- decollement fold
- складчатость срыва
Англо-русский словарь нефтегазовой промышленности. 2011.
decollement fold
Смотреть что такое "decollement fold" в других словарях:
Décollement — Fig. 1 Imbricate fan in a thrust system with a basal décollement[1][2] Décollement (dé collé ment) is a gliding plane between two rock masses. In French, décoller means to detach from or to rip of … Wikipedia
Fold mountain — Fold mountains are mountains formed due mainly to the effects of folding on layers within the upper part of the Earth s crust. In the time before either Plate tectonic theory developed, or the internal architecture of thrust belts became well… … Wikipedia
Fold (geology) — For other uses, see Fold (disambiguation). Very tight folds. Formation near Moruya, New South Wales, Australia … Wikipedia
fold-thrust hills — A landscape along an orogenic belt margin underlain dominantly by sedimentary rocks that have undergone intensive structural deformation via a series of sub parallel thrust faults and associated folds. The thrust faults typically merge along a … Glossary of landform and geologic terms
Thrust fault — in the Qilian Shan, China. The older (left, blue and red) thrust over the younger (right, brown). A thrust fault is a type of fault, or break in the Earth s crust across which there has been relative movement, in which rocks of lower… … Wikipedia
mountain — mountainless, adj. /mown tn/, n. 1. a natural elevation of the earth s surface rising more or less abruptly to a summit, and attaining an altitude greater than that of a hill, usually greater than 2000 ft. (610 m). 2. a large mass of something… … Universalium
Nappe — For other uses, see Nappe (disambiguation). Schematic overview of an eroded thrust system. The shaded material is the nappe. The erosional hole is called a window or fenster. The klippe is the isolated block of the nappe overlying autochthonous… … Wikipedia
Critical taper — In mechanics and geodynamics, a critical taper is the equilibrium angle made by the far end of a wedge shaped agglomeration of material that is being pushed by the near end. The angle of the critical taper is a function of the material properties … Wikipedia
Geology of the Alps — The Alps form a part of a Tertiary orogenic belt of mountain chains, called the Alpide belt, that stretches through southern Europe and Asia from the Atlantic all the way to the Himalayas. This belt of mountain chains was formed during the Alpine … Wikipedia
Olympic-Wallowa Lineament — Location of the Olympic Wallowa Lineament. Is the OWL an optical illusion? The Olympic Wallowa lineament (OWL) – first reported by cartographer Erwin Raisz in 1945 [1] on a relief map of the continental United States – is a physiographic feature… … Wikipedia
Zagros Mountains — Topographic map of Iran with the Zagros Mountains The Zagros Mountains from space, September 1992 … Wikipedia
