EGU General Assembly 2007
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  List of Accepted Contributions - GD01 Geodynamics and Geochemistry of the Early Earth (co-listed in TS & GMPV)

Please, click Abstract Number to find the corresponding abstract as PDF file; if necessary, download Adobe Acrobat Reader 4.0 first to open the file. Any abstract may be freely reproduced for non-commercial, scientific purposes; however, the moral right of the author(s) to be identified as the author(s) of such abstracts is asserted.

Markov, A.
Geodynamic evolution of North-Caspian Region with the purpose of prognosis of a big Gas and Oil deposits in shelf - to - basin Caspian sedimentary Devonian Continental Margins.

Markov, A.
Geodynamic of South-Kurilian Arc System and subduction of Pacific Plate.

Sarkarinejad, K.
Kinenimatics of the tectonic wedging of the oblique Zagros accretionary prism and lateral exhumation of the HP-LT metamorphic rocks, southwestern Iran.

Varlamova, A.; Sadovnikov, A.; Novikov, D.
Layered Proterozoic PGE-bearing intrusions on the N-E Baltic Shield: new U-Pb on zircon and He4/He3 for accessory minerals data

Sharkov, E.; Bogina, M.
Major geological catastrophe in the history of the Earth: evidence from evolution of tectonomagmatic processes in the Paleoproterozoic

Samuel, H; Tackley, P J
Core Formation in Terrestrial Planets by Negative Diapirism

Galimov, E; Bibikova, E
Geodynamic and geochronological Approach to the Formation and Evolution of the Early Earthís Crust

Abdeen, M. M.; Abdelghaffar, A. A.
Post-accretionary structures in the Pan-African central

Golabek, G.; Schmeling, H.
Earthís core formation aided by flow channelling induced by Rayleigh-Taylor instabilities

Rollinson, H
Can we recognise early Archaean mantle in the rock record ?

Slabunov, A.I.
Archaean collisional orogen: the main stages and duration of the Archaean lithospheric evolution of the Belomorian province (Fennoscandian Shield)

Benn, K.; Moyen, J.-F.
The Late Archean Abitibi-Opatica terrane, Superior Province: a Late Archean oceanic plateau modified by subduction and slab window magmatism (withdrawn)

Stroncik, N.A.; Niedermann, S.; Haase, K.M.
Helium and neon isotopes as tracers of mantle evolution, mantle dynamics and mantle reservoirs

Chardon, D.; Jayananda, M.; Peucat, J.J.; Chetty, T.R.K
Forced flow and growth of weak Precambrian lithosphere: 3D crustal-scale perpective from a tilted craton

Khachay, Y
Research of the structure and thermal Earthís evolution at the stage of itís accumulation in a frame of 2-d model

Muehlenbachs, K.; Furnes, H.; de Wit, M.
Oxygen isotope composition of the Archean seafloor and its implication of early seafloor spreading

Davaille, A; Arndt, N
When hot thermochemical instabilities trigger subduction and continental growth : the episodic Earth history.

Flament, N.; Coltice, N.; Rey, P.
Emerged land surface in the Archean: constraints on continental growth and mantle thermal history

Halla, J.; Heilimo, E.
Archean sanukitoid series granitoids and their implications for the plate tectonic theory

Liu, S.; Fraser, D. G.
The effect of temperature on the adsorption of biomolecules on halloysite clay (withdrawn)

Hansen, U. ; Schmalzl, J. ; Stemmer, K.
Dynamical evolution of layered structures in the early Earth

Enjolvy, R; Moniť, P; Bruguier, O; Delor, C; Barbey, P; Bosch, D
The Transamazonian juvenile crust of French Guiana revisited: New LA-ICP-MS U-Pb and Ar/Ar geochronological data.

van Hunen, J; van Thienen, P
The evolution of plate tectonics

Halls, H.C.; Davis, D.W.; Stott, G.M.; Ernst, R.E.
The Paleoproterozoic Marathon Large Igneous Province: new evidence for a 2.1 Ga long-lived mantle plume event along the southern margin of the North American Superior craton

Riedel, M.R.
Nanoscale properties of rocks and subduction zone rheology:

Harrison, T.M.; McCulloch, M.T.; Freeman, J.; Mojzsis, S.J.
Origin and evolution of the Hadean crust

Sitdikova, L.; Izotov, V.
Deep geo-observatories as a tool for monitoring nonequilibrium geological and geophysical processes

Porcelli, D.; Elliott, T.
Continuing He/U fractionation in the mantle and the generation of high 3He/4He ratios in ocean island basalts

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