From surface structures to the integral depth model of the Kirovograd ore region (Ukrainian Shield). 1

The discovery of a middle-scale mantle trough in the Kirovograd ore district under uranium, gold and lithium deposits brought a new insight into metallogeny of the district and made it necessary to trace its surface structures to the M boundary.In this study, surface structures are described in more...

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Бібліографічні деталі
Дата:2010
Автори: Starostenko, V. I., Kazansky, V. I., Popov, N.I., Drogitskaya, G. M., Zayats, V. B., Makivchuk, O. F., Trypolsky, A. A., Chicherov, M. V.
Формат: Стаття
Мова:rus
Опубліковано: Subbotin Institute of Geophysics of the NAS of Ukraine 2010
Онлайн доступ:https://journals.uran.ua/geofizicheskiy/article/view/117567
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Назва журналу:Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal
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spelling journalsuranua-geofizicheskiy-article-1175672020-10-07T10:57:50Z From surface structures to the integral depth model of the Kirovograd ore region (Ukrainian Shield). 1 Starostenko, V. I. Kazansky, V. I. Popov, N.I. Drogitskaya, G. M. Zayats, V. B. Makivchuk, O. F. Trypolsky, A. A. Chicherov, M. V. The discovery of a middle-scale mantle trough in the Kirovograd ore district under uranium, gold and lithium deposits brought a new insight into metallogeny of the district and made it necessary to trace its surface structures to the M boundary.In this study, surface structures are described in more detales using numerous data from exploration drilling, relationships between the crustal Kirovograd-Novoukrainsk granitoid massif, mantle-related Korsun-Novomirgorod massif and M interface are discussed, surface and deep structures of uranium ore fields are correlated and vertical metasomatic and ore zonality of large uranium deposits is considered. Subbotin Institute of Geophysics of the NAS of Ukraine 2010-02-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/117567 10.24028/gzh.0203-3100.v32i1.2010.117567 Geofizicheskiy Zhurnal; Vol. 32 No. 1 (2010); 3-33 Геофизический журнал; Том 32 № 1 (2010); 3-33 Геофізичний журнал; Том 32 № 1 (2010); 3-33 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/117567/111609 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
institution Geofizicheskiy Zhurnal
collection OJS
language rus
format Article
author Starostenko, V. I.
Kazansky, V. I.
Popov, N.I.
Drogitskaya, G. M.
Zayats, V. B.
Makivchuk, O. F.
Trypolsky, A. A.
Chicherov, M. V.
spellingShingle Starostenko, V. I.
Kazansky, V. I.
Popov, N.I.
Drogitskaya, G. M.
Zayats, V. B.
Makivchuk, O. F.
Trypolsky, A. A.
Chicherov, M. V.
From surface structures to the integral depth model of the Kirovograd ore region (Ukrainian Shield). 1
author_facet Starostenko, V. I.
Kazansky, V. I.
Popov, N.I.
Drogitskaya, G. M.
Zayats, V. B.
Makivchuk, O. F.
Trypolsky, A. A.
Chicherov, M. V.
author_sort Starostenko, V. I.
title From surface structures to the integral depth model of the Kirovograd ore region (Ukrainian Shield). 1
title_short From surface structures to the integral depth model of the Kirovograd ore region (Ukrainian Shield). 1
title_full From surface structures to the integral depth model of the Kirovograd ore region (Ukrainian Shield). 1
title_fullStr From surface structures to the integral depth model of the Kirovograd ore region (Ukrainian Shield). 1
title_full_unstemmed From surface structures to the integral depth model of the Kirovograd ore region (Ukrainian Shield). 1
title_sort from surface structures to the integral depth model of the kirovograd ore region (ukrainian shield). 1
description The discovery of a middle-scale mantle trough in the Kirovograd ore district under uranium, gold and lithium deposits brought a new insight into metallogeny of the district and made it necessary to trace its surface structures to the M boundary.In this study, surface structures are described in more detales using numerous data from exploration drilling, relationships between the crustal Kirovograd-Novoukrainsk granitoid massif, mantle-related Korsun-Novomirgorod massif and M interface are discussed, surface and deep structures of uranium ore fields are correlated and vertical metasomatic and ore zonality of large uranium deposits is considered.
publisher Subbotin Institute of Geophysics of the NAS of Ukraine
publishDate 2010
url https://journals.uran.ua/geofizicheskiy/article/view/117567
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