Progress in Earth and Planetary Science

Table 1 Fault-slip dataset of the meso-scale faults obtained by Naruse and Otsubo (2011a) and misfit angles on the meso-scale faults. When a stress with a misfit of < 30° is judged to be compatible (e.g., Nemcok and Lisle 1995), then stresses A, C, D, and F can explain slip vectors on 20 faults (excluding the data for faults 4 and 7). This result indicates that only stresses A, C, D, and F can be adopted as the optimum solution in this study. In other words, stresses B and E are not needed to explain the data

From: Temporal changes in the internal stresses and pore pressures in a large-scale submarine mass transport deposit

No.	Faults				Misfit angle (°)
No.	Strike (°)	Dip (°)	Rake (°)	Sense	Stress A	Stress B	Stress C	Stress D	Stress E	Stress F
1	N23W	74S	R85E	N	2	3.3	93.5	146.2	149.4	3.6
2	N24W	62S	R80E	N	2.3	2.3	90.2	140.7	117.2	34.6
3	N34W	48S	R90W	N	8.2	25.2	95.8	172.7	122.3	144.2
4	N14W	88S	R13W	N	92.4	91.3	164.7	142.2	31.9	101.5
5	N40E	68N	R74E	R	156.8	146.5	13.3	9.4	136.9	34.7
6	N18W	64S	R87E	N	5.8	12.3	97.4	141.7	110.8	6.8
7	N30W	80S	R85E	N	2.3	4.9	97.2	155.4	164.9	0.3
8	N45W	72N	R73E	N	1.3	120.7	8	19.3	65.5	161.8
9	N50W	66S	R86E	N	3.4	14.5	131.1	155.1	151.4	32.3
10	N16W	40S	R25W	R	102.9	41.9	10	3.2	2.2	92.6
11	N4E	40N	R16E	R	93.4	8.3	15.6	17.7	7	104.4
12	N23W	68S	R76E	N	6.6	3.8	85.6	136.8	118.6	12.3
13	N22W	50S	R52E	R	151.5	167.9	116.9	77.7	100.8	4.3
14	N16W	27S	R60E	R	167.6	55.2	105.6	143.4	99.5	1.2
15	N12E	40N	R30E	R	108.1	31.5	9.4	7.5	5.8	92.1
16	N8W	60S	R45W	R	124.6	111.9	30.6	2.8	42.7	65.6
17	N33W	62S	R62E	R	157.7	157.9	107	40.1	68.4	122.6
18	N10W	20S	R20W	R	85.6	60.8	0.8	57.9	2.6	104
19	N68W	58S	R54E	R	144.9	135.2	3.7	19	68.3	53.6
20	N30W	82N	R34W	N	76	131	23.6	29.7	148.5	112.2
21	N64W	84N	R50E	N	3.6	91.9	8.1	5	27.7	121.9
22	N42W	82S	R20W	R	117.9	123.4	17	73.1	78.7	115.5

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