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Middle Paleozoic kimberlite magmatism in the northeastern Siberian craton. / Egorova, E. O.; Afanas’ev, V. P.; Pokhilenko, N. P.

In: Doklady Earth Sciences, Vol. 470, No. 2, 01.10.2016, p. 1023-1026.

Research output: Contribution to journal › Article › peer-review

Harvard

Egorova, EO, Afanas’ev, VP & Pokhilenko, NP 2016, 'Middle Paleozoic kimberlite magmatism in the northeastern Siberian craton', Doklady Earth Sciences, vol. 470, no. 2, pp. 1023-1026. https://doi.org/10.1134/S1028334X16100214

APA

Egorova, E. O., Afanas’ev, V. P., & Pokhilenko, N. P. (2016). Middle Paleozoic kimberlite magmatism in the northeastern Siberian craton. Doklady Earth Sciences, 470(2), 1023-1026. https://doi.org/10.1134/S1028334X16100214

Vancouver

Egorova EO, Afanas’ev VP, Pokhilenko NP. Middle Paleozoic kimberlite magmatism in the northeastern Siberian craton. Doklady Earth Sciences. 2016 Oct 1;470(2):1023-1026. doi: 10.1134/S1028334X16100214

Author

Egorova, E. O. ; Afanas’ev, V. P. ; Pokhilenko, N. P. / Middle Paleozoic kimberlite magmatism in the northeastern Siberian craton. In: Doklady Earth Sciences. 2016 ; Vol. 470, No. 2. pp. 1023-1026.

BibTeX

@article{d708379a9cab4feeb6be2bea466aa569,
title = "Middle Paleozoic kimberlite magmatism in the northeastern Siberian craton",
abstract = "The mineral chemistry and crystal morphology of kimberlite pyropes from the Billyakh River placer in the northeastern Siberian craton are characterised in terms of the placer history. The pyropes bear signatures of chemical weathering (dissolution), presumably in a Middle Paleozoic laterite profile, and therefore were originally hosted by Middle Paleozoic kimberlites. The broad occurrence of placer pyropes with lateritic dissolution signatures points to the presence of Middle Paleozoic diamond-bearing kimberlites in the study area.",
author = "Egorova, {E. O.} and Afanas{\textquoteright}ev, {V. P.} and Pokhilenko, {N. P.}",
year = "2016",
month = oct,
day = "1",
doi = "10.1134/S1028334X16100214",
language = "English",
volume = "470",
pages = "1023--1026",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Middle Paleozoic kimberlite magmatism in the northeastern Siberian craton

AU - Egorova, E. O.

AU - Afanas’ev, V. P.

AU - Pokhilenko, N. P.

PY - 2016/10/1

Y1 - 2016/10/1

N2 - The mineral chemistry and crystal morphology of kimberlite pyropes from the Billyakh River placer in the northeastern Siberian craton are characterised in terms of the placer history. The pyropes bear signatures of chemical weathering (dissolution), presumably in a Middle Paleozoic laterite profile, and therefore were originally hosted by Middle Paleozoic kimberlites. The broad occurrence of placer pyropes with lateritic dissolution signatures points to the presence of Middle Paleozoic diamond-bearing kimberlites in the study area.

AB - The mineral chemistry and crystal morphology of kimberlite pyropes from the Billyakh River placer in the northeastern Siberian craton are characterised in terms of the placer history. The pyropes bear signatures of chemical weathering (dissolution), presumably in a Middle Paleozoic laterite profile, and therefore were originally hosted by Middle Paleozoic kimberlites. The broad occurrence of placer pyropes with lateritic dissolution signatures points to the presence of Middle Paleozoic diamond-bearing kimberlites in the study area.

UR - http://www.scopus.com/inward/record.url?scp=84994311337&partnerID=8YFLogxK

U2 - 10.1134/S1028334X16100214

DO - 10.1134/S1028334X16100214

M3 - Article

AN - SCOPUS:84994311337

VL - 470

SP - 1023

EP - 1026

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 25755694