2. Mineralogy – Petrology – Geochemistry - SWISS GEOSCIENCE ...

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Edited by the Swiss Academy of Sciences Cover page images (author: Pierre Dèzes, SCNAT): Large picture: Mammoth Hot Springs, Yellowstone National Park, Park County, Wyoming, USA Small picture: Alpine ibex, (Capra ibex). Brienzer Rothorn, Berner Oberland, Switzerland.
9 th Swiss Geoscience Meeting, Zurich 2011 Table of contents Organisation 2 Abstracts 0. Plenary Session 4 1. Structural Geology, Tectonics and Geodynamics 10 2. Mineralogy – Petrology – Geochemistry 82 3. Low-Temperature Isotope Geochemistry 138 4. Perspectives on batholith formation and evolution in 4D 156 5. Geomorphology 184 6. Quaternary Research 200 8. Hydrology and Sustainable Water Resources Management in View of Global Changes 230 9. Open Cryosphere Session 254 10. Meteorology and Climatology 286 11. Greenhouse Gases: Linkages between Biosphere and Climate 286 12. Natural or man-made mineral dust and its influence on humans, environment and climate 294 14. Traces of life on planet Earth: A tribute to the late Professor Lukas Hottinger 306 15. Geoscience and Geoinformation - From data acquisition to modelling and visualisation 332 16. Earth System Science related Earth Observation 350 17. Synergies between Advancements in Geodesy and other Geosciences 364 18. Advances in GIScience and Remote Sensing 378 20. Deep Geothermal Energy 394 21. Geophysics and Rockphysics 410 22. Special symposium in honor of Daniel Bernoulli & Albert Matter 434 http://geoscience-meeting.scnatweb.ch
Page 1: Abstract Volume 9 th Swiss Geoscien
Page 5 and 6: Participating Societies and Organis
Page 7 and 8: 1 The origin of the Earth and its v
Page 9 and 10: REFERENCES Alvarez, L. W., F. Alvar
Page 11 and 12: Platform Geosciences, Swiss Academy
Page 13 and 14: POSTERS «Global & Planetary» 1.A.
Page 15 and 16: 1.1 Unravelling of continued magmat
Page 17 and 18: 1.3 A simple thermo-mechanical shea
Page 19 and 20: dismembered and partly underplated
Page 21 and 22: 1.6 Causes of single-sided subducti
Page 23 and 24: Figure 3. Simulation snapshots of a
Page 25 and 26: pected formation temperature. The r
Page 27 and 28: 1.12 Spatial distribution of quartz
Page 29 and 30: The lateral continuity of the Helve
Page 31 and 32: Figure 1. Schematic block diagram (
Page 33 and 34: 1.16 Thermal evolution in a spheric
Page 35 and 36: Figure 2: Simulations with multiple
Page 37 and 38: Figure 1. Top: Schematic map of nor
Page 39 and 40: Late Precambrian Late Cambrian - Ea
Page 41 and 42: REFERENCES Bunte, M.K., Williams, D
Page 43 and 44: pressures, deformation by interstic
Page 45 and 46: Figure 2. Determination of the temp
Page 47 and 48: 1.B.2 Long term evolution of subduc
Page 49 and 50: 1.B.4 Decoupled and coupled multile
Page 51 and 52: with time (c) 7.2 Myr and (d) 13.5
Page 53 and 54:
1.C.2 Plastic deformation of quartz
Page 55 and 56:
1.C.5 Mechanics of kink-bands durin
Page 57 and 58:
1.C.8 Grain size evolution in 2D nu
Page 59 and 60:
Figure 1: Tectonic Map of the Fribo
Page 61 and 62:
Figure 1: Geographical location (N
Page 63 and 64:
1.D.5 Dextral movements between the
Page 65 and 66:
ding aftershock distribution that t
Page 67 and 68:
Figure 1: Lateral facies variations
Page 69 and 70:
There are no 3D numerical studies w
Page 71 and 72:
Figure 1. The Doruneh fault satelli
Page 73 and 74:
Table 2. Specific Activity of urani
Page 75 and 76:
nism on Earth, which forms very sma
Page 77 and 78:
REFERENCES Simoes, M. and Avouac, J
Page 79 and 80:
REFERENCE: Aridhi K., Ould Bagga M.
