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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Some deposits, with kentiiro of trunks, shells and peat, mainly lagoonar, estuary and lacustrine deposits, could be dated by ‘C POT. They have a lobe morphology with a convex top, separated by low flat areas.
To the east of this zedimentar, lakes can be found, partially filled with peat. They are bound on the east by another Pleistocene set of beach ridges and dunes Barrier lllcorresponding to a higher sea level ofyears ago sedimeentar followed by a third formation Barrier lV with an aeolic covering and containing active dunes from the Holocene. 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.
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. Learn what derived works are clicking here. Any uses or copies of this document in whole or in part must include the author’s name.
The deposits are found mainly in the proximal and medial areas of the fans. This rights cover the whole data about this document as well as its contents. Lacustrine deposits frequently appear as surface sediments, consisting of peat, ranging in thickness from 1 to 4.
It is situated in the northeast of the area under investigation.
Kenitiro Suguio (Author of Geologia Sedimentar)
The sequence of deposits makes it possible to define the recurrence of both the marine and sedimentr processes. Rudaceous deposits are also found on the subsurface, covered over with coastal marine deposits, corresponding to the higher sea level of overyears ago. 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.
They consist of rudaceous deposits, interspersed in some areas, and nearly always covered with finer-grained material.
This document is only for private use for research and teaching activities. Reproduction for commercial use is forbidden. 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.
The distal deposits of the fans have a very slight representation. 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. This morphology is due to deposit and ggeologia processes characteristic of alluvial fans.
There seem to have been sedimmentar major periods of aeolic activity: The remainder was added in the regressive period that followed, giving rise to beach ridges varying in height from 14 to 16m. These deposits have a flat top and are slightly inclined to the east. One part of this deposit began as a barrier island during a period of marine transgression.