- Page 1 and 2: Abstract Volume 9 th Swiss Geoscien
- Page 3 and 4: 9 th Swiss Geoscience Meeting, Zuri
- 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: The lateral continuity of the Helve
- 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.
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1.E.9 Direct versus indirect thermo
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Figure 1: Schematic tectonic map of
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POSTERS: P 2.1 Arlaux Y., Poté J,,
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2.1 C-O-H solubility under reduced
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largest partial molar volume compon
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REFERENCES Bonev, I. 2007: Crystal
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REFERENCES Antignano, A. & Manning,
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2.9 Percolation and impregnation of
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2.11 Fluid chemistry and fluid-rock
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A pile of up to 7000 m of volcanic
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2.15 Fluid composition and mineral
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Caucasus, close to the Iranian bord
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2.19 Application of high-precision
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lish the possible reaction path for
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P 2.4 Stratigraphy and sedimentolog
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P 2.6 Geology of Piz Duan: an ocean
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Figure 2. Summary of LA-ICPMS conco
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P 2.9 New age constraints on the op
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P 2.11 The influence of bulk and mi
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P 2.13 Petrographic and sedimentolo
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P 2.15 The Petrology and Geochemist
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Peridotites from the Dehshekh Massi
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REFERENCES Conticelli, S., Guranier
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P 2.21 Stratigraphic successions in
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Aknowledgement This study was suppo
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Water-settled pyroclastic fall depo
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P 2.26 Main Features of the Tectoni
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Figure 1. (A and B) Reconstruction
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P 2.29 The coupling of deformation
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P 2.31 When did the large meteorite
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3.1 Late Albian Carbon Isotope Stra
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3.3 Solution speciation controls me
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3.5 Clumped isotope analysis of Poz
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REFERENCES Erickson, B.E., & Helz,
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Extreme events such as destructive
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REFERENCES Archer, C. & Vance D., 2
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P 3.1 A volcanically induced climat
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P 3.2 In the Tethys Ocean black sha
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Swiss Geoscience Meeting 2011 Platf
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POSTERS: P 4.1 Broderick, C., Schal
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4.2 The importance of visco-elasto-
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4.4 Andesite production in a deep c
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4.6 Petrologic consequences of vari
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ages of the NE-Adamello with the Mi
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The example of the Adamello batholi
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4.12 Fluid evolution of the Monte M
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4.14 Magma Emplacement Tectonics: W
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P 4.2 2D numerical modelling of flu
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P 4.4 Trace-element partitioning in
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REFERENCES Hamilton, M.A., Pearson,
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P 4.8 Textures and chemistry of zir
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REFERENCES Bindeman I. 2008 Reviews
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P 4.11 Field relations and conseque
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5.1 Quaternary Geologic Map of Osog
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5.4 Tectonics, Climate, and Mountai
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Intense rainfall events may trigger
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P 5.1 InSAR Terrasar-X visibility a
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P 5.3 Landscape Evolution of the H
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Most of the other factors like slop
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P 5.8 Crack air convection and resu
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Swiss Geoscience Meeting 2011 Platf
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POSTERS P 6.1 Brönnimann D., Ismai
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6.2 Stalagmite evidence for a highl
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6.4 Nature and Timing of Terminatio
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6.6 Fluid inclusions in stalagmites
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6.8 Paleoenvironmental changes in e
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6.10 The recurrence pattern of mega
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6.12 Exposure ages from erratic bou
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6.14 Phylogeographic and morphologi
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We thank the ELEMO Scientific Progr
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P 6.4 Preliminary archeomagnetic re
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Anisotropy of magnetic susceptibili
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Table 1- Quaternary Chronostratigra
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P 6.10 A multidisciplinary approach
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like tsunami. Further detailed stud
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Swiss Geoscience Meeting 2011 Platf
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8.1 Respiration and microbial dynam
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8.3 Water management and allocation
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Figure 1: Glacier de la Plaine Mort
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8.6 Karst system characterization (
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cess points to the groundwater. Add
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8.10 Real-time spatiotemporal combi
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REFERENCES Barnett T., J.Adam, and
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P 8.1 Effect of climatic forcing on
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P 8.2 Impact of the uncertainty in
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REFERENCES Farinotti, D., S. Usselm
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REFERENCES GRETILLAT, P.-A., 1992 :
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Swiss Geoscience Meeting 2011 Platf
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POSTERS P 9.1 Alig C., Mitterer C.,
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We could show that both a critical
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9.5 Recent glacier changes in the A
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9.8 Seismological Experiments on th
