2011
DOI: 10.1134/s1028334x11080137
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Autonomous anorthosites of the Aldan Shield and associated rocks: Age, geochemistry, and formation mechanism (example of the Kalar Massif)

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Cited by 3 publications
(3 citation statements)
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“…This process having a relatively long crustal prehistory (T Nd (DM) = 3825-3479 Ma) was developed along the wide and long ancient tectonic zone. It is overlain by platform deposits in the north; in the south it controls the location of Neoarchean granosyenite of the Dzhyal tuktinskii massif and subalkaline charnockite and enderbite of the Altual' Dzheluiskii massif, which is broken by Paleoproterozoic anorthosite of the Kalar skii massif containing captured xenogenic zircon grains with an age of 2670 and 2620 Ma [6] (Fig. 1).…”
mentioning
confidence: 98%
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“…This process having a relatively long crustal prehistory (T Nd (DM) = 3825-3479 Ma) was developed along the wide and long ancient tectonic zone. It is overlain by platform deposits in the north; in the south it controls the location of Neoarchean granosyenite of the Dzhyal tuktinskii massif and subalkaline charnockite and enderbite of the Altual' Dzheluiskii massif, which is broken by Paleoproterozoic anorthosite of the Kalar skii massif containing captured xenogenic zircon grains with an age of 2670 and 2620 Ma [6] (Fig. 1).…”
mentioning
confidence: 98%
“…This is in harmony with ideas on the leading role of the long living (Archean-Proterozoic) mantle megaplume in the tectonic evolution of the Aldan Shield. This plume is structurally expressed in the Aldano-Stanovoe sialic core (nuclear) and its satellite (Charskii gneiss oval) [1,6] (Fig. 1).…”
mentioning
confidence: 99%
“…1. Scheme of the tectonic zoning (Aldan shield) with the elements of kinematics of the lower-middle crust tectonic flows [Glukhovskii et al, 2011].…”
Section: гранатовые гранулиты алданского щита как следы постгадейскойmentioning
confidence: 99%