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

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2 Plenary Session Organisation Host Institution Departement of Earth Sciences of the ETH Zurich Patronnage Platform Geosciences, Swiss Academy of Sciences Program Committee Daniel Ariztegui Stefano Bernasconi Rizlan Bernier-Latmani Gilles Borel Hugo Bucher Beat Bürki Lionel Cavin Nathalie Chèvre Reynald Delaloye Pierre Dèzes Hans-Rudolf Egli Markus Egli Werner Eugster Charles Fierz David Floess Swiss Geoscience Meeting 2011 Karl Föllmi Markus Furger Isabelle Gärtner-Roer Alain Geiger Bernard Grobéty Irka Hajdas Kurt Hanselmann Elena Havlicek Christoph Heinrich Adrian Jakob Christophe Joerin Edi Kissling Florian Kober Rainer Kündig Local Organizing Committee Helmut Weissert Neil Mancktelow Peter Ulmer Eric Reusser Neil Mancktelow Peter Bayer Stefano Bernasconi Alain Geiger Florian Kober Franziska Nyffenegger Nils Oesterling Adrian Pfiffner Rolf Philipona Eric Reusser Bruno Schädler Michael Schaepman Jürg Schweizer Manfred Thüring Peter Ulmer Dea Voegelin Helmut Weissert Adrian Wiget Peter Brack Paul Tackley Hugo Bucher Christophe Schneble Platform Geosciences, Swiss Academy of Science, SCNAT
Participating Societies and Organisations Federal Office of Meteorology and Climatology (MeteoSwiss) Federal Office of Topography (swisstopo) Forum for Climate and Global Change (ProClim<strong>–</strong>) International Geosphere-Biosphere Programme, Swiss Committee (IGBP) International Union of Geodesy and Geophysics, Swiss Committee (IUGG) International Union of Geological Sciences, Swiss Committee (IUGS) Kommission der Schweizerischen Paläontologischen Abhandlungen (KSPA) Steering Committee NRP 61 (SNSF) Swiss Association of Geologists (CHGEOL) Swiss Commission for Oceanography and Limnology (COL) Swiss Commission for Phenology and Seasonality (CPS) Swiss Commission for Remote Sensing (SCRS) Swiss Commission on Atmospheric Chemistry and Physics (ACP) Swiss Geodetic Commission (SGC) Swiss Geological Society (SGG/SGS) Swiss Geological Survey (swisstopo) Swiss Geomorphological Society (SGGm/SSGm) Swiss Geophysical Commission (SGPK) Swiss Geotechnical Commission (SGTK) Swiss Group for Engineering Geology (SFIG) Swiss Hydrogeological Society (SGH) Swiss Hydrological Commission (CHy) Swiss Meteorological Society (SGM) Swiss National Science Foundation (SNSF) Swiss Paleontological Society (SPG/SPS) Swiss Snow, Ice and Permafrost Society (SIP) Swiss Society for Hydrology and Limnology (SGHL / SSHL) Swiss Society for Microbiology (SSM) Swiss Society for Quaternary Research (CH-QUAT) Swiss Society of <strong>Mineralogy</strong> Petrography (SMPG / SSMP) Swiss Soil Science Society (SSSS) Swiss Tectonics Studies Group (Swiss Geologiocal Society) Platform Geosciences, Swiss Academy of Science, SCNAT Swiss Geoscience Meeting 2011 3 Plenary Session
Page 1 and 2: Abstract Volume 9 th Swiss Geoscien
Page 3: 9 th Swiss Geoscience Meeting, Zuri
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
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Figure 1: Geographical location (N
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1.D.5 Dextral movements between the
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ding aftershock distribution that t
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Figure 1: Lateral facies variations
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There are no 3D numerical studies w
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Figure 1. The Doruneh fault satelli
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Table 2. Specific Activity of urani
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nism on Earth, which forms very sma
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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
Page 179 and 180:
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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Page 203 and 204:
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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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
Page 251 and 252:
REFERENCES Farinotti, D., S. Usselm
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REFERENCES GRETILLAT, P.-A., 1992 :
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Page 257 and 258:
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
Page 267 and 268:
P 9.1 On the reliability of indicat
Page 269 and 270:
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
Page 287 and 288:
Page 289 and 290:
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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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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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
Page 373 and 374:
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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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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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
Page 405 and 406:
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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Page 437 and 438:
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
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