Abstract The East African Orogen, extending from southern Israel, Sinai and Jordan in the north to Mozambique and Madagascar in the south, is the world́s largest Neoproterozoic to …
Neoproterozoic granitic intrusions in South China have traditionally been interpreted as related to orogenesis, marking the cratonisation of the Yangtze Block. However, a number of …
The assembly of the eastern part of Gondwana (eastern Africa, Arabian–Nubian shield (ANS), Seychelles, India, Madagascar, Sri Lanka, East Antarctica and Australia) resulted …
The Neoproterozoic global reorganisation that saw the demise of Rodinia and the amalgamation of Gondwana took place during an incredibly dynamic period of Earth …
Age relations for assembly of Gondwana and Pangea indicate that the timing of collisional orogenesis between amalgamating continental bodies was synchronous with subduction …
The origin of the Antarctic continent can be traced to a relatively small late Archaean cratonic nucleus centred on the Terre Adélie regions of East Antarctica and the Gawler Craton region …
The East African Orogen (EAO) is one of Earth's great collision zones, where East and West Gondwana collided to form the supercontinentGreater Gondwana'orPannotia'at the end of …
Peninsular India forms a keystone in Gondwana, linking the East African and Malagasy orogens with Ediacaran–Cambrian orogenic belts in Sri Lanka and the Lützow Holm Bay …
B Bingen, O Nordgulen, G Viola - Norsk geologisk tidsskrift, 2008 - geologi.no
The Sveconorwegian orogenic belt is situated at the southwestern margin of Fennoscandia. It is one of the classical, well-exposed Grenvillian orogenic belts (Fig. 1)(Berthelsen 1980) …