Zobrazeno 1 - 10
of 40
pro vyhledávání: '"V.O. Gimon"'
Publikováno v:
Russian Geology and Geophysics. 62:445-459
––Two stages are recognized in the evolution of the Aksug ore-magmatic system (OMS): (1) formation of the Aksug granitoid pluton and (2) emplacement of small ore-bearing intrusions. Intrusive bodies of the two stages are composed of rocks of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9e19f14b3020c2081445cf47ba600df3
https://doi.org/10.2113/rgg20194115
https://doi.org/10.2113/rgg20194115
Publikováno v:
Russian Geology and Geophysics. 60:1060-1075
—The Aksug porphyry Cu–Mo deposit is located in a region of long-lasting magmatic activity. Gabbroids of the Khoito-Oka complex are the earliest intrusive rocks, in which the Aksug granitoid pluton hosting ore-bearing small porphyry intrusions is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2dc5bba7c5283f38087b788677136e94
https://doi.org/10.15372/rgg2019070
https://doi.org/10.15372/rgg2019070
Publikováno v:
Russian Geology and Geophysics. 60:583-601
—The Kultuminskoe deposit is located within the Gazimur metallogenic zone in eastern Transbaikalia. Mineralization is associated with the Middle–Upper Jurassic Kultuma pluton composed of subalkaline rock series ranging from quartz monzonites and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4b64160802d6c3e61926170f97083925
https://doi.org/10.15372/rgg2019078
https://doi.org/10.15372/rgg2019078
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Autor:
E. N. Lepekhina, V.Yu. Kiseleva, A. N. Berzina, A. P. Berzina, Tamara B. Bayanova, S. V. Palesskii, V.O. Gimon, R.Sh. Krymskii
Publikováno v:
Russian Geology and Geophysics. 56:446-465
Two intrusive complexes are recognized in the Zhireken deposit: Amanan and ore-bearing porphyry. According to the ages obtained by U–Pb zircon dating (Amanan complex—162.6 ± 1.4 Ma, granites and monzonite-porphyry of the ore-bearing complex—15
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1ed537776ffefbe55d894902c426792d
https://doi.org/10.1016/j.rgg.2015.02.006
https://doi.org/10.1016/j.rgg.2015.02.006
Publikováno v:
Journal of Asian Earth Sciences. 79:655-665
The Shakhtama Mo–Cu porphyry deposit is located within the eastern segment of the Central Asian Orogenic Belt, bordering the southern margin of the Mongol–Okhotsk suture zone. The deposit includes rocks of two magmatic complexes: the precursor pl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::95adae730b764462a3503375940fffd8
https://doi.org/10.1016/j.jseaes.2013.07.028
https://doi.org/10.1016/j.jseaes.2013.07.028
Publikováno v:
Acta Geologica Sinica - English Edition. 88:494-496
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::55dfbf5f0ec42d3b8c17dfab9c143ef2
https://doi.org/10.1111/1755-6724.12374_1
https://doi.org/10.1111/1755-6724.12374_1
Autor:
A. P. Berzina, V.O. Gimon, R.Sh. Krymskii, Pavel Serov, A.N. Larionov, A. N. Berzina, I.V. Nikolaeva
Publikováno v:
Russian Geology and Geophysics. 54:587-605
Two intrusive complexes are recognized at the Shakhtama deposit: Shakhtama and ore-bearing porphyry. The U–Pb zircon dates (SHRIMP II) are 161.7 ± 1.4 and 161.0 ± 1.7 Ma for the monzonites and granites of the Shakhtama complex and 159.3 ± 0.9 an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d07cb17b5f0db18bf0b85ab261c0aad7
https://doi.org/10.1016/j.rgg.2013.04.009
https://doi.org/10.1016/j.rgg.2013.04.009
Publikováno v:
Doklady Earth Sciences. 442:249-255
The Erdenetuin-Obo porphyry Cu-Mo deposit was formed at the final stage of development of magmatic activity occasionally manifested in the Late Permian-Early Triassic in the period of at least 40 Ma. Early plutonic (host) and late ore-bearing porphyr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a2c400c7fea37af299c7febe45698d81
https://doi.org/10.1134/s1028334x12010059
https://doi.org/10.1134/s1028334x12010059
Publikováno v:
Russian Geology and Geophysics. 52:1553-1562
Several complexes are recognized within the Sora porphyry Cu-Mo deposit: plutonogenic, porphyry (ore-bearing), and dike. They formed since Ordovician till Devonian at the collision, postcollisional, and rift stages of the regional evolution, respecti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a8d89ce58149b71be97133efb7f39c05
https://doi.org/10.1016/j.rgg.2011.11.004
https://doi.org/10.1016/j.rgg.2011.11.004