THE ERDENETUIN-OBO PORPHYRY CU-MO MAGMA CHAMBER (MONGOLIA) AS A REFLECTION OF THE PERMIAN-TRIASSIC SUPERPLUME
| dc.contributor.author | Berzina A.P. | |
| dc.contributor.author | Dobretsov N.L. | |
| dc.contributor.author | Sotnikov V.I. | |
| dc.contributor.author | Ponomarchuk V.A. | |
| dc.date.accessioned | 2022-07-18T00:49:00Z | |
| dc.date.available | 2022-07-18T00:49:00Z | |
| dc.date.issued | 2004 | |
| dc.description.abstract | Large-scale Permian-Triassic magmatism of northern and central Asia has been recently proved to be of plume origin. Based on these concepts, the present paper considers a possible relationship between the evolution of the Erdenetuin-Obo porphyry Cu-Mo magma chamber and the Siberian superplume. | |
| dc.identifier | https://www.elibrary.ru/item.asp?id=13448665 | |
| dc.identifier.citation | Doklady Earth Sciences, 2004, 399, 9, 1311-1314 | |
| dc.identifier.issn | 1028-334X | |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/38191 | |
| dc.subject | Triassic | |
| dc.subject | Permian | |
| dc.subject.age | Mesozoic::Triassic | |
| dc.subject.age | Paleozoic::Permian | |
| dc.title | THE ERDENETUIN-OBO PORPHYRY CU-MO MAGMA CHAMBER (MONGOLIA) AS A REFLECTION OF THE PERMIAN-TRIASSIC SUPERPLUME | |
| dc.type | Статья |