(Q97485590)

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Extension of continental lithosphere: A model for two scales of basin and range deformation

scientific article published in 1986

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Extension of continental lithosphere: A model for two scales of basin and range deformation (English)

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M. T. Zuber

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E. M. Parmentier

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2

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R. C. Fletcher

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publication date

1986

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published in

Journal of Geophysical Research

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volume

91

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issue

B5

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page(s)

4826

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cites work

Cenozoic and Mesozoic structure of the eastern Basin and Range province, Utah, from COCORP seismic-reflection data

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Implications of selected subsurface data on the structural form and evolution of some basins in the northern Basin and Range province, Nevada and Utah

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Limits on lithospheric stress imposed by laboratory experiments

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https://api.crossref.org/works/10.1029%2FJB091IB05P04826

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7 January 2021

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The Basin and Range Province: Origin and Tectonic Significance

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Regional gravity and tectonic patterns: Their relation to late Cenozoic epeirogeny and lateral spreading in the western Cordillera

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Unstable extension of the lithosphere: A mechanical model for basin-and-range structure

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Evolution of lithospheric strength after thrusting

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7 January 2021

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Cenozoic geology of the Yerington district, Nevada, and implications for the nature and origin of Basin and Range faulting

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Seismicity, crustal structure, and intraplate tectonics of the interior of the western Cordillera

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Deep structure of the Scottish Caledonides revealed by the MOIST reflection profile

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Basin-range structure in western North America: A review

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Regional tilt patterns of late Cenozoic basin-range fault blocks, western United States

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7 January 2021

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Regional Geophysics of the Basin and Range Province

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Low-angle normal faults in the Basin and Range Province: nappe tectonics in an extending orogen

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Cainozoic evolution of the state of stress and style of tectonism of the Basin and Range province of the western United States

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7 January 2021

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Identifiers

DOI

10.1029/JB091IB05P04826

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ADS bibcode

1986JGR....91.4826Z

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(Q97485590)

Extension of continental lithosphere: A model for two scales of basin and range deformation

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