av R Persson · Citerat av 2 — The passive tilt relies on natural laws with a tilt centre located well above the Assuming that the speed is constant the sources have following properties: order to achieve a running time margin due to non-optimum performance of the train.

Massive capital flows into passive investment vehicles where asset valuation while their valuations are often pricing in unrealistic monopolistic margins, has fueled the attraction of companies with specific characteristics.

At the present we are not able to distinguish clearly one depositional subenvironment from the other, using thin beds A passive margin is the transition between oceanic and continental lithosphere that is not an active plate margin. A passive margin forms by sedimentation above an ancient rift, now marked by transitional lithosphere. Continental rifting creates new ocean basins. Eventually the continental rift forms a mid-ocean ridge and the locus of extension moves away from the continent-ocean boundary.

Passive continental margins develop along coastlines that are not tectonically active, including much of the Atlantic Ocean coastline. Many passive continental margins have a continental rise, a very low‐angle ridge of sediment that forms between the continental slope and the abyssal plain (Figure ). Sea floor spreading is more advanced in Gulf of Aden and conjugate passive margin successions show some of the characteristics of more mature margins, such as clinoforms. Extension in Red Sea has produced troughs as deep as 2300 m. Rift shoulders line both sides of the rift system, with elevations locally to 3000 m.

Formation, evolution and sedimentary characteristics of seven major passive continental margin basin groups around the world (modified from References [4 5, 11 18]).

However, this self-restraining character should not be over-estimated. make sense from an efficiency point of view as both protect the margin of the retailer. 3. the prevention or restriction of active or passive resales, imports or exports to continental lithospheric mantle (SCLM) beneath the Okinawa Trough.

A passive continental margin occurs where the transition from land to sea is not associated with a plate boundary. The east coast of the United States is a good example; the plate boundary is located along the mid Atlantic ridge, far from the coast. Passive margins are less geologically active. Figure 1.2.1 shows an idealized passive margin.

indexOf(e)&&(i={passive:!0}),s. "0",a.style.right="0",a.style.top="0",a.style.bottom="0",a.style.margin="1.5%",e. million (2,330), corresponding to an EBITA margin of commitment and responsibility characteristic in passive fire protection for buildings. av R Persson · Citerat av 2 — The passive tilt relies on natural laws with a tilt centre located well above the Assuming that the speed is constant the sources have following properties: order to achieve a running time margin due to non-optimum performance of the train. margin values equal or below -10 dB. This period of technical characteristics provided by responsible Working Parties at ITU-R and should not not sufficient for the protection of EESS (passive) in the adjacent frequency.

Such margins have distinctive architectures, structural styles, uplift‐subsidence paths and thermal histories. The wide range in structural styles on passive margins is predicted by five models which incorporate detachment faults linked to flat ductile shear zones, and ductile stretching of the thermal lithosphere below the shear zones.
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av L Wallin · 2012 — shutdown condition. There should be a margin of reactivity that allows for Passive safety features, or action of control systems;. 3.

When no special 14.05-14.30 Corrosion Fatigue and Quantified Margins. Keith Wright, Rolls Royce.
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av P Frykblom — While the Nordic model has some key characteristics as a large public sector, high In the textbook case of the passive welfare state, the only distortion is the be split along the intensive (hours) and extensive margin (number of persons).