Search results. 8 results for Books: “Kenitiro Suguio” Dicionário de Geologia Sedimentar e Áreas Afins (Em Portuguese do Brasil). by Kenitiro Suguio. 8 set. Books by Kenitiro Suguio, Rochas sedimentares, Depósitos geologia marinha, Dicionário de geologia sedimentar e áreas afins, Geologia do. Rochas Sedimentares – Kenitiro Suguio. Uploaded by Guilherme Madrid Pereira . Uploaded by. Guilherme Madrid Pereira · Cunha.
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Suguio, Kenitiro 1937-
The deposits are found mainly in the proximal kenitrio medial areas of the fans. This document is only for private use for research and teaching activities.
The rock formations appear in the form of scarps and residual elevations and underlie the Cenozoic sediments that cover the greater part of the area under investigation.
Geologia Sedimentar | Kenitiro Suguio | download
These sediments consist of various deposits that originated under different conditions and environments and are distributed from the foot of the scarp of the “Serra Geral” General Range to the Atlantic Ocean.
They are bound on the east by another Pleistocene set of beach ridges and dunes Barrier lllcorresponding to a higher sea level ofyears ago and followed by a third formation Barrier lV with an aeolic covering and containing active dunes from the Holocene. They have a lobe morphology with a convex top, separated by low flat areas. One part of this deposit began as a barrier island during a period of marine transgression. Learn what derived works are clicking here. There seem to have been two major periods of aeolic activity: Rudaceous deposits are also found on the subsurface, covered over with coastal marine deposits, corresponding to the higher sea level of overyears ago.
Depósitos cenozoicos costeiros e a morfologia do extremo sul de Santa Catarina
These deposits have a flat top and are slightly inclined to the east. Paleolagoonar and estuary deposits in certain stretches and situations are covered by lacustrine deposits, running parallel or perpendicular to beach ridges sandy bodies from various ages. Some deposits, with samples of trunks, shells and peat, mainly lagoonar, estuary and lacustrine deposits, could be dated by ‘C POT.
It is situated in the northeast of the area under investigation. Sandy beach deposits are from varying ages of the Pleistocene and Holocene and cover areas of two river basins.
To the east of this assemblage, lakes can be found, partially filled with peat. The deposits and processes generated in the alluvial fans began earlier than this older coastal deposits and therefore the subsurface rudaceous deposits show lower sea level than the present one.
Belonging to the Pleistocene is a large formation of aeolic origin that reaches an altitude of m and is supported by rocks of the Palermo Formation. This rights cover the whole data about this seddimentar as well as its contents.
Lacustrine deposits frequently appear as surface sediments, consisting of peat, ranging in thickness from 1 to 4. They consist of rudaceous deposits, interspersed in some areas, and nearly always covered with finer-grained material.
The sedkmentar of deposits makes it possible to define the recurrence of both the marine and continental processes. The remainder was added in the regressive period that followed, giving rise to beach ridges varying in height from 14 to 16m.