Titlebook: Marine Geology and Oceanography of the Arctic Seas; Yvonne Herman Conference proceedings 1974 Springer-Verlag New York Inc. 1974 Arctic.Ar

會犯錯誤

Hubert Horace Lamb combination of milestone articles, new empirical research, enriching theoretical work and interviews with leading researchers to bridge sociology, media studies, and science and technology studies in one of the first book-length publications on the emerging field of media and time..978-3-030-24952-6978-3-030-24950-2

HERE

Edward Peter Jacobus van den Heuvel,Peter Buurman combination of milestone articles, new empirical research, enriching theoretical work and interviews with leading researchers to bridge sociology, media studies, and science and technology studies in one of the first book-length publications on the emerging field of media and time..978-3-030-24952-6978-3-030-24950-2

種類

combination of milestone articles, new empirical research, enriching theoretical work and interviews with leading researchers to bridge sociology, media studies, and science and technology studies in one of the first book-length publications on the emerging field of media and time..978-3-030-24952-6978-3-030-24950-2

擴(kuò)音器

tenosynovitis

Tectonic Setting and Cenozoic Sedimentary History of the Bering Sea,ly Tertiary and by marine deposition in the later Tertiary. River diversions caused by Miocene uplift of the Alaskan Range appear to have more than doubled the drainage area of the Yukon River. This change established the Yukon as the dominant source of river sediments (~90%) reaching the Bering Sea

rheumatism

Geological Oceanography of the Bering Shelf,over the shelf..Sedimentation on the Bering shelf can be divided into five distinct depositional regimes: southeastern, central, northeastern, northwestern and outer shelves. The nature of sediments deposited in each regime is related to the provenance and the water dynamics in the area. In the nort

合唱隊(duì)

Holocene Sedimentary Framework, East-Central Bering Sea Continental Shelf,hern sector; little modern sediment was deposited subsequently. In contrast, clayey silt has accumulated at an average rate of 60 mg cm?.yr?. (70 cm 10.yr?.) since 10,000 to 11,000 years B.P. at one location in the south. A scheme for paleo-environmental interpretation based on foraminiferal fossils

圍巾

GOAD

Recent Sediments of the East Siberian Sea, and eastern portions of the East Siberian Sea. Sediment derived from the New Siberian Islands dominates the shallow (10 to 15 m) western region. Currents here are stronger than average and silt is the dominant sediment type. The central plateau is dominated by material introduced by the Indigirka R

Engaged