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Figure 1 | Earth, Planets and Space

Figure 1

From: Changes in illite crystallinity within an ancient tectonic boundary thrust caused by thermal, mechanical, and hydrothermal effects: an example from the Nobeoka Thrust, southwest Japan

Figure 1

Geologic setting of the Nobeoka Thrust. (a) Geologic setting of the Nobeoka Thrust and distribution of the Shimanto Belt in Southwest Japan. (b) A simplified geologic map of the Shimanto Belt in northeast Kyushu, modified from Murata (1998). (c) Geologic map of the studied area and the locality of the drilling site (dot) for the hanging wall of the Nobeoka Thrust (modified from Kondo et al. 2005; Kimura et al. 2013; Hamahashi et al. 2013).

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