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Meso to Neoproterozoic store and clear belts on the timberland ofr of the SFC show umbrella low to general grade metasediments and orthogneisses. That feature is in agreement with the subhorizontal driving you. Bacia do Sao Francisco: Their lithotectonic domains are offered in Fig. O Supergrupo Espinhaco em Minas Gerais:.
They are represented by deep-level plumbing systems consisting of giant dyke buanhaes, sill provinces and layered intrusions. Based on geological and geochronological data, the 1. The first one occurred at 1. Both are summarized in Table 1 and can be considered as LIP events.
Table 1 Summary of the 1. Sedimentation of the southern Espinhaco Supergroup basal sequence accompanied by the formation guanhhaes maar craters containing diamond-bearing vent breccias and deposition of the Arai Group within the Pirapora Graben. Pirapora magnetic anomaly 1. Iin normal faulting with NW-SE strike. The link between mantle plume activity forr LIPs has been widely recognized. Condie, ; Ernst and Buchan, During the plume-related initial rift phase, sites for the deposition of the Guanhars and Espinhaco sedimentary basal sequence Lookjng developed skngle the NW-SE Guanhwes Graben.
Many examples worldwide show a very Quick hook up app relationship of carbonatitic and kimberlitic rocks to mantle plume magmatism Bell, Lookiny Heaman and Kjarsgaard, ; Haggerty, This basal pile also hosts Loooking craters containing diamond-bearing vent breccias hit generally by phreatomagmatic activity, which increased Looking for hot single in guanhaes explosive action Nixon, Thus, although Paleoproterozoic guanheas diamondiferous rocks in southern Espinhaco have not been located precisely, it is probable that diamonds were brought to the sedimentary basin surface by eingle or lamproitic magmatism related to the 1.
Although there is no slngle from drill core, the enigmatic large Pirapora magnetic anomaly clearly ib inside the Pirapora Gravimetric Low Fig. The aforementioned features point to 1. This fact would mean the difference between our two-plume model and the single-plume model proposed by Suita and Chemale When a mantle plume reaches the base of the lithosphere with its head and conduit tail structure e. Far away from the plume center, the mafic magma spreads laterally in the lithosphere as dykes e. Singl can be explained by Lookng activity of a 1.
Ernst and Buchan proposed that mafic—ultramafic complexes can be fed from the system of a plume-related giant radiating dyke swarm and Lopking they guanahes be located either near or far from the plume center. Rubin refers to close relationship between graben subsidence and dyke-induced faulting in Hawaiian volcanic rift zones. The prominent normal fault shown in Fig. The real density of the Para de Minas dykes is not shown in Fig. On average, they are 5 km apart from each other in southern SFC and keep the same pattern under the cratonic cover in the Pirapora Graben Chaves, The Pirapora Graben subsidence certainly was accompanied by an increasing sedimentation rate both in Arai and southern Espinhaco.
In the deep crustal sections of this Graben the heat transfer from the plume-related rising mafic magmas and probably the regional decompression deflation under the Graben yielded extensive crustal melting and generated the acid anorogenic volcanism and plutonism around 1. The possibility of the occurrence of Late Paleoproterozoic continental flood basalts in the studied area can be presumed taking into account the large magnetic anomaly inside the coeval Pirapora Graben. Therefore, the widespread magmatism, rifting and sedimentation yielded by these two endogenic events insert them among the most prominent geodynamic processes of the Brazilian Precambrian Geology.
A bacia intracratonica do Sao Francisco: A origem dos diamantes da Serra do Espinhaco Meridional: Geociencias 31 4— O Pre-Cambriano do Brasil. Sao Paulo, Brasil, p. Proceedings of the 31st Int. Bacia Sao Francisco—Geologia e Rec. A evolucao geocronologica da Cordilheira do Espinhaco: Revista Brasileira Geociencias 9 171— ATafrogenese Estateriana nos blocos paleoproterozoicos da America do Sul e processos subsequentes. Geonomos 3 21— Radiometric ages, aeromagnetic expression and general geology of mafic dykes from Southeastern Brazil and implications for Africa—South American correlations. Mantle Plumes and their Record in Earth History. Proceedings of the 32nd International Geological Congress, Italy abstracts.
Earth, Venus and Mars. Maximum size and distribution in time and space of mantle plumes: Recognizing mantle plumes in the geological record. Timing of eastern North American kimberlite magmatism: Analise faciologica e estratigrafica do Paleo-Mesoproterozoico: O Supergrupo Espinhaco em Minas Gerais: Geociencias 28 2— Collapse features and narrow grabens on Mars and Venus: The morphology and nature of primary diamondiferous occurrences. U-Pb zircon geochronology of Precambrian tin-bearing continental-type acid magmatism in Central Brazil. Sr and Nd isotopic characteristics of 1. Ciencias 73 2— Flood basalts and hot-spot tracks: Dike-induced faulting and graben subsidence in volcanic rift zones.
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