Parent Rock
Mostrando 1-8 de 8 artigos, teses e dissertações.
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1. Micromorphology and Genesis of Soils from Topolitosequences in the Brazilian Central Plateau
ABSTRACT The micromorphology of deeply weathered soils (Ferralsols/ Latossolos ) from the Central Plateau of Brazil remains little studied, and its affiliation to different parent materials, poorly known. To clarify the processes of soil formation of these acric, gibbsitic, Fe-oxide rich Ferralsols, three lithotoposequences on local ultrabasic to basic intru
Rev. Bras. Ciênc. Solo. Publicado em: 09/09/2019
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2. Genesis of Soils Formed from Mafic Igneous Rock in the Atlantic Forest Environment
ABSTRACT Different parent materials participate in the formation of soils in the hilly landscape of “Mar de Morros” in the Atlantic Forest environment. Those derived from mafic igneous rock (gabbro) frequently show erosion problems because of land use, which is aggravated by the mountainous relief and soil attributes. This study evaluated the main pedoge
Rev. Bras. Ciênc. Solo. Publicado em: 23/06/2016
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3. Metais pesados como indicadores de materiais de origem em uma topolitosequencia do triangulo mineiro, Estado de Minas Gerais.
Objetivou-se neste trabalho determinar os teores de metais pesados em amostras de solos de um topolitosequencia coletada no Triangulo Mineiro, Estado de Minas Gerais, para testar a hipotese de que tais elementos podem ser utilizados na identificacao e separacao da influencia do material de origem. Os teores de Cd, Cr, Cu, Fe, Mn, Ni, Pb, e Zn foramm determin
Pesquisa Agropecuaria Brasileira. Publicado em: 2011
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4. Relações solo-vegetação no Parque Nacional da Serra do Cipó, Espinhaço Meridional, Minas Gerais / Soil vegetation relationships in the National Park Serra do Cipó, in Espinhaço Meridional, Minas Gerais
The region of Serra do Rio Cipó, in the southern part of the Serra do Espinhaço, comprises large areas of Cerrado, Atlantic forest, forest islands and one of the richest high-altitude rocky vegetation in Brazil. The ecotonal character between the Cerrado and Atlantic Forest biomes, described in many studies of regional flora and fauna, is one of the factor
Publicado em: 2009
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5. Geologia, geometalurgia, controles e gênese dos depósitos de fósforo, terras raras e titânio do complexo carbonatítico Catalão i , GO
This work describes the geological and geometallurgical characteristics of the phosphate, titanium, niobium and rare-earth elements deposits in the northeast part of the Catalão I carbonatite complex, Central Brazil. The mineralization controls were determined for magmatic, metasomatic and weathering processes. The ore types were defined on the basis of geo
Publicado em: 2008
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6. Metodologia de datação em carbonatos pela série de desequilíbrio do urânio por espectrometria de massa
There are many dating methods largely used according to the kind of material to be dated. Methods that rely on the time-dependency of geochemical disequilibrium 238 235 232 U, U and Th natural decay system, between daughter and parent isotope, from the whose final members are stable Pb isotopes, are the most useful in a broader variety of geological, hydrolo
Publicado em: 2006
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7. Caracterização e classificação de solos da Ilha de Fernando de Noronha (PE)
In the main island of Fernando de Noronha Archipelago, the dry tropical climate with oceanic influence and the recent parent material of volcanic origin, are responsible for the small weathering of soils with high scientific importance for the development of the Brazilian System of Soil Classification (SiBCS). Seven representative soil profiles, involving tw
Publicado em: 2004
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8. STRESS - STRAIN BEHAVIOR OF A GNEISS RESIDUAL SOIL USING THE CUBIC TRIAXIAL CELL / COMPORTAMIENTO TENSIÓN X DEFORMACIÓN EN SUELOS RESIDUALES / COMPORTAMENTO TENSÃO X DEFORMAÇÃO DE SOLOS RESIDUAIS NO EQUIPAMENTO TRIAXIAL
The knowledge of the mechanical behaviour of residual soils is of great importance in geotechnical projects, because of its abundance in tropical regions, such as Brazil and particularly in the area of Rio de Janeiro. The present work presents a study on the fundamental stress-strain behaviour of a residual soil resulting from a profile of a gneiss rock in R
Publicado em: 1998