- Vening-Meinesz hypothesis
-
гипотеза изостазии Венинг-Мейнеца
English-Russian dictionary of geology. 2011.
Vening-Meinesz hypothesis
Смотреть что такое "Vening-Meinesz hypothesis" в других словарях:
Plate tectonics — The tectonic plates of the world were mapped in the second half of the 20th century … Wikipedia
Motonori Matuyama — (松山 基範, Matsuyama Motonori?, October 25, 1884 – January 27, 1958) was a Japanese geophysicist who was the first to surmise that the Earth s magnetic field had undergone reversals in the past. The era of reversed polarity preceding the current… … Wikipedia
Oceanic trench — Oceanic crust is formed at an oceanic ridge, while the lithosphere is subducted back into the asthenosphere at trenches. The oceanic trenches are hemispheric scale long but narrow topographic depressions of the sea floor. They are also the… … Wikipedia
1963 en science — Années : 1960 1961 1962 1963 1964 1965 1966 Décennies : 1930 1940 1950 1960 1970 1980 1990 Siècles : XIXe siècle XXe siècl … Wikipédia en Français
Isostasy — (Greek isos = equal , stásis = standstill ) is a term used in Geology to refer to the state of gravitational equilibrium between the earth s lithosphere and asthenosphere such that the tectonic plates float at an elevation which depends on their… … Wikipedia
Indian Ocean — an ocean S of Asia, E of Africa, and W of Australia. 28,357,000 sq. mi. (73,444,630 sq. km). * * * Indian Ocean Introduction Indian Ocean Background: The Indian Ocean is the third largest of the world s five oceans (after the Pacific Ocean and… … Universalium
Matuyama , Motonori — (1884–1958) Japanese geologist Matuyama, who was born at Uyeda (now Usa) in Japan, was the son of a Zen abbot. He was educated at the University of Hiroshima and the Imperial University in Kyoto, where he was appointed to a lectureship in 1913.… … Scientists
