Moho Structure Across the Backarc‐Craton Transition in the Northern U.S. Cordillera

Author:

DiCaprio L.1ORCID,Maiti T.1ORCID,Dettmer J.1,Eaton D. W.1ORCID

Affiliation:

1. Department of Geoscience University of Calgary Calgary Alberta Canada

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference97 articles.

1. Amante C. &Eakins B.(2009).Etopo1 1 arc‐minute global relief model: Procedures data sources and analysis.https://doi.org/10.7289/V5C8276M

2. Armstrong R. L. &Ghosh D. K.(1990).Westward movement of the 87Sr/g6Sr=.704 line in southern British Columbia from Triassic to Eocene time: Monitoringthe tectonic overlap of accreted terranes on North America; in Southern Cordillera Transect Workshop Lithoprobe Report 11 p. 53–56.p.A4.

3. Early Proterozoic basement exposures in the southern Canadian Cordillera: core gneiss of Frenchman Cap, Unit I of the Grand Forks Gneiss, and the Vaseaux Formation

4. Rb-Sr and K-Ar geochronometry of Mesozoic granitic rocks and their Sr isotopic composition, Oregon, Washington, and Idaho

5. Plateau uplift in western Canada caused by lithospheric delamination along a craton edge

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