... units 1 2 3 4 5 6 7 8 9 10 15 11 12 13 14 50 100 150 200 250 300 350 400 450 50 00 0 - 25 -50 Depth (Km) 55 0 crust mantle oceanic domain continental domain COT Fig. 29 Present bathymetry and structural setting ... 2 4 .50 E-01 4.00E-01 3 .50 E-01 3.00E-01 2 .50 E-01 2.00E-01 1 .50 E-01 1.00E-01 5. 00E-02 0.00E+00 AB 300 250 200 150 50 -200 - 150 -100 -50 50 100 150 200 250 300...
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... subsides, the risk of flooding increases, directly affecting local New Frontiers in Integrated Solid Earth Sciences Group picture – ILP meeting Frontiers in Integrated Solid Earth Science” – Potsdam ... process modelling 1 S. Cloetingh, J. Negendank (eds.), New Frontiers in Integrated Solid Earth Sciences, International Year of Planet Earth, DOI 10.1007/97...
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.New Frontiers in Integrated Solid Earth Sciences Phần 2 ppsx
... Wirth R., 2009, Integrated geo- sciences: from atomic scale to mountain buildings, in Cloet- ingh S. and Negendank J. (Eds), New Frontiers in Integrated Solid Earth Sciences, Springer. Dressler, ... Studies, in Cloetingh S. and Negendank J., (Eds), New Frontiers in Integrated Solid Earth Sciences, Springer, New York. Nakajima J. and Hasegawa A., 2007, Tomog...
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.New Frontiers in Integrated Solid Earth Sciences Phần 3 ppt
... 158 .5 D 34. 25 50 6.27E+12 5. 44E+12 87% 33 6 2 767 942 40.9 200 S 26 56 .5 5.46E+13 2.44E+13 41% 1 05 1 1 55 0 750 43.2 226 T 33 .5 47 5. 71E+12 4.63E+12 81% 25. 6 5 2 837 967 43.6 155 U 29. 75 46. 75 2.30E+13 ... produces in point U an increase close to 80% in both the integrated lithospheric and crustal strength and about 50 % in Te. In addition, the stronger lowe...
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.New Frontiers in Integrated Solid Earth Sciences Phần 4 pot
... 4b Gulf of Gascogne Western Mediterranean Paris Basin Hercynian Front 0 100 200 300 km 54 40 50 00 450 0 4000 350 0 3000 250 0 2000 150 0 1000 50 0 100 0 5 0 20km 10 13 std NE 0 5 10 13 std SW 54 40 50 00 450 0 4000 350 0 3000 250 0 2000 150 0 1000 50 0 ... the integration of fluid-rock 1 45 S. Cloetingh, J. Negendank (eds.), New Frontiers in Integrated Solid Earth Scie...
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.New Frontiers in Integrated Solid Earth Sciences Phần 6 docx
... Strain Accumulated Plastic Strain 50 0 -50 0 0 -1000 - 150 0 -2000 50 0 -50 0 0 8060 806040200 40200 0 0 -5 -10 - 15 -20 Depth (m)Depth (m) 0 -5 -10 - 15 -20 0 -5 -10 - 15 -20 Depth (m) -5 -10 - 15 -20 8.1e+04 5. 6e+07 ... published in 2002 by the United Nations 2 35 S. Cloetingh, J. Negendank (eds.), New Frontiers in Integrated Solid Earth Sciences, Internati...
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.New Frontiers in Integrated Solid Earth Sciences Phần 7 docx
... “non-volcanic 287 S. Cloetingh, J. Negendank (eds.), New Frontiers in Integrated Solid Earth Sciences, International Year of Planet Earth, DOI 10.1007/978-90-481-2737 -5_ 8, © Springer Science+Business Media ... other ancient continen- tal rifts, J. Geophys. Res. B Solid Earth Planets, 101(3), 54 59 54 75. Passive Seismic Monitoring of Natural and Induced Earthquakes 2 65...
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.New Frontiers in Integrated Solid Earth Sciences Phần 8 pps
... Ashikule Basin (AKB) in northwest- ern Tibet, in order to gain insight into the origin of the magmas produced in this continental collision setting. The basin contains several silicic domes ( 450 50 0 ... questions remain unanswered. Following is a discussion of some of the outstanding issues that are topics of ongoing research. Understanding Why Tremor Occurs in Certain Places By now...
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.New Frontiers in Integrated Solid Earth Sciences Phần 9 ppsx
... importance in geodesy, since Earth rotation, polar motion and crustal 349 S. Cloetingh, J. Negendank (eds.), New Frontiers in Integrated Solid Earth Sciences, International Year of Planet Earth, ... the deep Earth and its 373 S. Cloetingh, J. Negendank (eds.), New Frontiers in Integrated Solid Earth Sciences, International Year of Planet Earth, DOI 10.1007/97...
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.New Frontiers in Integrated Solid Earth Sciences Phần 10 pps
... 172f, 176, 199, 214, 238, 239, 243, 2 45, 250 – 252 , 255 , 256 , 258 , 264, 271, 278, 288, 289f, 316, 323, 3 25, 350 , 351 , 353 f, 359 , 360, 361f I ILP task force on sedimentary basins, 211 Iron and iron alloys, ... 350 , 352 , 355 , 356 , 358 , 359 , 360, 3 65, 366, 389 Lithosphere rheology, 112–1 15, 159 –188, 201f M Magma transport, 31, 326, 339, 340 Mantle, 2, 4, 5, 6, 9, 10, 11, 12...
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