma chambers in the Earth's mantle |
| topic_facet |
mantle of the oceans and continents deep processes magma sources PT-parameters |
| format |
Article |
| author |
Gordienko, V.V. |
| author_facet |
Gordienko, V.V. |
| author_sort |
Gordienko, V.V. |
| title |
About PT conditions in magma chambers in the Earth's mantle |
| title_short |
About PT conditions in magma chambers in the Earth's mantle |
| title_full |
About PT conditions in magma chambers in the Earth's mantle |
| title_fullStr |
About PT conditions in magma chambers in the Earth's mantle |
| title_full_unstemmed |
About PT conditions in magma chambers in the Earth's mantle |
| title_sort |
about pt conditions in magma chambers in the earth's mantle |
| description |
The investigation of the PT-parameters of magma in the mantle of this and other oceans is conducted. They are about 25 km and 1150 °С, 55—60 km and 1200 °С, 95 km and 1300 °С, 145 km and 1500 °С, 210 km and 1700 °С. The results are consistent with the advection-polymorphic hypothesis of deep processes. |
| publisher |
Subbotin Institute of Geophysics of the NAS of Ukraine |
| publishDate |
2014 |
| url |
https://journals.uran.ua/geofizicheskiy/article/view/111022 |
| work_keys_str_mv |
AT gordienkovv aboutptconditionsinmagmachambersintheearthsmantle |
| first_indexed |
2024-04-21T19:39:55Z |
| last_indexed |
2024-04-21T19:39:55Z |
| _version_ |
1796974466483355648 |