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Table 1 Observed velocity reduction and aspect ratio and fluid fraction of H2O-filled pores in the lower crust.

From: Deep crustal structure around the Atotsugawa fault system, central Japan: A weak zone below the seismogenic zone and its role in earthquake generation

 

Atotsugawa fault system

Niigata-Kobe Tectonic Zone

 

Pyroxene amphibolite

Hornblende-pyroxene gabbro

Pyroxene amphibolite

Hornblende-pyroxene gabbro

dlnV p

−0.10

−0.13

−0.058

−0.088

dlnV s

−0.11

−0.12

−0.085

−0.092

dlnV s /dlnV p

1.10

0.92

1.44

1.05

Aspect ratio

0.04–0.05

0.2

0.01–0.02

0.05–0.06

Volume fraction

2–3%

10%

0.8%

3–4%