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• W2005203378 abstract "Such paradoxes as synchronous compression and tension in extensional sedimentary basins, and synchronous deformation of intractonic basins and eustatic sea-level falls, can each be related to pulsed changes in curvature of the Earth's surface. Australia is everywhere in a state of significant, relatively uniform, upper crustal horizontal compression, approximately perpendicular to the continental margins and generally directed towards its centre. The compression commenced in the Pliocene but was absent in the Late Miocene. During the evolution of the Gippsland and Bass basins under extensional stress from the Late Jurassic to Recent, seven pulses of similarly directed compression have been identified from the Campanian to Recent. Time equivalent compressional pulses can also be demonstrated in such widely separated areas as Northwest and Northeast Australia, Northwest Europe and Central America. Nine earlier pulses of Early Triassic to Albian age are similarly synchronous global events and another twenty-three pulses inferred since the Neoproterozoic (800 Ma) are probably similarly globally synchronous. Earth expansion (with subduction) can explain these observations since it causes the surface curvature to decrease resulting in ‘flattening’ of the semi-rigid crust. Flattening results in lower crustal extension which generates sedimentary basins while contemporaneous upper crustal compression inverts and folds the sediments. Since globally synchronous compressional pulses may reflect expansion in the ocean basins there is a correlation of such pulses with major eustatic sea-level lowstands. Any site of expansion within the earth is transmitted to the semi-rigid crust as a volume increase by the whole gravitating-fluid, oblate spheroid. This results in ubiquitous synchronous compressional pulses in the upper crust detectable on seismic reflection data not only at basin scale, but also in individual petroleum-producing structures." @default.
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• W2005203378 date "1997-08-01" @default.
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• W2005203378 title "Synchronous compressional pulses in extensional basins" @default.
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• W2005203378 doi "https://doi.org/10.1016/s0264-8172(97)00014-7" @default.
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