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TURKIC-TYPE OROGENY AND ITS ROLE IN THE MAKING OF THE CONTINENTAL CRUST

Sengör, A. M. Celâl, Natal'in, Boris A.·1996·Annual Review of Earth and Planetary Sciences

Abstract

▪ Abstract Turkic-type orogeny is a class of collisional mountain building, in which the precollision history of one, or both, of the colliding continents involves the growth of very large, subcontinent-size subduction-accretion complexes, into which magmatic arc axes commonly migrate and thus enlarge the continent to which they are attached. A review of the evolution of two Phanerozoic (Altaids, Nipponides), one Neoproterozoic (East African), and one Archean (Yilgarn) Turkic-type orogens shows that this type of orogeny may have been the principal builder of the continental crust through recorded Earth history. The total juvenile material added to Turkic-type orogens at any one time in the Phanerozoic seems close to 1 km 3/year, which about equals the amount of material annually fed into the mantle at subduction zones. As some 0.02 to 0.03% of that material is generally agreed to return to the crust by arc magmatism, these figures provide a minimum net growth rate for the continental crust during the Phanerozoic.

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Metadata

Authors
Sengör, A. M. C., & Natal'in, B. A.
Venue
Annual Review of Earth and Planetary Sciences
Published
1996-05
Volume
24
Issue
1
Pages
263-337
ISSN
  • 0084-6597 (ISSN-L)
  • 1545-4495
OpenAlex
W2119695127
Cited by
661
References
4
FWCI
1.39
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: TURKIC-TYPE OROGENY AND ITS ROLE IN THE MAKING OF THE CONTINENTAL CRUST. https://app.cochat.ai/papers/10.1146/annurev.earth.24.1.263
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Sengör, A. M. C., & Natal'in, B. A. (1996). TURKIC-TYPE OROGENY AND ITS ROLE IN THE MAKING OF THE CONTINENTAL CRUST. Annual Review of Earth and Planetary Sciences. https://doi.org/10.1146/annurev.earth.24.1.263

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