Sr-nd-isotopic systematics of alkaline rocks and carbonatites of edelweiss complex (the north-chuisky ridge, gorny altai)

Sr-nd-isotopic systematics of alkaline rocks and carbonatites of edelweiss complex (the north-chuisky ridge, gorny altai)

מידע ביבליוגרפי
Parent link:Doklady Akademii Nauk.— , 2004
Vol. 397, N 6.— 2004.— P. 802-806
מחברים אחרים: Vrublevskij V. V., Zhuravlev D. Z., Gertner I. F., Krupchatnikov V. I., Vladimirov A. G., Rikhvanov L. P. Leonid Petrovich
סיכום: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
יצא לאור: 2004
נושאים:
труды учёных ТПУ
פורמט: Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=599642

פריטים דומים

פריטים דומים