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Progress in Earth and Planetary Science
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Fig. 10 | Progress in Earth and Planetary Science

Fig. 10

From: The architecture of long-lived fault zones: insights from microstructure and quartz lattice-preferred orientations in mylonites of the Median Tectonic Line, SW Japan

Fig. 10

Variation in quartz [c]-axis LPO strength (as indicated by fabric intensity) and the relative proportion of point and girdle components of the LPOs with distance from the MTL in the Tsukide (a–b) and Ako–Miyamae (c–d) areas. Cluster = S1 – S2, girdle = 2 × (S2 – S3), where S1–3 represent the eigenvalues of the normalised orientation tensor (Vollmer 1990)

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