Perfil antioxidante e bioatividade de três espécies de macroalgas da Praia do Morro de Pernambuco no litoral Sul da Bahia, Brasil

Santos, Janaina Pires

doi:10.11606/t.41.2017.tde-03012017-142742

Cited by 1 publication

(2 citation statements)

References 130 publications

(145 reference statements)

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“…Some exposures show a rhythmic structure with centimetric sandstone beds alternating with decimetric metapelite beds. The composition and geochemical data support a deep-sea turbiditic, syn-orogenic sedimentation record for the Mandacaru Formation [116]. Furthermore, the Mandacaru Formation shows distinctive provenance patterns, with TDM model ages averaging 1.6-1.4 Ga [92,101,109,117].…”

Section: The Riacho Do Pontal Orogensupporting

confidence: 55%

“…The outer zone includes the Casa Nova Group, which is divided into two units: the Barra Bonita Formation and the Mandacaru Formation. The Barra Bonita Formation consists of metapelitic rocks and muscovite quartzite with marble lenses and is interpreted to have been deposited in a shallow marine platform environment [92,101,116]. The marble lenses can reach thicknesses of up to 200 m and locally preserve original sedimentary structures.…”

Section: The Riacho Do Pontal Orogenmentioning

confidence: 99%

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Wrapping a Craton: A Review of Neoproterozoic Fold Belts Surrounding the São Francisco Craton, Eastern Brazil

Uhlein,

Caxito

et al. 2023

Minerals

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A synthesis of the evolution of the Neoproterozoic belts or orogens surrounding the São Francisco craton (SFC) in northeastern and southeastern Brazil is presented. Emphasis is placed on recognizing the superposition of sedimentary basins, from rift to passive margin to retroarc and foreland, as well as identifying three diachronic continental collisions in the formation of the SFC. The Tonian passive margin occurs in the southern Brasília Belt with the Vazante, Canastra, and Araxá Groups. During the Tonian, island magmatic arcs and basins developed in front and behind these arcs (fore- and back-arcs). Subsequently, in the Cryogenian–Ediacaran, a retroarc foreland basin developed with part of the Araxá Group and the Ibiá Group, and finally, a foreland basin developed, which was filled by the Bambuí Group. A tectonic structure of superimposed nappes, with subhorizontal S1–2 foliation, formed between 650 and 610 Ma, is striking. In the northern Brasília Belt, there is the Stenian passive margin of the Paranoá Group, the Tonian intrusion of the Mafic–Ultramafic Complexes, and the Mara Rosa Island magmatic arc, active since the Tonian, with limited volcanic–sedimentary basins associated with the arc. A thrust–fold belt structure is prominent, with S1 foliation and late transcurrent, transpressive tectonics characterized by the Transbrasiliano (TB) lineament. The Cryogenian–Ediacaran collision between the Paranapanema and São Francisco cratons is the first collisional orogenic event to the west. In the Rio Preto belt, on the northwestern margin of the São Francisco craton, the Cryogenian–Ediacaran Canabravinha rift basin is prominent, with gravitational sediments that represent the intracontinental termination of the passive margin that occurs further northeast. The rift basin was intensely deformed at the Ediacaran–Cambrian boundary, as was the Bambuí Group. On the northern and northeastern margins of the São Francisco craton, the Riacho do Pontal and Sergipano orogens stand out, showing a comparable evolution with Tonian and Cryogenian rifts (Brejo Seco, Miaba, and Canindé); Cryogenian–Ediacaran passive margin, where the Monte Orebe ophiolite is located; and Cordilleran magmatic arcs, which developed between 620 and 610 Ma. In the Sergipano fold belt, with a better-preserved outer domain, gravitational sedimentation occurs with glacial influence. A continental collision between the SFC and the PEAL (Pernambuco-Alagoas Massif) occurred between 610 and 540 Ma, with intense deformation of nappes and thrusts, with vergence to the south and accommodation by dextral transcurrent shear zones, such as the Pernambuco Lineament (PE). The Araçuaí belt or orogen was formed at the southeastern limit of the SFC by a Tonian intracontinental rift, later superimposed by a Cryogenian–Ediacaran rift–passive margin of the Macaúbas Group, with gravitational sedimentation and glacial influence, and distally by oceanic crust. It is overlain by a retroarc basin with syn-orogenic sedimentation of the Salinas Formation, partly derived from the Rio Doce cordilleran magmatic arc and associated basins, such as the Rio Doce and Nova Venécia Groups. A third continental collision event (SF and Congo cratons), at the end of the Ediacaran (580–530 Ma), developed a thrust–fold belt that deforms the sediments of the Araçuaí Belt and penetrates the Paramirim Corridor, transitioning to the south to a dextral strike-slip shear zone that characterizes the Ribeira Belt.

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Section: The Riacho Do Pontal Orogensupporting

confidence: 55%

Section: The Riacho Do Pontal Orogenmentioning

confidence: 99%

Wrapping a Craton: A Review of Neoproterozoic Fold Belts Surrounding the São Francisco Craton, Eastern Brazil

Uhlein,

Caxito

et al. 2023

Minerals

View full text Add to dashboard Cite

show abstract

Perfil antioxidante e bioatividade de três espécies de macroalgas da Praia do Morro de Pernambuco no litoral Sul da Bahia, Brasil

Abstract: Tão difícil quanto escrever a tese, é tentar expor em poucas páginas o quanto sou imensamente grata a cada pessoa que fez parte da minha trajetória, nesses quatro anos

Cited by 1 publication

References 130 publications

Wrapping a Craton: A Review of Neoproterozoic Fold Belts Surrounding the São Francisco Craton, Eastern Brazil

Wrapping a Craton: A Review of Neoproterozoic Fold Belts Surrounding the São Francisco Craton, Eastern Brazil

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