Page 81 and 82:
1.E.9 Direct versus indirect thermo
Page 83 and 84:
Figure 1: Schematic tectonic map of
Page 85 and 86:
POSTERS: P 2.1 Arlaux Y., Poté J,,
Page 87 and 88:
2.1 C-O-H solubility under reduced
Page 89 and 90:
largest partial molar volume compon
Page 91 and 92:
REFERENCES Bonev, I. 2007: Crystal
Page 93 and 94:
REFERENCES Antignano, A. & Manning,
Page 95 and 96:
2.9 Percolation and impregnation of
Page 97 and 98:
2.11 Fluid chemistry and fluid-rock
Page 99 and 100:
A pile of up to 7000 m of volcanic
Page 101 and 102:
2.15 Fluid composition and mineral
Page 103 and 104:
Caucasus, close to the Iranian bord
Page 105 and 106:
2.19 Application of high-precision
Page 107 and 108:
lish the possible reaction path for
Page 109 and 110:
P 2.4 Stratigraphy and sedimentolog
Page 111 and 112:
P 2.6 Geology of Piz Duan: an ocean
Page 113 and 114:
Figure 2. Summary of LA-ICPMS conco
Page 115 and 116:
P 2.9 New age constraints on the op
Page 117 and 118:
P 2.11 The influence of bulk and mi
Page 119 and 120:
P 2.13 Petrographic and sedimentolo
Page 121 and 122:
P 2.15 The Petrology and Geochemist
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Peridotites from the Dehshekh Massi
Page 125 and 126:
REFERENCES Conticelli, S., Guranier
Page 127 and 128:
P 2.21 Stratigraphic successions in
Page 129 and 130:
Aknowledgement This study was suppo
Page 131 and 132:
Water-settled pyroclastic fall depo
Page 133 and 134:
P 2.26 Main Features of the Tectoni
Page 135 and 136:
Figure 1. (A and B) Reconstruction
Page 137 and 138:
P 2.29 The coupling of deformation
Page 139 and 140:
P 2.31 When did the large meteorite
Page 141 and 142:
3.1 Late Albian Carbon Isotope Stra
Page 143 and 144:
3.3 Solution speciation controls me
Page 145 and 146:
3.5 Clumped isotope analysis of Poz
Page 147 and 148:
REFERENCES Erickson, B.E., & Helz,
Page 149 and 150:
Extreme events such as destructive
Page 151 and 152:
REFERENCES Archer, C. & Vance D., 2
Page 153 and 154:
P 3.1 A volcanically induced climat
Page 155 and 156:
P 3.2 In the Tethys Ocean black sha
Page 157 and 158:
Swiss Geoscience Meeting 2011 Platf
Page 159 and 160:
POSTERS: P 4.1 Broderick, C., Schal
Page 161 and 162:
4.2 The importance of visco-elasto-
Page 163 and 164:
4.4 Andesite production in a deep c
Page 165 and 166:
4.6 Petrologic consequences of vari
Page 167 and 168:
ages of the NE-Adamello with the Mi
Page 169 and 170:
The example of the Adamello batholi
Page 171 and 172:
4.12 Fluid evolution of the Monte M
Page 173 and 174:
4.14 Magma Emplacement Tectonics: W
Page 175 and 176:
P 4.2 2D numerical modelling of flu
Page 177 and 178:
P 4.4 Trace-element partitioning in
Page 179 and 180:
REFERENCES Hamilton, M.A., Pearson,
Page 181 and 182:
P 4.8 Textures and chemistry of zir
Page 183 and 184:
REFERENCES Bindeman I. 2008 Reviews
Page 185 and 186:
P 4.11 Field relations and conseque
Page 187 and 188:
5.1 Quaternary Geologic Map of Osog
Page 189 and 190:
5.4 Tectonics, Climate, and Mountai
Page 191 and 192:
Intense rainfall events may trigger
Page 193 and 194:
P 5.1 InSAR Terrasar-X visibility a
Page 195 and 196:
P 5.3 Landscape Evolution of the H
Page 197 and 198:
Most of the other factors like slop
Page 199 and 200:
P 5.8 Crack air convection and resu
Page 201 and 202:
