THE LATE TRIASSIC KATAEV VOLCANOPLUTONIC ASSOCIATION IN WESTERN TRANSBAIKALIA, A FRAGMENT OF THE ACTIVE CONTINENTAL MARGIN OF THE MONGOL-OKHOTSK OCEAN
T.V. Donskayaa, D.P. Gladkochuba, A.M. Mazukabzova, B. De Waeleb, and S.L. Presnyakovc
aInstitute of the Earth's Crust, Siberian Branch of the Russian Academy of Sciences, ul. Lermontova 128, Irkutsk, 664033, Russia
bSPK Consulting, 10 Richardson Street, West Perth WA 6005, Australia
cA.P. Karpinsky All-Russian Research Geological Institute, Srednii pr. 74, St. Petersburg, 199106, Russia
Keywords: Volcanics, granites, U-Pb geochronology, geochemistry, active continental margin, Triassic, Mongolo-Okhotsk ocean, Transbaikalia
Pages: 22-36
Abstract
The Kataev volcanoplutonic association has been recognized in western Transbaikalia. It unites the volcanosedimentary rocks of the Kataev Formation and associated granites localized within the lower plates of the Buteel-Nuur and Zagan metamorphic-core complexes. The rocks of the Kataev association are dynamometamorphosed to different degrees, which is due to the tectonic exposure of metamorphic-core complexes in the Early Cretaceous. The U-Pb zircon dating of the Kataev Formation rhyolites yielded their age of 226 ± 3 Ma. The U-Pb zircon age of the granites intruding the Kataev Formation rocks is 223.4 ± 5.0 Ma. The volcanics of the Kataev Formation belong to the subalkalic basalt-andesite-dacite-rhyolite series. The trachybasalts and trachyandesite-basalts of the Kataev Formation have geochemical characteristics of igneous rocks formed as a result of subduction, e.g., they show distinct negative Nb and Ti and positive Ba and Sr anomalies on multielemental patterns. The specific composition of mafic volcanics points to their formation through the melting of a mantle source resulted from the mixing of depleted mantle and subduction components. Trachyandesites have higher Th and U contents than basaltoids. They can result from the contamination of a mantle source, similar in composition to the Kataev Formation basaltoids, with crustal material. The felsic volcanics of the Kataev Formation and granites inbruding them show nearly identical geochemical characteristics corresponding to both A - and I -type granites. These rocks might have formed through the melting of a moderately water-saturated magmatic source of diorite-tonalite composition at 742-833?C.
We have established that the rocks of the Kataev volcanoplutonic association in western Transbaikalia and northern Mongolia formed in the Late Triassic synchronously with the calc-alkalic granitoids of the Henteyn-Daurian batholith and the alkali granites and bimodal volcanic associations of the Kharitonovo and Tsagaan-Hurtey volcanoplutonic associations. The synchronous formation of volcanoplutonic associations of normal and high alkalinity agrees with the geodynamic setting of the Andean-type active continental margin existing in the area of present-day western Transbaikalia and northern Mongolia in the Early Mesozoic. This setting was the result of the subduction of the Mongolo-Okhotsk oceanic plate beneath the Siberian continent.
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