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 |
|