Age of Alkaline Ultramafic Explosion Pipes of the Chapinsky Complex (Yenisei Ridge)

Мұқаба

Дәйексөз келтіру

Толық мәтін

Ашық рұқсат Ашық рұқсат
Рұқсат жабық Рұқсат берілді
Рұқсат жабық Тек жазылушылар үшін

Аннотация

The age of formation of explosion pipes of the Chapinsky complex in the Chingasan magmatic belt in the north of the Yenisei Ridge was determined. U-Pb dating of zircon megacrysts from alkaline-ultramafic rocks established values of 657.7 ± 13.4 and 647.6 ± 9.7 Ma for the Natalyinskaya and № 3 pipes, respectively. The intrusion of alkaline-ultramafic explosion pipes of the Chapinsky complex corresponds to the time of manifestation of ultramafic alkaline magmatism along the southern and southwestern margin of the Siberian craton.

Толық мәтін

Рұқсат жабық

Авторлар туралы

Yu. Danilova

Institute of the Earth’s Crust of the Siberian Branch of the Russian Academy of Sciences

Хат алмасуға жауапты Автор.
Email: jdan@crust.irk.ru
Ресей, Irkutsk

I. Sharygin

Institute of the Earth’s Crust of the Siberian Branch of the Russian Academy of Sciences

Email: jdan@crust.irk.ru
Ресей, Irkutsk

E. Gladkochub

Institute of the Earth’s Crust of the Siberian Branch of the Russian Academy of Sciences

Email: jdan@crust.irk.ru
Ресей, Irkutsk

E. Nikolenko

ALROSA (ZIMBABWE)(PRIVATE) LIMITED

Email: jdan@crust.irk.ru
Зимбабве, Harare

N. Bryansky

Institute of the Earth’s Crust of the Siberian Branch of the Russian Academy of Sciences; Irkutsk State University

Email: jdan@crust.irk.ru
Ресей, Irkutsk; Irkutsk

S. Skuzovatov

Vinogradov Institute of Geochemistry Siberian Branch of the Russian Academy of Sciences

Email: jdan@crust.irk.ru
Ресей, Irkutsk

A. Gladkov

Institute of the Earth’s Crust of the Siberian Branch of the Russian Academy of Sciences

Email: jdan@crust.irk.ru
Ресей, Irkutsk

A. Ivanov

Institute of the Earth’s Crust of the Siberian Branch of the Russian Academy of Sciences

Email: jdan@crust.irk.ru
Ресей, Irkutsk

D. Koshkarev

ALROSA

Email: jdan@crust.irk.ru
Ресей, Mirny

F. Letnikov

Institute of the Earth’s Crust of the Siberian Branch of the Russian Academy of Sciences

Email: jdan@crust.irk.ru

Academician of the RAS

Ресей, Irkutsk

Әдебиет тізімі

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Әрекет
1. JATS XML
Жүктеу
2. Fig. 1. Scheme of the geological structure of the Chapinsky ultrabasic alkaline complex in the structure of the Yenisei Ridge (a): 1 - alluvial deposits; 2 - Early Paleozoic sedimentary deposits; 3 - volcanogenic-sedimentary deposits of the Chapa series; 4 - Neoproterozoic terrigenous and volcanogenic-terrigenous complexes; 5 - Early Proterozoic metamorphosed carbonate-terrigenous deposits; 6 - Archean undissected metamorphic complexes. 7-10 magmatic formations: 7 - Chapinsky CSM: explosion pipes (a), stokes (b), sills (c), dikes (d) (out of scale); 8 - Orlovsky subvolcanic complex of basalt-andesite-rhyolite composition; 9 - Garevsky ultrametamorphic complex of granite-granite-gneisses; 10 - Shumikhinsky metapicritic-basalt subvolcanic complex. 11 - faults: Ishimbinsky deep fault (a), minor faults (b), tectonic disturbances (c). The inset (b) shows the marginal structures of the southern and southwestern margins of the Siberian Craton: I - Prisayan basement ledge; II - Uriksko-Iisky graben, including the Ziminsky SCR (H); III - Yenisei ridge, including the Chapin SCR (C)

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3. Fig. 2. Mineral relationships in the rocks of the Nataliinskaya, No. 3, and Glubokaya pipes. Photographs of slits (a-d), images in backscattered electrons (e-h). Mineral symbols: Ap - apatite, Bdy - baddeleyite, Cal - calcite, Chl - chlorite, Dol - dolomite, Mag - magnetite, Ol - olivine, Phl - phlogopite, Py - pyrite, Qz - quartz, Spl - spinel, Srp - serpentine, Zrn - zircon

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4. Fig. 3. U-Pb-age of zircon megacrysts from explosion tubes of the Chapinsky CSF field. Cathodoluminescence images: a - Natalinskaya pipe; b - pipe No. 3; c - kimberlite [13], d and e - concordia diagrams for zircon megacrysts

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5. Supplementary
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