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Record #88887:

Взаимоотношения ультрабазитового, базитового и щелочно-базитового платформенного магматизма (на примере Сибирской платформы)

Title: Взаимоотношения ультрабазитового, базитового и щелочно-базитового платформенного магматизма (на примере Сибирской платформы)
Title, transliterated: Vzaimootnoshenii︠a︡ ulʹtrabazitovogo, bazitovogo i shchelochno-bazitovogo platformennogo magmatizma (na primere Sibirskoĭ platformy) / V.V. Zolotukhin, I︠U︡.R. Vasilʹev.
Translated title: Interrelations of ultrabasic, basic and alkaline-basic platform magmatism (exemplified by the Siberian platform).
Author(s): Zolotukhin, V. V.
Vasilʹev, I︠U︡. R.
Vasiliėv, I︠U︡. R.
Date: 1987.
Language: Russian.
In: Geologii︠a︡ i Geofizika. (1987.), (1) (1987)
Abstract: Diversity in composition of matter of magmatic rocks is related to evolution of four discrete initial picritic (ultrabasic) melts. Mathematical modelling of crystallization process of melts agrees well with natural processes of fractional crystallization. Bulk of basites related genetically to feldspar picritic initial melt. Recurrence of paragenesis of platform magmatic formations over time is explained by their genetic relations.
Notes:

Geologii︠a︡ i Geofizika. (1) :43-54 (1987).

English summary, p.54.

Keywords: 552.3 -- Igneous rocks.
519.673 -- Modelling.
B -- Geology and soil sciences.
(*50) -- Soviet Union.
SPRI record no.: 88887

MARCXML

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005 20240328145931.0
007 ta
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040 ## ‡aUkCU-P‡beng‡eaacr
041 0# ‡arus
100 1# ‡6880-01‡aZolotukhin, V. V.
242 10 ‡aInterrelations of ultrabasic, basic and alkaline-basic platform magmatism (exemplified by the Siberian platform).‡yeng
245 10 ‡6880-02‡aVzaimootnoshenii︠a︡ ulʹtrabazitovogo, bazitovogo i shchelochno-bazitovogo platformennogo magmatizma (na primere Sibirskoĭ platformy) /‡cV.V. Zolotukhin, I︠U︡.R. Vasilʹev.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1987.
300 ## ‡ap. 43-54 :‡bdiags., tables, map.
500 ## ‡aGeologii︠a︡ i Geofizika. (1) :43-54 (1987).
500 ## ‡aEnglish summary, p.54.
520 3# ‡aDiversity in composition of matter of magmatic rocks is related to evolution of four discrete initial picritic (ultrabasic) melts. Mathematical modelling of crystallization process of melts agrees well with natural processes of fractional crystallization. Bulk of basites related genetically to feldspar picritic initial melt. Recurrence of paragenesis of platform magmatic formations over time is explained by their genetic relations.
546 ## ‡aIn Russian.
546 ## ‡aRussian transliteration entered into original records using BGN/PCGN 1947 romanisation of Russian; Cyrillic text in MARC 880 field(s) reverse transliterated from this by automated process; BGN/PCGN 1947 text then upgraded to Library of Congress romanisation.
650 07 ‡a552.3 -- Igneous rocks.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡aB -- Geology and soil sciences.‡2local
651 #7 ‡a(*50) -- Soviet Union.‡2udc
700 1# ‡6880-03‡aVasilʹev, I︠U︡. R.
700 1# ‡6880-04‡aVasiliėv, I︠U︡. R.‡g(alternative name)
773 0# ‡6880-05‡7nnas ‡tGeologii︠a︡ i Geofizika. ‡g(1) (1987) ‡wSPRI-35274
880 1# ‡6100-01/(N‡aЗолотухин, В. В.
880 10 ‡6245-02/(N‡aВзаимоотношения ультрабазитового, базитового и щелочно-базитового платформенного магматизма (на примере Сибирской платформы) /‡cВ.В. Золотухин, Ю.Р. Васильев.
880 1# ‡6700-03/(N‡aВасильев, Ю. Р.
880 1# ‡6700-04/(N‡aВасилиэв, Ю. Р.‡g(alternative name)
880 0# ‡6773-05/(N‡7nnas ‡tГеология и Геофизика. ‡g(1) (1987) ‡wSPRI-35274
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240328