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A orogénese timanida (em russo: Ороген Про … A orogénese timanida (em russo: Ороген Протоуралид-Тиманид) é uma orogénese pré-uraliana que se formou a nordeste dos Montes Urais durante a era do Neoproterozóico. A orogénese tem cerca de 3.000 quilómetros de comprimento. Os seus pontos extremos incluem os Urais do sul e os Urais Polares, e as penínsulas Kanin e Varanger no norte. O tergo Timan é a área tipo da orogénese. A oeste, na Península de Varange, a orogénese timanida é truncada pela mais jovem orogénese caledonídea escandinava, que tem uma disposição oblíqua. As partes nordestes da orogénese são constituídas por rochas vulcânicas e sedimentares, granitóides e poucos ofiolitos. Em contraste, a parte sudoeste da orogénese é composta principalmente de rochas sedimentares. Granitóides do tipo I e A e rochas vulcânicas são comuns na orogénese. Desde a era do Neoproterozóico Superior até ao Cambriano Médio, a orogénese timanide foi associada a uma zona de subducção que existia a nordeste dela. A maioria dos estudos interpreta a subducção como indo para dentro (placa subduzida movendo-se para sudoeste), embora um sugira o contrário (placa subduzida movendo-se para nordeste). No Cambriano, acredita-se que a orogénese timanida tenha-se desenvolvido em um contexto de colisão continental quando a Báltica e a Arctida colidiram entre 528 e 510 milhões de anos atrás. Alguns pesquisadores, entretanto, discordam dessa visão, sugerindo que nunca houve tal colisão. A erosão da orogénese timanida produziu sedimentos que agora são encontrados na Plataforma do Leste Europeu, incluindo a Formação Sablino Cambriana perto do Lago Ladoga. Estudos de sedimentos apontam que é provável que a erosão da orogénese tenha começado no Cambriano e depois se tornado mais forte no Ordoviciano. Os primeiros geólogos a estudar a orogénese foram Wilhelm Ramsay e Feodosy Tschernyschev, que publicaram trabalhos sobre o assunto em 1899 e 1901, respectivamente. Hans Reusch compilou o conhecimento existente sobre a orogénese em 1900.mento existente sobre a orogénese em 1900.
, The Timanide Orogen (Russian: Ороген Прото … The Timanide Orogen (Russian: Ороген Протоуралид-Тиманид, literally: "Protouralian–Timanide Orogen") is a pre-Uralian orogen that formed in northeastern Baltica during the Neoproterozoic in the Timanide orogeny. The orogen is about 3000 km long. Its extreme points include the southern Urals in the south and the Polar Urals, the Kanin and Varanger peninsulas in the north. The Timan Ridge is the type area of the orogen. To the west, at the Varanger Peninsula, the north-west oriented Timanide Orogen is truncated by the younger Scandinavian Caledonide Orogen that has an oblique disposition. The northeastern parts of the orogen are made up of volcanic and sedimentary rocks, granitoids and few ophiolites. In contrast the southwestern part of the orogen is made up mostly of sedimentary rocks. I and A type granitoids and volcanic rocks are common in the orogen. From the Late Neoproterozoic o the Middle Cambrian the Timanide Orogen was associated to a subduction zone that existed to the northeast of it. Most studies interpret subduction as going inward (subducted plate moving southwest) albeit one suggest the opposite (subducted plate moving to the northeast). In the Cambrian the Timanide Orogen is believed to have developed in a continental collision context as Baltica and Arctida collided between 528 and 510 million years ago. Some researchers do however dissent from this view suggesting there was never such a collision. Erosion of the Timanide Orogen have produced sediments that are now found in the East European Platform, including the Cambrian near Lake Ladoga. Studies of sediments points that it is likely that the erosion of the orogen was beginning in the Cambrian and then became stronger in Ordovician. The first geologists to study the orogen where Wilhelm Ramsay and Feodosy Tschernyschev who published works in 1899 and 1901 respectively. Hans Reusch compiled the existing knowledge on the orogen in 1900. existing knowledge on the orogen in 1900.
, L’orogenesi timanide (in lingua russa: Оро … L’orogenesi timanide (in lingua russa: Ороген Протоуралид-Тиманид, Orogen Protouralid-Timanid) è un'orogenesi pre-uraliana che si è formata nella parte nordorientale della Baltica durante il Neoproterozoico. Tra gli studiosi russi, fino agli anni 1990 la terminologia più utilizzata per riferirsi a questa orogenesi era Baikaliana, termine coniato da Nikolay Shatsky nel 1935.rmine coniato da Nikolay Shatsky nel 1935.
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The Timanide Orogen (Russian: Ороген Прото … The Timanide Orogen (Russian: Ороген Протоуралид-Тиманид, literally: "Protouralian–Timanide Orogen") is a pre-Uralian orogen that formed in northeastern Baltica during the Neoproterozoic in the Timanide orogeny. The orogen is about 3000 km long. Its extreme points include the southern Urals in the south and the Polar Urals, the Kanin and Varanger peninsulas in the north. The Timan Ridge is the type area of the orogen. To the west, at the Varanger Peninsula, the north-west oriented Timanide Orogen is truncated by the younger Scandinavian Caledonide Orogen that has an oblique disposition. The northeastern parts of the orogen are made up of volcanic and sedimentary rocks, granitoids and few ophiolites. In contrast the southwestern part of the orogen is made up mostly of sedimentary rocks. I as made up mostly of sedimentary rocks. I a
, L’orogenesi timanide (in lingua russa: Оро … L’orogenesi timanide (in lingua russa: Ороген Протоуралид-Тиманид, Orogen Protouralid-Timanid) è un'orogenesi pre-uraliana che si è formata nella parte nordorientale della Baltica durante il Neoproterozoico. Tra gli studiosi russi, fino agli anni 1990 la terminologia più utilizzata per riferirsi a questa orogenesi era Baikaliana, termine coniato da Nikolay Shatsky nel 1935.rmine coniato da Nikolay Shatsky nel 1935.
, A orogénese timanida (em russo: Ороген Про … A orogénese timanida (em russo: Ороген Протоуралид-Тиманид) é uma orogénese pré-uraliana que se formou a nordeste dos Montes Urais durante a era do Neoproterozóico. A orogénese tem cerca de 3.000 quilómetros de comprimento. Os seus pontos extremos incluem os Urais do sul e os Urais Polares, e as penínsulas Kanin e Varanger no norte. O tergo Timan é a área tipo da orogénese. A oeste, na Península de Varange, a orogénese timanida é truncada pela mais jovem orogénese caledonídea escandinava, que tem uma disposição oblíqua. As partes nordestes da orogénese são constituídas por rochas vulcânicas e sedimentares, granitóides e poucos ofiolitos. Em contraste, a parte sudoeste da orogénese é composta principalmente de rochas sedimentares. Granitóides do tipo I e A e rochas vulcânicas são comuns napo I e A e rochas vulcânicas são comuns na
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Orogénese timanida
, Timanide Orogen
, Orogenesi timanide
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