| dc.contributor.author |
Sinkina, Ekaterina Andreevna |
|
| dc.contributor.author |
Savinova, Olesya Vyacheslavovna |
|
| dc.contributor.author |
Nepryakhina, O.B. |
|
| dc.contributor.author |
Kolbysheva, Yuliya Vladimirovna |
|
| dc.date.accessioned |
2019-07-24T12:44:51Z |
|
| dc.date.available |
2019-07-24T12:44:51Z |
|
| dc.date.issued |
2016 |
|
| dc.identifier |
http://earchive.tpu.ru/handle/11683/35120 |
|
| dc.identifier.citation |
Peculiarities of pyrrhotite mineralization in the Chertovo Koryto deposit (Patom Uplands) / E. A. Sinkina [et al.] // 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. — [012011, 4 p.]. |
|
| dc.identifier.uri |
https://repository.geologyscience.ru/handle/123456789/3282 |
|
| dc.description.abstract |
Pyrrhotite mineralization of black shale gold-ore deposit in the central part of Chertovo Koryto (Patom Uplands) was studied. It was found that pyrrhotite consists of three generations, containing hexagonal and monoclinic modifications in various proportions. The increase in the monoclinic modification from the earlier to later generation was observed. |
|
| dc.language.iso |
en |
|
| dc.publisher |
IOP Publishing |
|
| dc.relation.ispartof |
IOP Conference Series: Earth and Environmental Science. Vol. 43 : Problems of Geology and Subsurface Development. — Bristol, 2016. |
|
| dc.rights |
info:eu-repo/semantics/openAccess |
|
| dc.subject |
минерализация |
|
| dc.subject |
месторождение Чертово Корыто |
|
| dc.subject |
пирротин |
|
| dc.subject |
пирротиновая минерализация |
|
| dc.subject |
сланцевые месторождения |
|
| dc.title |
Peculiarities of pyrrhotite mineralization in the Chertovo Koryto deposit (Patom Uplands) |
|
| dc.type |
Conference Paper |
|
| dc.type |
info:eu-repo/semantics/publishedVersion |
|
| dc.type |
info:eu-repo/semantics/conferencePaper |
|
| dc.identifier.doi |
10.1088/1755-1315/43/1/012011 |
|