Results 301 to 310 of about 305,558 (359)
Assessing glacier changes and hydrological impacts in the upper Indus Basin under CMIP6 climate scenarios. [PDF]
Abdullah T, Bashir J, Romshoo SA.
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Reconstruction of Provenance and Paleo-Sedimentary Environment of the Saihan Formation in the Manglai Uranium Deposit, Central-Eastern Erlian Basin, China. [PDF]
Zheng Y+10 more
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Protracted circum-continent subduction: A mechanism for craton destruction and a rationale for craton longevity. [PDF]
Xu X+12 more
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Multifractal structure of a riddled basin
Chaos: An Interdisciplinary Journal of Nonlinear Science, 2001For a two-dimensional piecewise linear map with a riddled basin, a multifractal spectrum f(γ), which characterizes the “skeletons” of the riddled basin, is introduced. With f(γ), the uncertainty exponent is obtained by a variational principle, which enables us to introduce a concept of a “boundary” for the riddled basin.
Hiromichi Suetani, Takehiko Horita
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The structure of basins of attraction and their trapping regions
Ergodic Theory and Dynamical Systems, 1997In dynamical systems examples are common in which two or more attractors coexist, and in such cases, the basin boundary is nonempty. When there are three basins of attraction, is it possible that every boundary point of one basin is on the boundary of the two remaining basins? Is it possible that all three boundaries of these basins coincide? When this
Helena E. Nusse, James A. Yorke
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Deep structure of the Mediterranean Basin
Journal of Geophysical Research, 1970From an analysis of the seismicity of the Mediterranean basin we obtain a model of the deep structure of this region that is a further improvement to the plate tectonic theory. Taking into account the data of seismology, the gravity anomalies, volcanism and the few available data on the heat flow in this region, we conclude that the African plate is ...
D. Postpischl+2 more
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The Structure of the Pacific Basin
Geological Magazine, 1934Since the return of the St. George Expedition from the Pacific in 1925, a series of nine papers (2–8, 26, 27), describing the geology of most of the volcanic islands visited, has been published, and it is now possible to co-ordinate the results already arrived at, and to use them in an attempt to throw light on the structure of the Pacific basin.
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