The most popular hypothesis for the origin of the Amerasia Basin of the Arctic Ocean is that it formed by the anticlockwise rotation of northern Alaska and...
Twelve second- and third-order T-R (transgressive-regressive) sequence boundaries have been delineated in the Triassic succession of the Sverdrup Basin, Arctic...
Sequence stratigraphy is based, for the most part, on the recognition and correlation of a variety of stratigraphic surfaces that
collectively can be...
Transgressive-regressive (T-R) sequence analysis has been applied to the Jurassic succession of the Sverdrup Basin with sequence boundaries drawn at subaerial...
Recently published Upper Paleozoic and Mesozoic paleogeographic syntheses for Arctic Euramerica (e.g. Ziegler, 1988; Green and Kaplan, 1987) do not include a...
To delineate more closely the age and evolution of the Amerasia Basin of the Arctic Ocean, a breakup unconformity has been identified in sedimentary basins...
Carnian (Lower Upper Triassic) strata occur throughout the Sverdrup Basin and are up to 1500 m thick. The strata outcrop in the Eurekan fold and thrust belt of...
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