Page 203 and 204:
POSTERS P 6.1 Brönnimann D., Ismai
Page 205 and 206:
6.2 Stalagmite evidence for a highl
Page 207 and 208:
6.4 Nature and Timing of Terminatio
Page 209 and 210:
6.6 Fluid inclusions in stalagmites
Page 211 and 212:
6.8 Paleoenvironmental changes in e
Page 213 and 214:
6.10 The recurrence pattern of mega
Page 215 and 216:
6.12 Exposure ages from erratic bou
Page 217 and 218:
6.14 Phylogeographic and morphologi
Page 219 and 220:
We thank the ELEMO Scientific Progr
Page 221 and 222:
P 6.4 Preliminary archeomagnetic re
Page 223 and 224:
Anisotropy of magnetic susceptibili
Page 225 and 226:
Table 1- Quaternary Chronostratigra
Page 227 and 228:
P 6.10 A multidisciplinary approach
Page 229 and 230:
like tsunami. Further detailed stud
Page 231 and 232:
Page 233 and 234:
8.1 Respiration and microbial dynam
Page 235 and 236:
8.3 Water management and allocation
Page 237 and 238:
Figure 1: Glacier de la Plaine Mort
Page 239 and 240:
8.6 Karst system characterization (
Page 241 and 242:
cess points to the groundwater. Add
Page 243 and 244:
8.10 Real-time spatiotemporal combi
Page 245 and 246:
REFERENCES Barnett T., J.Adam, and
Page 247 and 248:
P 8.1 Effect of climatic forcing on
Page 249 and 250:
P 8.2 Impact of the uncertainty in
Page 251 and 252:
REFERENCES Farinotti, D., S. Usselm
Page 253 and 254:
REFERENCES GRETILLAT, P.-A., 1992 :
Page 255 and 256:
Page 257 and 258:
POSTERS P 9.1 Alig C., Mitterer C.,
Page 259 and 260:
We could show that both a critical
Page 261 and 262:
9.5 Recent glacier changes in the A
Page 263 and 264:
9.8 Seismological Experiments on th
Page 265 and 266:
tive sites. Analyzing more samples
Page 267 and 268:
P 9.1 On the reliability of indicat
Page 269 and 270:
Figure 1. Overview of the study reg
Page 271 and 272:
The internationally coordinated col
Page 273 and 274:
REFERENCES Bahr, D. B., M. F. Meier
Page 275 and 276:
P 9.10 Stability information suppli
Page 277 and 278:
Figure 1. Resistivity - temperature
Page 279 and 280:
P 9.13 The first complete inventory
Page 281 and 282:
P 9.16 Monitoring temporal changes
Page 283 and 284:
9.18 Study of a new Svalbard ice co
Page 285 and 286:
P 9.20 Glacier Laser-scanning Exper
Page 287 and 288:
Page 289 and 290:
10.1 Numerical simulations of short
Page 291 and 292:
10.3 New balloon sounding technic u
Page 293 and 294:
10.5 Radiation errors and uncertain
Page 295 and 296:
P 10.1 A simple statistical model f
Page 297 and 298:
12.1 Dust analysis in human lungs K
Page 299 and 300:
Figure 2: concentration of selected
Page 301 and 302:
The examined particles range from 2
Page 303 and 304:
Figure 1. Comparison of the cytotox
Page 305 and 306:
P12.2 Sediments size characteristic
Page 307 and 308:
Page 309 and 310:
POSTERS: P 14.1 Costeur L., Domenic
Page 311 and 312:
14.2 Palaeoenvironmental reconstruc
Page 313 and 314:
Our results suggest that oceanograp
Page 315 and 316:
14.5 Biogeographic morphological in
Page 317 and 318:
Considerable amounts of the platfor
Page 319 and 320:
14.8 Recovery Patterns of Chondrich
Page 321 and 322:
14.10 Terrestrial ecosystems during
Page 323 and 324:
P 14.1 A Cretaceous fish takes a fa
Page 325 and 326:
The site “Les Plantées” is sit
Page 327 and 328:
P 14.4 Mining morphological evoluti
Page 329 and 330:
