منابع مشابه
Orogeny can be very short.
In contrast to continent/continent collision, arc-continent collision generates very short-lived orogeny because the buoyancy-driven impedance of the subduction of continental lithosphere, accompanied by arc/suprasubduction-zone ophiolite obduction, is relieved by subduction polarity reversal (flip). This tectonic principle is illustrated by the early Ordovician Grampian Orogeny in the British ...
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ژورنال
عنوان ژورنال: Journal of the Geological Society
سال: 2000
ISSN: 0016-7649,2041-479X
DOI: 10.1144/jgs.157.6.1149