 |
| Titel |
Field Evidence of Slab Break-off in the Internal Dinarides: An Emerging Picture of Dinaric Post Tethyan-Closure Tectonics. |
| VerfasserIn |
Gabriele Casale, Darrel Cowan, Richard Bennett, Goran Buble |
| Konferenz |
EGU General Assembly 2011
|
| Medientyp |
Artikel
|
| Sprache |
Englisch
|
| Digitales Dokument |
PDF |
| Erschienen |
In: GRA - Volume 13 (2011) |
| Datensatznummer |
250045701
|
|
|
|
|
|
| Zusammenfassung |
| Syn or post collisional extension is expressed in several Mediterranean orogens as mid-crustal rocks exhumed along low angle normal faults and has variously been attributed to slab roll-back or break-off. The Dinarides are a late Cretaceous-presently active fold-and-thrust belt driven by the collision between the Adria microplate and Eurasia. The Mid-Bosnian Schist Mountains (MBSM) are a fault bounded body of lower greenschist facies metamorphic rocks in the hinterland of the active Dinaric fold-and-thrust belt. Existing geologic maps and cross sections indicate that the faults bounding the MBSM are thrust faults and interpret the emplacement of these mid-crustal rocks as a compressional event. However, field observations along the fault bounding the east side of the MBSM support a normal shear sense suggesting an extensional tectonic exhumation. New low temperature thermochronolgic dates along with published Ar/Ar dates reveal an Eocene-Oligocene episode of relatively rapid cooling synchronous with foreland shortening. We propose that the MBSM represent the tectonic inversion from shortening to extension in an active fold-and-thrust belt. The relatively short duration and geographically restricted extent of exhumation supports a slab break-off event rather than an ongoing and migrating process (roll-back) as the exhumational driving force.
Several important considerations remain regarding the implications of tectonic inversion in the Dinaric setting. First, exhumation occurred along the paleogeographic margin of a thick carbonate platform. Second, tomographic images across the Dinarides reveal an intact shallowly dipping slab, the entirety of which may have been subducted following break-off of a pre-existing slab. The questions arise: What is the role of upper crustal lithology on microplate interaction, and what drives subduction in the absence of a negatively buoyant slab? |
|
|
|
|
|
|