Exact(1)
Although these reversals of the tonotopic representations were present at all intensity levels, the lateral spread of activation depended on sound amplitude, with increasing recruitment of the adjacent belt areas as the intensities increased.
Similar(59)
"We are extremely disappointed by Mole Valley Council's determination to dispose of a vital community asset and to allow building on adjacent green belt fields," the spokesman said.
This arrangement is most obvious in A1 in individual animals, but the relationship generally holds for R and the adjacent lateral belt fields as well.
The expanded form of the FWHS can be adjusted by changing the inclination angles α and β. α means the inclined angle between the adjacent woven belts, and β means the inclined angle of each woven belt expanded along the folding part.
Their formation is attributed to erosion and isostatic rebound of proximal parts of the foreland basin following thrust events in the adjacent Sevier orogenic belt.
As for the Kitakawaguchi SK-1 and MITI Rumoi, a constant value of 48 mW/m20%20% higher than Urakawa) was adopted through the consideration of prolonged igneous activities within the adjacent Rebun-Kabato Belt.
The observed nested sequence architecture of the Upper Mesaverde Group is considered to be controlled by variation in subsidence rate related to the emplacement and erosion of thrust sheets in the adjacent Sevier orogenic belt.
Periods of rapid subsidence, likely associated with thrust emplacement in the adjacent fold-thrust belt, resulted in mudstone-dominated successions with isolated sandstone bodies, whereas tectonically inactive periods, associated with less subsidence, resulted in amalgamated sandstone units.
Stronger deformation along the eastern margin of the Finlayson Lake greenstone belt, adjacent to the Marmion Shear Zone, suggest reactivation during exhumation and is likely related to the 2.7 Ga amalgamation of the Superior Province.
Paleocene fluvial strata in this region contain several notable characteristics, including variable degrees of channel sandstone amalgamation, regionally-variable stratigraphic architecture, and a large fan-shaped sandstone unit that emanated from the adjacent fold-thrust belt.
The eastern Ecuadorian Andes appear as a fold-and-thrust belt adjacent to a continental foredeep represented by one of the world's largest tropical alluvial megafans, the Pastaza megafan, debouching into the Amazonian lowland.
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