Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Morphology of the Nyurba kimberlite pipe and its relationship with the dolerite dike. / Tomshin, M. D.; Pokhilenko, N. P.; Tarskikh, E. V.
в: Doklady Earth Sciences, Том 477, № 2, 01.12.2017, стр. 1458-1460.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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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