Table 1 Summary of experiments.

From: Dehydration-driven stress transfer triggers intermediate-depth earthquakes

Exp.

Sample

φatg (%)

σ m (GPa)

(GPa)

/

AEs nb.

ɛ at 923K (%)

D1665

00–1.2

0

1.2±0.1

2.2±0.1

1.8±0.1

1

21

D1617

05–1.1

5

1.1±0.1

1.5±0.1

1.4±0.1

37

22

D1619

20–1.1

20

1.1±0.1

0.9±0.1

0.8±0.1

0

14

D1777

20–1.2

20

1.2±0.1

1.4±0.1

1.2±0.1

0

21

D1778

00–3.5

0

3.5±0.1

2.8±0.1

0.8±0.1

8

23

D1659

05–3.5

5

3.5±0.1

1.9±0.1

0.5±0.1

12

21

D1662

20–3.5

20

3.5±0.1

2.0±0.1

0.6±0.1

16

22

D1779

50–3.5

50

3.5±0.1

1.3±0.1

0.4±0.1

14

21

  1. Conditions and sample characteristics for the eight experiments performed under Synchrotron X-ray beam: antigorite fraction φatg, initial mean stress at the beginning of deformation σm, differential stress , ratio between effective and differential stresses, number of recorded AEs during the experiment and strain ɛ at 923 K. The first column shows the name of the experiment in GSECARS experimental database. The second column shows the sample name, defined with antigorite content and confining pressure.