Zobrazeno 1 - 10
of 11
pro vyhledávání: '"Yu. I. Konovalov"'
Publikováno v:
Lithology and Mineral Resources. 58:42-59
Publikováno v:
Oceanology. 62:685-694
Autor:
V. B. Kurnosov, Yu. I. Konovalov
Publikováno v:
Russian Journal of Pacific Geology. 16:243-256
Publikováno v:
Geochemistry International. 58:922-932
This paper addresses the vertical distribution of total mercury and its thermoforms in the Holocene–Upper Pleistocene sedimentary rocks from the Dead Dog active hydrothermal field in the Middle Valley, Juan de Fuca Ridge, Pacific Ocean. Sediment sa
Publikováno v:
Lithology and Mineral Resources. 55:152-163
Clay minerals in basalt sills from the northern East Pacific Rise, covered by Upper Pleistocene clayey–sandy–silty sediments (turbidites, hemipelagites, and diatom oozes) sampled from DSDP Holes 477, 478, and 481A, were studied by X-ray methods b
Autor:
Konstantin Galin, E. O. Goncharov, V. B. Kurnosov, Yu. I. Konovalov, A. R. Geptner, N. N. Ignatyev
Publikováno v:
Oceanology. 60:98-107
—Chemical composition of the Upper Pleistocene sediments (turbidites interbedded with hemipelagic sediments) from contact zones with basalt sills in the Guaymas Basin, Gulf of the California (DSDP Hole 481A), was studied by the methods of XRF and I
Publikováno v:
Russian Journal of Pacific Geology. 13:479-491
The clay minerals in the Upper Pleistocene sediments from DSDP Hole 478 (a drilled depth of 464 m) located in the central area of the Guaymas Basin, Gulf of California, are studied. The composition of the clay minerals and their quantitative proporti
Publikováno v:
Литология и полезные ископаемые. :234-247
Clay minerals (fraction
Publikováno v:
Lithology and Mineral Resources. 53:361-379
The content and distribution of mercury in Holocene–Upper Pleistocene turbidites, hemipelagic sediments intercalating therein, as well as basement basalts are studied. Samples of sediments were taken from the core of Holes 858A, 858B, 858C, 858D, a
Publikováno v:
Doklady Earth Sciences. 480:575-579
The results of studying Hg in an underwater hydrothermal system in the ocean using the Middle Valley of the Juan de Fuca ridge as an example are presented. A significant part of Hg is accumulated in the basalt fundament (Holes 858F, G), forming anoma