Skip to main content
Progress in Earth and Planetary Science
Figure 7 | Progress in Earth and Planetary Science

Figure 7

From: Mechanism of long-standing Cenozoic basin formation in central Hokkaido: an integrated basin study on an oblique convergent margin

Figure 7

Configuration of sedimentary basins in the Minaminaganuma stage (late Oligocene) and Kawabata stage (middle Miocene). Fault names adopted for numerical modeling are after Kusumoto et al. (2013) and annotated in the figure. Isopach map of the Kawabata stage is after the Association of Natural Gas Mining and Association for Offshore Petroleum Exploration (1982).

Back to article page