Results 111 to 120 of about 461,360 (322)
Hydrogeology of the Dakota Sandstone in the San Juan structural basin, New Mexico, Colorado, Arizona, and Utah [PDF]
, 1989 Steven D. Craigg +3 more
openalex +1 more source
The Depositional Record, EarlyView.A classical peripheral foreland basin is bounded longitudinally by a pair of marginal ocean basins (DeCelles & Giles, 1996). The WTFB sediments transfer to adjacent marginal ocean basins. The western Taiwan foreland basin (WTFB) is regarded as a classical peripheral foreland basin, longitudinally bounded by the southern Okinawa Trough (SOT) to the ...
Cheng‐Shing Chiang +2 more
wiley +1 more source
Journal of Morphology, Volume 284, Issue 1, January 2023., 2023 The perpendicular insertion of Sharpey's fibers in the external cortex suggests the presence of a thick leathery skin layer overlying notosuchian osteoderms. Although intramembranous ossification is the main process involved in the development of crocodyliform osteoderms, we reported a case of metaplastic development.
Mariana Valéria de Araújo Sena +12 more
wiley +1 more source
The steepest watershed: from graphs to images [PDF]
arXiv, 2012 The watershed is a powerful tool for segmenting objects whose contours appear as crest lines on a gradient image. The watershed transform associates to a topographic surface a partition into catchment basins, defined as attraction zones of a drop of water falling on the relief and following a line of steepest descent.
arxiv
Hydrogeology of the Ojo Alamo Sandstone in the San Juan structural basin, New Mexico, Colorado, Arizona and Utah [PDF]
, 1990 C.R. Thorn +4 more
openalex +1 more source
Lacustrine and fan‐delta sediments in syn‐rift lake basins
The Depositional Record, EarlyView.A consistent model for the sequence framework and depositional pattern of asymmetric half‐grabens in syn‐rift lake basins bounded by active faults has been established, complementing existing models for marine rift successions. Syn‐rift lake basins are characterised by relatively small dimensions, steep slopes, poorly developed shoreline strata ...
Qianyou Wang +6 more
wiley +1 more source
The coexistence and evolution of attractors in the web map with weak dissipation [PDF]
arXiv, 2013 The dynamics of the web map with weak linear dissipation is studied. The evolution of the coexisting attractors and the structure of their basins while changing the dissipation and nonlinearity are revealed. It is shown that the structure of the basins remains the same when the dissipation and nonlinearity changes simultaneously.
arxiv
Hydrogeology of the Menefee Formation in the San Juan structural basin, New Mexico, Colorado, Arizona, and Utah [PDF]
, 1990 Gary W. Levings +4 more
openalex +1 more source
Journal of Quaternary Science, Volume 38, Issue 1, Page 107-122, January 2023., 2023 Abstract Small mountain lakes are natural archives for understanding long‐term natural and anthropogenic impact on the environment. This study focused on long‐term (last ca. 13 000 years) vegetation changes and sedimentary processes in the catchment area of Lake Planina pri jezeru (1430 m a.s.l.) by using mineralogical, geochemical and palynological ...
Nina Caf +8 more
wiley +1 more source
Registro da deformação pós-paleozóica na Bacia do Amazonas, região de Itaituba (PA)
Brazilian Journal of GeologyResumo: A Bacia do Amazonas compreende uma área de aproximadamente 500.000 km2 abrangendo parte dos estados do Pará e Amazonas. A região estudada localiza-se na porção sudoeste da bacia, próximo à cidade de Itaituba (PA), e contém rochas da cobertura ...
Thais Borba Santos +4 more
doaj +1 more source