Age of Palaeozoic granites and metamorphism in the Tuvino-Mongolian Massif of the Central Asian Mobile Belt: Loss of a Precambrian microcontinent

Precambrian Research

Volumn 110, Issue 1-4, 2001, Pages 143-164

  Salnikova, E B ^a   Kozakov, I K ^a   Kotov, A B ^a   Kroner A ^b   Todt, W ^c   Bibikova, E V ^d   Nutman, A ^e,f   Yakovleva, S Z ^a   Kovach, V P ^a  

^a INSTITUTE OF PRECAMBRIAN GEOLOGY AND GEOCHRONOLOGY   (Russian Federation)

^b JOHANNES GUTENBERG UNIVERSITY   (Germany)

^c MAX PLANCK INSTITUTE FOR CHEMISTRY   (Germany)

^d VERNADSKY INSTITUTE OF GEOCHEMISTRY AND ANALYTICAL CHEMISTRY   (Russian Federation)

^e HIROSHIMA UNIVERSITY   (Japan)

^f AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

Author keywords

Central Asian Mobile Belt; Granitoids; High grade metamorphism; Siberia; Tuvino Mongolian Massif; U Pb zircon geochronology

Indexed keywords

LEAD; URANIUM; ZIRCONIUM;

AMPHIBOLITE FACIES; COLLISION; GRANITE; METAMORPHISM; PALEOZOIC; TECTONIC EVOLUTION;

ANALYTIC METHOD; ASIA; CHRONOLOGY; GEOLOGY; MONGOLIA; REVIEW; ROCK; SAMPLING; SCANNING ELECTRON MICROSCOPY;

ASIA;

EID: 0035420820     PISSN: 03019268     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0301-9268(01)00185-1     Document Type: Article

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