Zobrazeno 1 - 10
of 18
pro vyhledávání: '"Tamara Bayanova"'
Autor:
Namık Aysal, Marcel Guillong, Tamara Bayanova, Mayuko Fukuyama, Nicole Leonard, İsak Yılmaz, Elif Varol, Fatma Şişman Tükel, Yusuf Kaan Kadıoğlu, Nurullah Hanilçi, Fulya Uzun, Ersin Kaygısız
Publikováno v:
Geostandards and Geoanalytical Research. 47:297-310
Publikováno v:
Geological Journal. 58:563-582
Publikováno v:
Записки Горного института. 255:405-418
A comprehensive study of a 340 m thick lenticular-sheet body of ultramafic composition penetrated by structural well M-1 at a depth of about 2.2 km was accomplished. Its main volume is composed of plagioharzburgite; fine-grained rocks of norite and o
Autor:
Tamara Bayanova
Publikováno v:
Труды Ферсмановской научной сессии ГИ КНЦ РАН. 18:321-325
Autor:
Tamara Bayanova
Publikováno v:
Труды Ферсмановской научной сессии ГИ КНЦ РАН. 18:352-358
Autor:
Tamara Bayanova, Victor Chashchin
Publikováno v:
Труды Ферсмановской научной сессии ГИ КНЦ РАН. 18:403-408
Autor:
Anatoliy Nikolaev, Tamara Bayanova, Viktor Subbotin, Ekaterina Steshenko, Svetlana Drogobuzhskaya
Publikováno v:
Open Journal of Geology. :474-496
Baddeleyite is an important mineral geochronometer. It is valued in the U-Pb (ID-TIMS) geochronology more than zircon because of its magmatic origin, while zircon can be metamorphic, hydrothermal or occur as xenocrysts. Detailed mineralogical (BSE, K
Autor:
Pavel Serov, Tamara Bayanova
The Sm-Nd systematics is one of the most demanded isotope-geochronological tools to study ancient geological complexes. With the accumulation of knowledge about the REE in various geological processes, the question arises of extending the capabilitie
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::87d4ed7bab72dccc7c3b80b223c07a75
https://doi.org/10.5194/egusphere-egu21-5518
https://doi.org/10.5194/egusphere-egu21-5518
The isotope U-Pb system on zircon and baddeleyite reflects the precise age of the origin (2.5, 2.45 and 2.4 Ga) and duration (more than 100 Ma) for Cu-Ni and PGE complex deposits widespread in the N-E part of the Fennoscandian Shield. The Monchegorsk
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::83c0bca56da2cb40a14740fe286fe1c5
https://doi.org/10.5194/egusphere-egu21-9233
https://doi.org/10.5194/egusphere-egu21-9233
Publikováno v:
Goldschmidt2021 abstracts.