/Interperiodica ” (Russia).
in area, is located in the southeastern Baltic Shield. The massif is divided by submeridional faults into three (northeastern Agan-ozero, central Shalozero, and southeastern Burakov) blocks. The massif is overlain by a thick cover of Qua-ternary sediments. The reconstruction of its vertical structur...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.613.5505 2023-05-15T17:01:07+02:00 /Interperiodica ” (Russia). The Lower Proterozoic Burakov Chr Ol The Pennsylvania State University CiteSeerX Archives 1423 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.613.5505 http://geo.web.ru/~ariskin/docs/papers/p00_129.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.613.5505 http://geo.web.ru/~ariskin/docs/papers/p00_129.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://geo.web.ru/~ariskin/docs/papers/p00_129.pdf text 1423 ftciteseerx 2016-01-08T14:37:46Z in area, is located in the southeastern Baltic Shield. The massif is divided by submeridional faults into three (northeastern Agan-ozero, central Shalozero, and southeastern Burakov) blocks. The massif is overlain by a thick cover of Qua-ternary sediments. The reconstruction of its vertical structure became possible only due to prospecting and mapping drilling carried out by the Karelian Geological Expedition from 1984 [1, 2], and the massif could be assigned to potentially platiniferous ones [3]. The weighted average composition of the intrusive one is close to that of komatiites [2]. The vertical section of the intrusive one is subdi-vided into the upper and lower near-contact zones (UCZ and LCZ) and the layered series (LS) with five alternating zones distinguished by prevailing cumula-tive parageneses [2]. The geochemical characteristics of the general vertical section is based on analytical data obtained for rocks from the following zones (from bottom to top): LCZ (Hole 20); ultramafic zone, UZ; Text karelia* karelian Unknown Ozero ENVELOPE(162.051,162.051,57.057,57.057) Tive ENVELOPE(12.480,12.480,65.107,65.107) |
institution |
Open Polar |
collection |
Unknown |
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ftciteseerx |
language |
English |
description |
in area, is located in the southeastern Baltic Shield. The massif is divided by submeridional faults into three (northeastern Agan-ozero, central Shalozero, and southeastern Burakov) blocks. The massif is overlain by a thick cover of Qua-ternary sediments. The reconstruction of its vertical structure became possible only due to prospecting and mapping drilling carried out by the Karelian Geological Expedition from 1984 [1, 2], and the massif could be assigned to potentially platiniferous ones [3]. The weighted average composition of the intrusive one is close to that of komatiites [2]. The vertical section of the intrusive one is subdi-vided into the upper and lower near-contact zones (UCZ and LCZ) and the layered series (LS) with five alternating zones distinguished by prevailing cumula-tive parageneses [2]. The geochemical characteristics of the general vertical section is based on analytical data obtained for rocks from the following zones (from bottom to top): LCZ (Hole 20); ultramafic zone, UZ; |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
The Lower Proterozoic Burakov Chr Ol |
spellingShingle |
The Lower Proterozoic Burakov Chr Ol /Interperiodica ” (Russia). |
author_facet |
The Lower Proterozoic Burakov Chr Ol |
author_sort |
The Lower |
title |
/Interperiodica ” (Russia). |
title_short |
/Interperiodica ” (Russia). |
title_full |
/Interperiodica ” (Russia). |
title_fullStr |
/Interperiodica ” (Russia). |
title_full_unstemmed |
/Interperiodica ” (Russia). |
title_sort |
/interperiodica ” (russia). |
publishDate |
1423 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.613.5505 http://geo.web.ru/~ariskin/docs/papers/p00_129.pdf |
long_lat |
ENVELOPE(162.051,162.051,57.057,57.057) ENVELOPE(12.480,12.480,65.107,65.107) |
geographic |
Ozero Tive |
geographic_facet |
Ozero Tive |
genre |
karelia* karelian |
genre_facet |
karelia* karelian |
op_source |
http://geo.web.ru/~ariskin/docs/papers/p00_129.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.613.5505 http://geo.web.ru/~ariskin/docs/papers/p00_129.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766054175327649792 |