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- W1985120498 abstract "The present-day continental crust has been more extensive in earlier time. A number of geological facts are assembled to demonstrate the youth of the continental outline. The young nature of this feature may be the result of the apparent disappearance and drifting apart of continental crust. The working hypothesis is advanced that the geosynclines of the past were mobile zones flanked by platform areas mostly covered by extensive epicontinental seas. The basement of the geosyncline was a mobile part of the continental crust. No direct relationship could be established between the subsiding forces creating the geosynclinal realms and the subsequent tectogenetic movements. Folding is not necessarily the outcome of a geosyncline. Mobile belts define the shape and extension of stable areas. The site of the youngest mobile zone determines the “definite” shape of the area spared by remobilisation. Continental areas, not remobilized, are gradually increasing in size during the geological evolution prior to the Recent activations of the earth's crust. The present mobile zones are not yet fixed within the geological column and therefore difficult to compare with the “frozen” mobile zones of the past." @default.
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- W1985120498 date "1968-09-01" @default.
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- W1985120498 title "Mobility of the earth's crust: A comparison between the present and the past" @default.
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- W1985120498 doi "https://doi.org/10.1016/0040-1951(68)90051-6" @default.
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