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Contact zone gypsum - Carbonate sediments by electron paramagnetic resonance

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dc.contributor.author Khasanova N.
dc.contributor.author Nizamutdinov N.
dc.contributor.author Khasanov R.
dc.contributor.author Salimov R.
dc.date.accessioned 2018-09-18T20:21:43Z
dc.date.available 2018-09-18T20:21:43Z
dc.date.issued 2014
dc.identifier.issn 1314-2704
dc.identifier.uri https://dspace.kpfu.ru/xmlui/handle/net/139079
dc.description.abstract © SGEM2014. All Rights Reserved. The purpose of this work is to study geochemical features in the contact zone of gypsum - carbonate deposits by the electron paramagnetic resonance (EPR) method on the example of the typical core samples Syukeevskogo field. Choosing the annealing temperature of 350, 600 and 950 °C is associated with decomposition of organic matter and carbonates. Five different kind contact zones of gypsum-carbonate strata Syukeevskogo field along the borehole were selected. Quantitative changes of the EPR parameters: Mn<sup>2+</sup>, Fe<sup>3+</sup>, Cr<sup>3+</sup>, α and radicals caused by thermochemical effects on the rock and organic matter are presented in the diagram forms. Geochemical features installed in the contact zones such as a manganese increase in the newly formed calcite, a decrease α in sample oil-saturated, a reason of calcium excess or magnesium deficiency at increase alpha are discussed.
dc.relation.ispartofseries International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM
dc.subject Calcite
dc.subject Dolomite
dc.subject EPR
dc.subject Gypsum
dc.subject Thermal annealing
dc.title Contact zone gypsum - Carbonate sediments by electron paramagnetic resonance
dc.type Conference Paper
dc.relation.ispartofseries-volume 1
dc.collection Публикации сотрудников КФУ
dc.relation.startpage 35
dc.source.id SCOPUS13142704-2014-1-SID84910127577


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  • Публикации сотрудников КФУ Scopus [24551]
    Коллекция содержит публикации сотрудников Казанского федерального (до 2010 года Казанского государственного) университета, проиндексированные в БД Scopus, начиная с 1970г.

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