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نمایش تعداد 1-10 از 14

Absolute plate velocities from seismic anisotropy: Importance of correlated errors

نوع: Journal Paper

نویسنده : Zheng, Lin - Gordon, Richard G. - Kreemer, Cornأ©

ناشر: American Geophysical Union

سال: 2014

Deep crustal structure in the eastern Gulf of Mexico

نوع: Journal Paper

ناشر: American Geophysical Union

سال: 2014

Why is Svalbard an island? Evidence for two-stage uplift, magmatic underplating, and mantle thermal anomalies

نوع: Journal Paper

نویسنده : Dörr,N.; Clift,P. D.; Lisker,F.; Spiegel,C.

ناشر: American Geophysical Union

سال: 2013

Comment on â€œA new model for the Paleogene motion of Greenland relative to North America: Plate reconstructions of the Davis Strait and Nares Strait regions between Canada and Greenlandâ€ by G. N. Oakey and J. A. Chalmers

نوع: Journal Paper

نویسنده : Denyszyn, Steven W. - Halls, Henry C.

ناشر: � American Geophysical Union

سال: 2014

Testing Iberian kinematics at Jurassic-Cretaceous times

نوع: Journal Paper

نویسنده : Neres,M.; Miranda,J. M.; Font,E.

ناشر: American Geophysical Union

سال: 2013

Slab detachment in laterally varying subduction zones: 3 D numerical modeling

نوع: Journal Paper

نویسنده : Duretz, T. - Gerya, T. V. - Spakman, W.

ناشر: American Geophysical Union

سال: 2014

Block like plate movements in eastern Anatolia observed by InSAR

نوع: Journal Paper

نویسنده : Cavaliأ©, Olivier - Jأ³nsson, Sigurjأ³n

ناشر: American Geophysical Union

سال: 2014

Asthenospheric Pacific Atlantic flow barriers and the West Scotia Ridge extinction

نوع: Journal Paper

ناشر: American Geophysical Union

سال: 2014

Revisiting the structure, age, and evolution of the Wharton Basin to better understand subduction under Indonesia

نوع: Journal Paper

نویسنده : Jacob, Jensen - Dyment, Jérôme - Yatheesh, V.

ناشر: � American Geophysical Union

سال: 2014

Flexural response of a continental margin to sedimentary loading and lithospheric rupturing: The mountain ridge between the Levant Basin and the Dead Sea Transform

نوع: Journal Paper

نویسنده : Steinberg, J. - Gvirtzman, Z. - Garfunkel, Z.

ناشر: American Geophysical Union

سال: 2014

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Absolute plate velocities from seismic anisotropy: Importance of correlated errors

Deep crustal structure in the eastern Gulf of Mexico

Why is Svalbard an island? Evidence for two-stage uplift, magmatic underplating, and mantle thermal anomalies

Comment on â€œA new model for the Paleogene motion of Greenland relative to North America: Plate reconstructions of the Davis Strait and Nares Strait regions between Canada and Greenlandâ€ by G. N. Oakey and J. A. Chalmers

Testing Iberian kinematics at Jurassic-Cretaceous times

Slab detachment in laterally varying subduction zones: 3 D numerical modeling

Block like plate movements in eastern Anatolia observed by InSAR

Asthenospheric Pacific Atlantic flow barriers and the West Scotia Ridge extinction

Revisiting the structure, age, and evolution of the Wharton Basin to better understand subduction under Indonesia

Flexural response of a continental margin to sedimentary loading and lithospheric rupturing: The mountain ridge between the Levant Basin and the Dead Sea Transform

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Absolute plate velocities from seismic anisotropy: Importance of correlated errors

Deep crustal structure in the eastern Gulf of Mexico

Why is Svalbard an island? Evidence for two-stage uplift, magmatic underplating, and mantle thermal anomalies

Comment on â€œA new model for the Paleogene motion of Greenland relative to North America: Plate reconstructions of the Davis Strait and Nares Strait regions between Canada and Greenlandâ€ by G. N. Oakey and J. A. Chalmers

Testing Iberian kinematics at Jurassic-Cretaceous times

Slab detachment in laterally varying subduction zones: 3 D numerical modeling

Block like plate movements in eastern Anatolia observed by InSAR

Asthenospheric Pacific Atlantic flow barriers and the West Scotia Ridge extinction

Revisiting the structure, age, and evolution of the Wharton Basin to better understand subduction under Indonesia

Flexural response of a continental margin to sedimentary loading and lithospheric rupturing: The mountain ridge between the Levant Basin and the Dead Sea Transform