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dc.contributor.authorKoveshnikov, Aleksandr Evgenievichen
dc.contributor.authorNesterova, A. C.en
dc.contributor.authorDolgaya, Tatiana Fedorovnaen
dc.date.accessioned2016-12-16T02:57:17Z-
dc.date.available2016-12-16T02:57:17Z-
dc.date.issued2016-
dc.identifier.citationKoveshnikov A. E. Fracture system influence on the reservoirs rock formation of Ordovician-Devonian carbonates in West Siberia tectonic depression / A. E. Koveshnikov, A. C. Nesterova, T. F. Dolgaya // IOP Conference Series: Earth and Environmental Science. — 2016. — Vol. 43 : Problems of Geology and Subsurface Development : XX International Scientific Symposium of Students, Postgraduates and Young Scientists, 4–8 April 2016, Tomsk, Russia. — [012008, 7 p.].en
dc.identifier.urihttp://earchive.tpu.ru/handle/11683/35185-
dc.description.abstractDuring the Paleozoic period from the beginning of the Cambrian to the end of the Carboniferous in the boundaries of the West Siberia tectonic depression there occurred the sea, where the carbonate platforms were formed by the limestones accumulation. All the area at the end of the Carboniferous period was turned to land. Resulting from Gertsynskaya folding in the times of Permian - Triassic the formed deposits were folded and denudated to a considerable extent. Besides, the reservoir rocks of the crust of weathering including redeposited one, were formed as a result of hypergenesis, during the continental stand of the area in the near-surface zone. A new geological prospecting unit has been suggested which underlies these crusts of weathering and formed during fracture tectonic processes with hydrothermal-metasomatic limestones reworking and the processes of hydrothermal leaching and dolomitization. So, in the carbonate platforms the system of fissure zones related to tectonic disturbance was formed. This has a dendrite profile where the series of tangential, more thinned fractures deviate from the stem and finish in pores and caverns. The carbonate platforms formation in the West Siberia tectonic depression has been analyzed, their dynamics and gradual increasing from the minimal in Ordovician and Silurian to maximal at the end of the Late Devonian has been shown.en
dc.language.isoenen
dc.publisherIOP Publishingen
dc.relation.ispartofIOP Conference Series: Earth and Environmental Science. Vol. 43 : Problems of Geology and Subsurface Development. — Bristol, 2016.en
dc.rightsinfo:eu-repo/semantics/openAccessen
dc.subjectводохранилищаru
dc.subjectордовикru
dc.subjectкарбонатыru
dc.subjectЗападная Сибирьru
dc.subjectсинеклизыru
dc.subjectгеологоразведкаru
dc.subjectпластовые пробыru
dc.subjectкарбонатные породыru
dc.subjectтектонические впадиныru
dc.titleFracture system influence on the reservoirs rock formation of Ordovician-Devonian carbonates in West Siberia tectonic depressionen
dc.typeConference Paperen
dc.typeinfo:eu-repo/semantics/publishedVersionen
dc.typeinfo:eu-repo/semantics/conferencePaperen
dcterms.audienceResearchesen
local.departmentНациональный исследовательский Томский политехнический университет (ТПУ)::Институт природных ресурсов (ИПР)::Кафедра геологии и разведки полезных ископаемых (ГРПИ)ru
local.description.firstpage12008-
local.filepathhttp://dx.doi.org/10.1088/1755-1315/43/1/012008-
local.identifier.bibrecRU\TPU\network\16052-
local.identifier.colkeyRU\TPU\col\18660-
local.identifier.perskeyRU\TPU\pers\32375-
local.identifier.perskeyRU\TPU\pers\30911-
local.localtypeДокладru
local.volume43-
local.conference.nameProblems of Geology and Subsurface Development-
local.conference.date2016-
dc.identifier.doi10.1088/1755-1315/43/1/012008-
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