Facies and sedimentation model of iron-ore sequence in Bakchar deposit; IOP Conference Series: Earth and Environmental Science; Vol. 24 : Scientific and Technical Challenges in the Well Drilling Progress, 24–27 November 2014, Tomsk, Russia

Manylion Llyfryddiaeth
Parent link:IOP Conference Series: Earth and Environmental Science
Vol. 24 : Scientific and Technical Challenges in the Well Drilling Progress, 24–27 November 2014, Tomsk, Russia.— 2015.— [012028, 7 p.]
Prif Awdur: Rudmin M. A. Maksim Andreevich
Awdur Corfforaethol: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра геологии и разведки полезных ископаемых (ГРПИ)
Awduron Eraill: Mazurov A. K. Aleksey Karpovich, Ruban A. S. Aleksey Sergeevich
Crynodeb:Title screen
This article describes the investigation in the behavior and structure features of the iron-ore sequence in Bakchar ore deposit. Five facies characterizing the typical sedimentation environments were identified based on the analysis of typomorphic attributes of ore-bearing and barren deposits. The facies where oolitic ores are localized have been determined. A conceptual sedimentation model of the Bakchar ore mineralization has been proposed. Two facies- littoral argillo-arenaceous ferriferous sediments and mobile shallow alluvium oolitics were proposed as prospecting indicators of oolite hydrogoethite ore deposits.
Режим доступа: по договору с организацией-держателем ресурса
Iaith:Saesneg
Cyhoeddwyd: 2015
Pynciau:
Mynediad Ar-lein:http://dx.doi.org/10.1088/1755-1315/24/1/012028
Fformat: Electronig Pennod Llyfr
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=639713

MARC

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330 |a This article describes the investigation in the behavior and structure features of the iron-ore sequence in Bakchar ore deposit. Five facies characterizing the typical sedimentation environments were identified based on the analysis of typomorphic attributes of ore-bearing and barren deposits. The facies where oolitic ores are localized have been determined. A conceptual sedimentation model of the Bakchar ore mineralization has been proposed. Two facies- littoral argillo-arenaceous ferriferous sediments and mobile shallow alluvium oolitics were proposed as prospecting indicators of oolite hydrogoethite ore deposits. 
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461 0 |0 (RuTPU)RU\TPU\network\2499  |t IOP Conference Series: Earth and Environmental Science 
463 0 |0 (RuTPU)RU\TPU\network\4016  |t Vol. 24 : Scientific and Technical Challenges in the Well Drilling Progress, 24–27 November 2014, Tomsk, Russia  |o [proceedings]  |f National Research Tomsk Polytechnic University (TPU)  |v [012028, 7 p.]  |d 2015 
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