Sr-nd-isotopic systematics of alkaline rocks and carbonatites of edelweiss complex (the north-chuisky ridge, gorny altai); Doklady Akademii Nauk; Vol. 397, N 6

Sr-nd-isotopic systematics of alkaline rocks and carbonatites of edelweiss complex (the north-chuisky ridge, gorny altai); Doklady Akademii Nauk; Vol. 397, N 6

Sonraí bibleagrafaíochta
Parent link:	Doklady Akademii Nauk.— , 2004 Vol. 397, N 6.— 2004.— P. 802-806
Rannpháirtithe:	Vrublevskij V. V., Zhuravlev D. Z., Gertner I. F., Krupchatnikov V. I., Vladimirov A. G., Rikhvanov L. P. Leonid Petrovich
Achoimre:	The obtained isotopic data allow the following conclusions. 1) The alkaline rocks and carbonatites of Edelweiss complex were formed at late-collisional stage of Middle Ordovician period. 2) The moderately depleted PREMA-type mantle served as a substance source for the formed comagmatic association. 3) Evolution of derivative melts was complicated by crust contamination, which effects were manifested as enhanced isotope ratios of Sr, O and C in rocks and minerals В фонде НТБ ТПУ отсутствует
Teanga:	Béarla
Foilsithe / Cruthaithe:	2004
Ábhair:	труды учёных ТПУ
Formáid:	Caibidil leabhair
KOHA link:	https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=599642

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