Sr-nd-isotopic systematics of alkaline rocks and carbonatites of edelweiss complex (the north-chuisky ridge, gorny altai)
| Parent link: | Doklady Akademii Nauk.— , 2004 Vol. 397, N 6.— 2004.— P. 802-806 |
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| Other Authors: | , , , , , |
| Summary: | 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 |
| Published: |
2004
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| Subjects: | |
| Format: | Book Chapter |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=599642 |