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• W1966697494 abstract "The University of Cambridge Atlas map-plotting computer program has been used to plot a reconstruction of the dispersal of continental blocks from eastern Gondwanaland from the Late Jurassic (160 Ma) until the Late Miocene (10 Ma). The geological basis for the reconstruction rests on the concept of South Tibet, Burma, western Thailand, Malaya and Sumatra having been part of the eastern Gondwana continent during the late Palaeozoic and early Mesozoic. The reconstruction is also based on the view that these Asian continental blocks were rifted from eastern Gondwanaland in the Late Jurassic. This rifting episode gave rise to the continental margin of central New Guinea and northern Australia. It was associated with the sea-floor spreading anomalies preserved in the floor of the northeastern Indian Ocean. The model considers the indication of crustal uplift in the Middle Jurassic followed by profound subsidence in the Cretaceous and Palaeogene, exposed in the islands of the Outer Banda Arc from Seram to Timor, and the similar Jurassic-Cretaceous facies in eastern Sulawesi implies that these areas formed part of this rifted northern margin of Australia in the Jurassic. Subsequent tectonic collision and associated major strike-slip movements have deformed and disrupted these rock sequences during the Cainozoic. The date of the rifting that removed South Tibet, Burma, western Thailand and Malaya from Gondwanaland is controversial. The indications in favour of the rifting episode having occurred in the Jurassic rather than in the Permo-Triassic are stratigraphie-structural observations on the northwestern Australian shelf, in the Banda Arc and in central New Guinea. The identification of the continental blocks removed by this rifting is based partly on stratigraphie correlation with the Banda Arc and New Guinea and partly on indications that the age of collision of Tibet, Burma, western Thailand and Malaya with Asia was a Late Cretaceous event and not Triassic-Jurassic as is generally held. There are very few reliable land-based palaeomagnetic measurements to constrain the movements of these dispersed continental fragments from Gondwanaland. The computer-generated map reconstructions put forward here fit the available Indian Ocean sea-floor spreading data although they are not unique solutions. Much of the critical ocean-floor data associated with the rifting and dispersal of these continental fragments has been destroyed in the tectonic collision processes that occurred at the Asian continental margin." @default.
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• W1966697494 date "1988-12-01" @default.
• W1966697494 modified "2023-10-18" @default.
• W1966697494 title "Mesozoic-Cenozoic rift-drift sequence of Asian fragments from Gondwanaland" @default.
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• W1966697494 doi "https://doi.org/10.1016/0040-1951(88)90272-7" @default.
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