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From: The crustal stress field of Germany: a refined prediction
Layer ID | Name | Density (kg/m3) | Young’s modulus (GPa) | Poisson’s ration (−) | Friction angle (°) | Cohesion (MPa) | Tensile strength (MPa) |
---|---|---|---|---|---|---|---|
2 | Relict elements | 2400a | 15b | 0.29b | 38b | 10b | 5 |
3 | Sediments outside 3DD | 2700 | 30 | 0.25 | 38b | 10b | 5 |
4 | Cenozoic volcanics | 2860a | 54c | 0.25c | 50i | 39i | 5 |
5 | Cenozoic sediments of the NGB | 2480a | 15b | 0.29b | 38b | 10b | 5 |
6 | Cenozoic sediments of the URG | 2300a | 15b | 0.29b | 38b | 10b | 5 |
7 | Cenozoic sediments of the Molasse Basin | 2350a | 15b | 0.29b | 38b | 10b | 5 |
8 | Folded Molasse | 2400a | 15b | 0.29b | 38b | 10b | 5 |
9 | Thrusted units of the Alps | 2700a | 23c | 0.25c | 40 | 25 | 5 |
10 | Cretaceous | 2590a | 20c | 0.25c | 40j | 18j | 7k |
11 | Jurassic | 2600a | 20c | 0.26c | 36b,j | 15b,j | 5 |
12 | Triassic | 2650a | 28c | 0.25c | 36b,j | 31b,j | 5 |
13 | Zechstein salt | 2100a | 25g | 0.27g | – | – | – |
14 | Zechstein carbonates | 2400a | 30c | 0.25c | 50i | 18i | 5 |
15 | Rotliegend sediments | 2600a | 15c | 0.19c | 43l,m | 25l,m | 5l,m |
16 | Rotliegend volcanics | 2650a | 26c | 0.25c | 40l | 57l | 15l |
17 | Pre-Permian | 2670a | 40c | 0.25h | 40l,n | 15l,n | 5l,n |
18 | Upper crust ALCAPA | 2750d | 70h | 0.25h | 40b,c | 30b,c | 5 |
19 | Upper crust ATA | 2790e | 70h | 0.25h | 40b,c | 30b,c | 5 |
20 | Upper crust AV | 2820d | 70h | 0.25h | 40b,c | 30b,c | 5 |
21 | Upper crust EEC | 2810d | 70h | 0.25h | 40b,c | 30b,c | 5 |
22 | Lower crust | 3000d,e | 80h | 0.25h | 40b,c | 30b,c | 5 |
1 | Lithospheric mantle | 3300e,f | 130 | 0.25h | 40b,c | 30b,c | 5 |