Emelyanova, T A; Kostitsyn, Yu A; Lelikov, Evgeny P (2012): Volcanic rocks from the submarine Vityaz Ridge: their age, chemical and isotopic compositions. PANGAEA, https://doi.org/10.1594/PANGAEA.788609, Supplement to: Emelyanova, TA et al. (2012): Geochemistry of the submarine Vityaz Ridge at the Pacific slope of the Kurile Island arc. Translated from Geokhimiya, 2012, 50(3), 316-332, Geochemistry International, 50(3), 289-303, https://doi.org/10.1134/S0016702912030056
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Results of geological studies at the submarine Vityaz Ridge carried out during cruises 37 and 41 of R/V Akademik Lavrent'ev in 2005 and 2006 are reported. The studied area is located at an near-island trench of the slope in the central part of the Kuril Island arc. Morphologically it consists of two parts: an inner volcanic arc represented by the Great Kuril Range and an outer arc corresponding to the submarine Vityaz Ridge. Diverse rocks composing the basement and the sedimentary cover of the ridge were recovered by dredging. Based on K-Ar dating and geochemistry, volcanics were divided into Paleocene, Eocene, late Oligocene, and Pliocene-Pleistocene complexes. Each of the complexes reflects a tectonomagmatic stage in the ridge evolution. Geochemical and isotope data on the volcanics indicate contribution of ancient crustal material in the magma source and, correspondingly, formation of this structure on the continental basement. Two-stage model ages (TDM2) vary in a wide range from zero values in mafic rocks to 0.77 Ga in felsic varieties, pointing to presence of Precambrian protolith in the source of the felsic rocks of the Vityaz Ridge. The Pliocene-Pleistocene volcanics are classed with tholeiitic, calc-alkaline, and subalkaline series, which differ in alkali contents and REE fractionation. Values of (La/Sm)_n and (La/Yb)_n ratios vary from 0.74 and 0.84 in the tholeiitic varieties to 1.19 and 1.44 in the calc-alkaline and 2.32 and 3.73 in the subalkaline rocks. All three varieties occur within the same volcanic edifices and formed during differentiation of magmatic melts that were channeled along fault zones from the mantle source slightly enriched in crustal component.
Median Latitude: 47.131782 * Median Longitude: 153.194851 * South-bound Latitude: 45.563067 * West-bound Longitude: 151.050000 * North-bound Latitude: 48.331000 * East-bound Longitude: 154.521000