Knappertsbusch, M., 2004 - 2009: Mo
Page 331 and 332:
P 14.7 The Exogyra aquila Marls (Lo
Page 333 and 334:
P 14.8 Pushing life to the extreme:
Page 335 and 336:
15.1 Managing authentication and pe
Page 337 and 338:
15.3 GIS-based modeling for landsli
Page 339 and 340:
15.5 Earth Modeling Seen from a Mul
Page 341 and 342:
Figure 1 Current progress on develo
Page 343 and 344:
Fig.1: Numerical Model of the basin
Page 345 and 346:
15.9 Numerical modelling for risk s
Page 347 and 348:
Results The resulting dataset inclu
Page 349 and 350:
A passive seismic acquisition campa
Page 351 and 352:
Page 353 and 354:
16.1 Investigating variations of gr
Page 355 and 356:
16.3 Retrieval of the ECV „snow s
Page 357 and 358:
16.5 Fusion of Digital Elevation Mo
Page 359 and 360:
Figure 2. Comparison of displacemen
Page 361 and 362:
P 16.3 Consistent Trends in Water V
Page 363 and 364:
Figure 1. Melting snow observed in
Page 365 and 366:
Random selection Active selection S
Page 367 and 368:
17.1 Station velocities in Switzerl
Page 369 and 370:
Figure 2. System prototype housed i
Page 371 and 372:
17.5 Gravity Field Determination at
Page 373 and 374:
REFERENZEN Brockmann, E., Grünig,
Page 375 and 376:
P 17.1 Permanent monitoring of rock
Page 377 and 378:
Figure 1.Time series of 2-hour solu
Page 379 and 380:
Page 381 and 382:
18.1 Automatic identification of fo
Page 383 and 384:
3D reference data is measured manua
Page 385 and 386:
ing 3D-matrices for each flight tra
Page 387 and 388:
Until now, most (semi)-automated sp
Page 389 and 390:
REFERENCES: Angert, A., Biraud, S.,
Page 391 and 392:
cy from these products requires cor
Page 393 and 394:
This contribution reports on curren
Page 395 and 396:
Page 397 and 398:
20.1 Prospects of Deep Geothermal E
Page 399 and 400:
20.3 Deep geothermal systems - adva
Page 401 and 402:
20.5 Enhanced Geothermal Systems (E
Page 403 and 404:
20.7 Process simulation: understand
Page 405 and 406:
20.9 Key success factors for Enhanc
Page 407 and 408:
We estimate stress drops of the ind
Page 409 and 410:
P 20.4 Changes of Coulomb Failure S
Page 411 and 412:
P 20.6 Geothermal energy potential
Page 413 and 414:
21.1 Macroscopic Source Properties
Page 415 and 416:
Attenuation arises due to induced p
Page 417 and 418:
nuous background medium. The contin
Page 419 and 420:
Figure 1 The distribution of polari
Page 421 and 422:
21.8 The long-term seismic cycle at
Page 423 and 424:
Figure 1: The results of the gravit
Page 425 and 426:
P 21.3 Toward source characterizati
Page 427 and 428:
P 21.5 Physical mechanisms for low-
Page 429 and 430:
Poshtkuh basin is located in Semnan
Page 431 and 432:
REFERENCES Jackson, I., and M. S. P
Page 433 and 434:
REFERENCES Goloshubin, G., Van Schu
Page 435 and 436:
Page 437 and 438:
22.1 Sediment budgets and fluvial d
Page 439 and 440:
Biochronologically controlled trans
Page 441 and 442:
Fig. 1. Section across the N part o
Page 443 and 444:
Sedimentary Petrology. 61, 1173-118
Page 445 and 446:
22.8 Tectonics versus palaeoceanogr
Page 447 and 448:
Eclogae Geologicae Helvetiae, v. 99
Page 449 and 450:
P 22.1 The Cretaceous-Tertiary tran
Page 451 and 452:
The young age of these km-sized fly
Page 453:
evolution of the basin is character
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