This decommissioned ERA site remains active temporarily to support our final migration steps to https://ualberta.scholaris.ca, ERA's new home. All new collections and items, including Spring 2025 theses, are at that site. For assistance, please contact erahelp@ualberta.ca.
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Skip to Search Results- 1Canadian Cordillera
- 1Continental lithosphere
- 1Craton
- 1Crustal structure
- 1Finite-Frequency tomography
- 1Lithospheric structure
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Fall 2014
The development of dense, broadband seismic network provides a solid foundation for the implementation of a variety of seismic imaging methods. The integration of receiver function method and finite-frequency traveltime tomography offers high-resolution images of the crust and upper mantle...
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Fall 2018
The Western Canada Sedimentary Basin (WCSB) resides in a transition region from the Precambrian Canadian Shield to the Phanerozoic Cordillera. This broad foreland area has undergone more than three billion years of tectonic evolution from the Paleoproterozoic assembly of the Laurentian craton to...