MANTLE-DRIVEN DEFORMATION OF OROGENIC ZONES AND CLUTCH TECTONICS

dc.contributor.author	Tikoff B.
dc.contributor.author	Russo R.
dc.contributor.author	Teyssier C.
dc.contributor.author	Tommasi A.
dc.date.accessioned	2022-10-03T05:50:59Z
dc.date.available	2022-10-03T05:50:59Z
dc.date.issued	2004
dc.identifier	https://elibrary.ru/item.asp?id=13812306
dc.identifier.citation	Geological Society Special Publication, 2004, 227, С., 41-64
dc.identifier.issn	0305-8719
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38885
dc.description.abstract	Compatible deformation between the upper crust and upper mantle is documented for a variety of ancient and neotectonic settings, suggesting that these lithospheric layers are coupled. Areas of neotectonic deformation are also characterized by high seismic attenuation. indicating that the uppermost mantle is theologically weak and flowing in these regions. The flow of the mantle, both lithospheric and asthenospheric, potentially drives deformation in continental orogenic zones. Three-dimensional models, controlled by bottom-driven mantle flow, are proposed for obliquely convergent, transcurrent and obliquely divergent plate margins. Our analysis indicates that the absolute, and not Just relative, plate motions play a critical role in the orogenic cycle.
dc.title	MANTLE-DRIVEN DEFORMATION OF OROGENIC ZONES AND CLUTCH TECTONICS
dc.type	Статья

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