Standard

Morphology of the Nyurba kimberlite pipe and its relationship with the dolerite dike. / Tomshin, M. D.; Pokhilenko, N. P.; Tarskikh, E. V.

In: Doklady Earth Sciences, Vol. 477, No. 2, 01.12.2017, p. 1458-1460.

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

Harvard

Tomshin, MD, Pokhilenko, NP & Tarskikh, EV 2017, 'Morphology of the Nyurba kimberlite pipe and its relationship with the dolerite dike', Doklady Earth Sciences, vol. 477, no. 2, pp. 1458-1460. https://doi.org/10.1134/S1028334X17120200

APA

Tomshin, M. D., Pokhilenko, N. P., & Tarskikh, E. V. (2017). Morphology of the Nyurba kimberlite pipe and its relationship with the dolerite dike. Doklady Earth Sciences, 477(2), 1458-1460. https://doi.org/10.1134/S1028334X17120200

Vancouver

Tomshin MD, Pokhilenko NP, Tarskikh EV. Morphology of the Nyurba kimberlite pipe and its relationship with the dolerite dike. Doklady Earth Sciences. 2017 Dec 1;477(2):1458-1460. doi: 10.1134/S1028334X17120200

Author

Tomshin, M. D. ; Pokhilenko, N. P. ; Tarskikh, E. V. / Morphology of the Nyurba kimberlite pipe and its relationship with the dolerite dike. In: Doklady Earth Sciences. 2017 ; Vol. 477, No. 2. pp. 1458-1460.

BibTeX

@article{b7efb62857174d60bd6db2ca5f36cc7e,
title = "Morphology of the Nyurba kimberlite pipe and its relationship with the dolerite dike",
abstract = "Study of the magmatics in the Nakyn kimberlite field, with consideration of the isotope dating results, allowed us to establish a sequence of their formation. First, 368.5–374.4 Ma ago intrusions of the Vilyui–Markha dike belt formed. Then (363–364 Ma) intrusion of kimberlites took place. In the Early Carboniferous (338.2–345.6 Ma), alkaline basaltic magma intruded through faults controlling the kimberlites. The magmatic activity finished 331–324.9 Ma ago with the formation of explosive breccias. It has been found that the Nyurba kimberlite pipe consists of two bodies: their kimberlite melts have successively intruded through independent channels.",
author = "Tomshin, {M. D.} and Pokhilenko, {N. P.} and Tarskikh, {E. V.}",
year = "2017",
month = dec,
day = "1",
doi = "10.1134/S1028334X17120200",
language = "English",
volume = "477",
pages = "1458--1460",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Morphology of the Nyurba kimberlite pipe and its relationship with the dolerite dike

AU - Tomshin, M. D.

AU - Pokhilenko, N. P.

AU - Tarskikh, E. V.

PY - 2017/12/1

Y1 - 2017/12/1

N2 - Study of the magmatics in the Nakyn kimberlite field, with consideration of the isotope dating results, allowed us to establish a sequence of their formation. First, 368.5–374.4 Ma ago intrusions of the Vilyui–Markha dike belt formed. Then (363–364 Ma) intrusion of kimberlites took place. In the Early Carboniferous (338.2–345.6 Ma), alkaline basaltic magma intruded through faults controlling the kimberlites. The magmatic activity finished 331–324.9 Ma ago with the formation of explosive breccias. It has been found that the Nyurba kimberlite pipe consists of two bodies: their kimberlite melts have successively intruded through independent channels.

AB - Study of the magmatics in the Nakyn kimberlite field, with consideration of the isotope dating results, allowed us to establish a sequence of their formation. First, 368.5–374.4 Ma ago intrusions of the Vilyui–Markha dike belt formed. Then (363–364 Ma) intrusion of kimberlites took place. In the Early Carboniferous (338.2–345.6 Ma), alkaline basaltic magma intruded through faults controlling the kimberlites. The magmatic activity finished 331–324.9 Ma ago with the formation of explosive breccias. It has been found that the Nyurba kimberlite pipe consists of two bodies: their kimberlite melts have successively intruded through independent channels.

UR - http://www.scopus.com/inward/record.url?scp=85040013351&partnerID=8YFLogxK

U2 - 10.1134/S1028334X17120200

DO - 10.1134/S1028334X17120200

M3 - Article

AN - SCOPUS:85040013351

VL - 477

SP - 1458

EP - 1460

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 25755068