The AAPG/Datapages Combined Publications Database
AAPG Bulletin
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AAPG Bulletin; Year: 2018; Issue: December DOI: 10.1306/05111817254
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Figure 9. The Late Jurassic was dominated by continuous transgression and basin widening. Continued sediment delivery to the North Slope and Hanna trough from the east and rifting within the Alaska–Chukotka microcontinent. Early accretion along the East Siberian shelf formed new provenance areas for sediment delivered to the South Anyui ocean. FJL = Franz Josef Land; NSI = New Siberian Islands; WI = Wrangel Island.
Figure 9. The Late Jurassic was dominated by continuous transgression and basin widening. Continued sediment delivery to the North Slope and Hanna trough from the east and rifting within the Alaska–Chukotka microcontinent. Early accretion along the East Siberian shelf formed new provenance areas for sediment delivered to the South Anyui ocean. FJL = Franz Josef Land; NSI = New Siberian Islands; WI = Wrangel Island.