Title: Looking from the orogen which is driving the backarc evolution
1Looking from the orogen which is driving the
backarc evolution
Liviu Matenco VU University Amsterdam, Faculty
of Earth and Life Sciences, Amsterdam, The
Netherlands
23.08.2008, Budapest, Hungary
VU University amsterdam
2Contents
- Introduction and overall units
- Pre-Miocene (i.e. orogenic) evolution of the
intra-Carpathian units - Carpathians shortening and back-arc opening
- The Carpathians collision when did it happen
- Pannonian-type of lithosphere how far and how
long - Post-orogenic evolution
3Integrated strength and EET of the European
lithosphere
Integrated strength distribution of the European
lithosphere
EET variations across Europe
Hardebol et al., 2006
Cloetingh et al., 2005
4Mesozoic evolution Oceans - how many?
Csontos Vörös, 2004
5The ALCADI system
Csontos Vörös, 2004
6The ALCADI system
Schmid et al., 2008
7Mesozoic reconstruction
Schmid et al., 2008
8Miocene Basins
Dolton, 2006
9Csontos Vörös, 2004
10Balla, 1987
11Lateral extrusion in the Alps
Post-Extrusion
Pre-Extrusion
Frisch et al., 2000
Ratschbacher et al., 1991 lateral extrusion
12Schmid et al., 2008
13The Polish Carpathians
Ozsczypko, 2006
14Ozsczypko, 2006
15Foreland-coupling - apparently a general
Carpathians ruleThe Polish Carpathians
Oszczypko, 2006
The Polish ridges foreland-coupling events
Poprawa and Malata, 2006
16Polish Carpathians, structure
Krzwiec et al., 2001, 2005
17Balla, 1987
18Docking the Alcapa with Tisza-Dacia The Piennides
Tischler et al., 2007
19The relationship between Transylvania and the
Piennides
Tischler et al., 2008
Foredeep deformation coeval with superimposed
foredeep wedges
Foredeep result of thrust loading
20Tischler et al., 2008
21The relationship between Transylvania and the
Piennides
Tischler et al., 2008
22- Überschiebungsrichtung konstant top SE
- zeitgleich mit Burdigalian clastic wedge
Tischler et al., 2007
23- -NW-SE Extensionsrichtung
- Bogdan-Dragos Voda Verwerfungssystem
- Versatz nach Osten abnehmend
Tischler et al., 2007
24Processes associated with the rotation and
indentation of Tisza-Dacia
25Regional structure
Schmid et al., 2008
26Detrital low temperature thermochronology
27Tectonic evolution
Fuegenschuh and Schmid, 2005
28Compiled fission track ages
Fuegenschuh and Schmid, 2005
29Compiled fission-track ages, South Carpathians
30The Sadu-Petrila fault
Fuegenschuh and Schmid, 2005
31Palinspastic reconstructions, South Carpathians
after Ratschbacher et al. (1993), Schmid et al.
(1998)
32Stratigraphic correlation and tectonic evolution
scheme, South Carpathians
Matenco Schmid (1999)
334. The Carpathians collision when did it happen
Schmid et al., 2008
34Problem statement - Growth of an orogenic wedge
and collisional exhumation
Reiners and Brandon, 2006
Hoth, 2005
Willett and Brandon, 2002
35Double vergent orogenic wedges orogens
dominated by convergence evolution of the
Central Alps
Rate of convergence versusRate of subduction
D A-A gt D B -B
Schmid et al., 1996
Royden and Burchfield, 1989
36Orogens dominated by subduction the Carpathians
37Orogenic core IIExhumation derived from sequence
stratigraphy in the back-arc basin
Krezsek et al., 2008
38Transition from shortening to back-arc collapse
lithospheric structure
Dererova et al., 2006
Szabo et al., 2004
39Upper crustal deformation Different upper
crustal structure in Pannonian and Transylvania
Tari et al., 1999
40Upper crustal deformation Exhumation of
Pannonian during initial simple-shear phase
Tari, 1996
41Transylvania Summary
1. Transylvania post-collisional history
- Intra-Albian (Mid-K, Austrian) Transylvanides
(over)thrusting in two steps - Post-Albian
extensional collapse - Intra-Turonian E-ward
Apuseni thrusting - post-Turonian, pre-top K
small grabens - Top-K (Laramian) inversion -
Eocene shortening
- Small normal faults during the Late Cretaceous.
In Transylvania two areas in particular hanging
wall of the Puini thrust (Internal Dacides,
Tisza) and Deleni structure. - Often smaller
Lower Miocene offsets - Symmetric small
grabens. - Age pre- Cretaceous Puini, i.e. pre-
intra-Turonian phase.
42Transition from shortening to back-arc collapse
lithospheric structure
Dererova et al., 2006
Szabo et al., 2004
43Post-orogenic ACADI Strain transfer from the
active Adriatic, Aegean and Vrancea deformation
fronts
Heidbach et al., 2007
Vrancea
Adria
Aegean
van der Hoeven et al., 2005
Grenerczy et al., 2005
Kahle et al., 1999
44SE Carpathians the relationship between upper
crustal and deep lithosphere
Matenco et al., 2007
45Carpathians deep structure
Ismail-Zadeh et al., 2005
Martin et al., 2006
46A bunch of models for the Vrancea slab
- slab detachment
- continental delamination
- delamination
Wortel and Spakman, 2000
Knapp et al., 2005
- detachment and delamination
Girbacea and Frisch, 1998
Gvirtzman, 2002
Cloetingh et al., 2004
47The last one
Viscous flow
Houseman and Gemmer, 2007
48SE Carpathians the relationship between upper
crustal and deep lithosphere
Matenco et al., 2007
49Custal folding main syncline Focsani basin
2. SE Carpathians post-collisional history
Matenco et al., 2007
502. SE Carpathians post-collisional history
Leever et al., 2006
Matenco et al., 2007
51Coupling between lithospheric and surface
processes folding
Link between (integrated) mantle strength and
wavelength of lithospheric folding
Cloetingh et al., 2006
Sokoutis et al., 2005. Tectonophysics
52Collision mechanics folding during collision
and decoupled
Type-1 model representing a cold lithosphere with
a strong upper mantle
Type-2 model simulating the collision between two
different lithospheric blocks
Sokoutis et al., 2005
53Tomographic sections across the Eifel plume
Ritter et al., 2001
54Coupling between mantle and surface processes
Guillou-Frottier et al., 2006
55Coupling between deep Earth and surface processes
Guillou-Frottier et al., 2006
56A typical research for the BASIN MASTER
programme dedicated to basin development
processes, mountain building, characteristics of
the deep lithosphere, thermochronological
methods, fluid flow or petroleum systems
Core universitiesVU University Amsterdam,
Université de Rennes 1, Eötvös University
Budapest, University of Technology Aachen,
Université Pierre et Marie Curie Paris 6
Universitetet i Bergen, Norway Industry and
institutesSHELL International, Total-Fina-Elf,
MOL, StatoilHydro, Institut Francais du Petrole,
Bureau de Recherches Geologiques et Minieres,
GeoForschungszentrum Potsdam, TNO Applied
Geosciences
http//www.basinmaster.eu