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Alice Springs Orogeny : ウィキペディア英語版 | Alice Springs Orogeny The Alice Springs Orogeny was a major intraplate tectonic (mountain building) episode in central Australia responsible for the formation of a series of large mountain ranges.〔 Wells AT, Forman DJ, Ranford LC, Cook PJ (1970). "Geology of the Amadeus Basin, Central Australia". Bureau of Mineral Resources, Australia, Bulletin 100. 〕 == Duration == The Alice Springs Orogeny was a long lived event, beginning approximately 450 million years ago and concluding about 300 million years ago,〔Bradshaw JD, Evans PR (1988). "Palaeozoic tectonics, Amadeus Basin, central Australia". The APEA Journal 28: 267–282〕〔 Haines PW, Hand M, Sandiford M (2001). "Palaeozoic synorogenic sedimentation in central and northern Australia: a review of distribution and timing with implications for the evolution of intracontinental orogens". Australian Journal of Earth Sciences 48 (6): 911–928 〕 and it involved less than 100 km of distributed shortening.〔
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