GEO-4840 TECTONICS-S05 PART 1: LECTURES [ Wed (16) ] 19/1 - 09/3 PART 2: STUDENT PROJECTS [ Presentations ] 13/4 PART 3: FIELD TEACHING [ Corsica ] end April PART 4: FIELD REPORTS [ Hand in ] 11/5 PART 5: EVALUATION [PROJECTS, REPORTS & EXAM] 14/6

LECTURES: Introduction and course content; Anatomy and tectonic processes in mountain belts. Main themes: 1) Material balance and properties Uplift and subsidence. Topography, crustal and lithospheric thicknesses/structure 2) Wilson cycle tectonics, Ocean-continent transition, Oceanic complexes, exotic terranes. Ophiolite obduction, (Oman, Caledonian and Appalachian). Andean margins, Incipient continental collision, Australia - Banda Arc collision. Continental collision GEO-4840 TECTONICS-S05

LECTURES (continued): 3) Examples of Continental collision zones: The Himalayan-Tibetan region The Caledonides, with emphasis on Scandinavia Mediterranean 4) From collision to extension, Dynamics of orogenic wedges, Exhumation, Renewed rifting.

Student projects (written and oral presentation): All projects are related to the field-course/work/excursions. The student seminar day will be Wed. 13. April 1)The Herzynian basement of Corsica () 2)The main tectonic units of the Alps and their correlation with Alpine Corsica. () 3)The structural geology of Alpine Corsica, an overview () 4)The high-pressure metamorphism of Alpine Corsica () 5)Exhumation of high-pressure rocks in the transect from Corsica to the Apennines in Italy () 6)The Alpine ophiolitic rocks of Corsica () 7)Formation of Pseudotachylytes () 8)Formation of Olistostromes ()

MOUNTAIN CHAINS ARE THE MOST IMPRESSIVE VISIBLE TOPOGRAPHIC FEATURES ON THE EARTH´S SURFACE MOUNTAIN CHAINS ARE THE MOST IMPRESSIVE VISIBLE TOPOGRAPHIC FEATURES ON THE EARTH´S SURFACE

The anatomy of mountain belts: The product of complex interactions of thrusting and extension accompanied by pro- and retrograde metamorphic reactions and erosional denudation The anatomy of mountain belts: The product of complex interactions of thrusting and extension accompanied by pro- and retrograde metamorphic reactions and erosional denudation

MOUNTAIN BELTS, OLD (at least from Mid Proterozoic) and YOUNG, HAVE VERY SIMILAR INTERNAL STRUCTURES: FORELAND CONTINENTAL BASEMENT-CORED NAPPES SUTURE WITH OCEANIC AND EXOTIC TERRANES HINTERLAND / PLATEAU REGIONS FORELAND

Various stages of orogenic maturity along strike Andean margins Foreland flexure Foreland basin Suture(s) Hinterland orogenic plateau Common internal structure of orogenic belts (in space and time)

5) Remnant stage Continental collision, suture zones, deform- ation and metamorphism, mountain building Extensional collapse, faulting and collapse basins 4) Terminal stage Near closure of ocean, mature arcs and back-arc, accreationary wedges, HP-LT metamorphic complexes (Mediterranean See area) 3) Vaning stage: Intra-oceanic subduction and island arcs transition to Andean margins. (SE Asia and Western Passific) 2) Mature stage Passive margins with large shelf-areas (Atlantic Ocean) 1) Embryonic to Young stage. Rifts to small ocean basin with sea-floor spreading. (East African rift and Red Sea) Schematic view of stages in a classical Wilson cycle

Le Pichon et al., 1993 Exact estimates of material present in the orogen

ESTIMATES OF MISSING CONTINENTAL MATERIAL Topography and erosional levels are taken into consideration: Dewey et al. (1986) ca 1,2 x 10 4 km 2 Le Pichon et al (1993) Linear shortening between km Surface loss during the past 45 myr from 57 to 62 x 10 5 km 2 Rate of surface loss: ≈ 1,1 x 10 km 2 x yr Arial deficit in sections ≈ x 10 5 km 2 (max) x 10 5 km 2 (min) (Depends on estimates of original surface elevation) WHAT IS THE EXPLANATIONS FOR THE DEFICIT? IndiaTarim erosion Present continental crust

1)LATERAL TRANSPORT OF MATERIAL

Tapponnier et al., 1982, 1986 The lateral extrusion model For SE Asia

Fournier Jolivet et al.

2) VERTICAL TRANSPORT OF MATERIAL (SUBDUCTION / EDUCTION)