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tive sites. Analyzing more samples
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P 9.1 On the reliability of indicat
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Figure 1. Overview of the study reg
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The internationally coordinated col
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REFERENCES Bahr, D. B., M. F. Meier
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P 9.10 Stability information suppli
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Figure 1. Resistivity - temperature
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P 9.13 The first complete inventory
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P 9.16 Monitoring temporal changes
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9.18 Study of a new Svalbard ice co
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P 9.20 Glacier Laser-scanning Exper
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Swiss Geoscience Meeting 2011 Platf
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10.1 Numerical simulations of short
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10.3 New balloon sounding technic u
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10.5 Radiation errors and uncertain
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P 10.1 A simple statistical model f
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12.1 Dust analysis in human lungs K
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Figure 2: concentration of selected
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The examined particles range from 2
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Figure 1. Comparison of the cytotox
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P12.2 Sediments size characteristic
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Swiss Geoscience Meeting 2011 Platf
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POSTERS: P 14.1 Costeur L., Domenic
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14.2 Palaeoenvironmental reconstruc
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Our results suggest that oceanograp
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14.5 Biogeographic morphological in
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Considerable amounts of the platfor
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14.8 Recovery Patterns of Chondrich
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14.10 Terrestrial ecosystems during
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P 14.1 A Cretaceous fish takes a fa
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The site “Les Plantées” is sit
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P 14.4 Mining morphological evoluti
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Knappertsbusch, M., 2004 - 2009: Mo
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P 14.7 The Exogyra aquila Marls (Lo
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P 14.8 Pushing life to the extreme:
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15.1 Managing authentication and pe
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15.3 GIS-based modeling for landsli
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15.5 Earth Modeling Seen from a Mul
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Figure 1 Current progress on develo
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Fig.1: Numerical Model of the basin
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15.9 Numerical modelling for risk s
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Results The resulting dataset inclu
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A passive seismic acquisition campa
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Swiss Geoscience Meeting 2011 Platf
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16.1 Investigating variations of gr
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16.3 Retrieval of the ECV „snow s
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16.5 Fusion of Digital Elevation Mo
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Figure 2. Comparison of displacemen
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P 16.3 Consistent Trends in Water V
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Figure 1. Melting snow observed in
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Random selection Active selection S
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17.1 Station velocities in Switzerl
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Figure 2. System prototype housed i
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17.5 Gravity Field Determination at
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REFERENZEN Brockmann, E., Grünig,
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P 17.1 Permanent monitoring of rock
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Figure 1.Time series of 2-hour solu
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Swiss Geoscience Meeting 2011 Platf
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18.1 Automatic identification of fo
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3D reference data is measured manua
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ing 3D-matrices for each flight tra
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Until now, most (semi)-automated sp
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REFERENCES: Angert, A., Biraud, S.,
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cy from these products requires cor
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This contribution reports on curren
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Swiss Geoscience Meeting 2011 Platf
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20.1 Prospects of Deep Geothermal E
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20.3 Deep geothermal systems - adva
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20.5 Enhanced Geothermal Systems (E
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20.7 Process simulation: understand
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20.9 Key success factors for Enhanc
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We estimate stress drops of the ind
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P 20.4 Changes of Coulomb Failure S
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P 20.6 Geothermal energy potential
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21.1 Macroscopic Source Properties
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Attenuation arises due to induced p
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nuous background medium. The contin
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Figure 1 The distribution of polari
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21.8 The long-term seismic cycle at
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Figure 1: The results of the gravit
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P 21.3 Toward source characterizati
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P 21.5 Physical mechanisms for low-
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Poshtkuh basin is located in Semnan
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REFERENCES Jackson, I., and M. S. P
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REFERENCES Goloshubin, G., Van Schu
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Swiss Geoscience Meeting 2011 Platf
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22.1 Sediment budgets and fluvial d
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Biochronologically controlled trans
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Fig. 1. Section across the N part o
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Sedimentary Petrology. 61, 1173-118
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22.8 Tectonics versus palaeoceanogr
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Eclogae Geologicae Helvetiae, v. 99
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P 22.1 The Cretaceous-Tertiary tran
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The young age of these km-sized fly
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evolution of the basin is character