Lancaster Aulacogen information

The Lancaster Aulacogen is a geological structure underlying Lancaster Sound and Prince Regent Inlet in the Arctic Archipelago of Nunavut, Canada.^[1] It formed as a result of extensional tectonics during the Eurekan Rifting Episode, which took place in the Canadian Arctic Rift System from the Cretaceous to the Tertiary.^[2]

^ Kerr, J. Wm. (1979). "Structural Framework of Lancaster Aulacogen, Arctic Canada". Open File 619. Geological Survey of Canada: 31.
^ E. M. Nairn, Alan; Churkin, Jr., Michael; G. Stehli, Francis (1981). The Ocean Basins and Margins: The Arctic Ocean. Vol. 5. Springer Science+Business Media. p. 166. ISBN 978-1-4757-1250-6.

[1] Kerr, J. Wm. (1979). "Structural Framework of Lancaster Aulacogen, Arctic Canada". Open File 619. Geological Survey of Canada: 31.

[2] E. M. Nairn, Alan; Churkin, Jr., Michael; G. Stehli, Francis (1981). The Ocean Basins and Margins: The Arctic Ocean. Vol. 5. Springer Science+Business Media. p. 166. ISBN 978-1-4757-1250-6.