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The presence of E W, NE SW, and NW SE stream trends in all illustrations recommends that the equivalent tectonic trends have been the main considerable tectonic events in the morphological advancement and hydrographic development of the basin.
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Only three major nuclei underwent Paleozoic tectonic events not obviously related to their flanking orogenic belts.
The physical geography of the Devonian can be reconstructed using evidence from paleomagnetism, paleoclimate, paleobiogeography, and tectonic events.
Those formed by tectonic events, such as folding or faulting of rock units, are called structural traps.
The Carboniferous Period (about 359 to 299 million years ago) was marked by the onset of several major tectonic events.
The tectonic events in Asia of the Paleozoic Era (about 541 to 252 million years ago) may be summarized under three categories: events in the Altaids, events in the Tethysides, and events in the continental nuclei.
Thus, it is often possible to reconstruct tectonic events of the past on the basis of metamorphic rock associations currently exposed at Earth's surface.
The interiors of the ancient cratons were not affected by the above tectonic events, and intracratonic sedimentary and volcanic sequences accumulated in large basins.
The 900-square-mile plateau is studded with ethereal karst formations, evidence of tectonic events that started molding the area over 400 million years ago.
In these rocks, dating reveals ages of 1 billion to 3.5 billion years, and they have been little affected by tectonic events postdating the Cambrian.
The tectonic events involved in the breakup of Rodinia also modified the ocean basins, forcing their expansion and flooding portions of many continents.
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