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Allochthon

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allochthon [ə′läk·thən]
(geology)
A rock that was transported a great distance from its original deposition by some tectonic process, generally related to overthrusting, recumbent folding, or gravity sliding.

Allochthon 

an organism inhabiting some locality which, unlike an autochthon, arose in the course of evolution in some other place. It reached the regions inhabited at the present time by migrating from its own original center of distribution. For example, the opossum and several hummingbird species are allochthons of North America, which they entered from South America.



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000 allochthon Turks in the year 2007 (of about 3,2 million allochthons on a total population of 16,3 million).
Specific topics include Silurian-bearing terranes of Alaska, the significance of detrital zircons in Upper Devonian ocean-basin strata of the Sonora allochthon and Lower Permian synorogenic strata of Mina Mexico foredeep in central Sonora, and Late Triassic mixed carbonate-volcaniclastic facies of the Olds Ferry terrane in eastern Oregon and western Idaho.
This little peak is located near the eastern edge of the Cordilleran allochthons in central Yukon, separated from strata of the North American shelf and slope by two major faults, the Tummel and the Tintina.
 
 
 
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