Imported Swine Count, December 2010

The imported swine court report monthly by the Department of Agricultural.

Imported Swine Count, January 2011

The imported swine court report monthly by the Department of Agricultural.

Imported Swine Count, February 2011

The imported swine court report monthly by the Department of Agricultural.

Imported Swine Count, March 2011

The imported swine court report monthly by the Department of Agricultural.

Imported Swine Count, April 2011

The imported swine court report monthly by the Department of Agricultural.

Imported Swine Count, May 2011

The imported swine court report monthly by the Department of Agricultural.

Imported Swine Count, June 2011

The imported swine court report monthly by the Department of Agricultural.

Imported Swine Count, July 2011

The imported swine court report monthly by the Department of Agricultural.

Imported Swine Count, August 2011

The imported swine court report monthly by the Department of Agricultural.

Imported Swine Count, October 2011

The imported swine court report monthly by the Department of Agricultural.

Imported Swine Count, November 2011

The imported swine court report monthly by the Department of Agricultural.

Imported Swine Count, December 2011

The imported swine court report monthly by the Department of Agricultural.

Imported Swine Count, January 2012

The imported swine court report monthly by the Department of Agricultural.

Imported Swine Count, March 2012

The imported swine court report monthly by the Department of Agricultural.

Evolution of the Pelagonian carbonate platform complex and the adjacent oceanic realm in response to plate tectonic forcing (Late Triassic and Jurassic), Evvoia, Greece

The Late Triassic and Jurassic platform and the oceanic complexes in Evvoia, Greece, share a complementary plate-tectonic evolution. Shallow marine carbonate deposition responded to changing rates of subsidence and uplift, whilst the adjacent ocean underwent spreading, and then convergence, collision and finally obduction over the platform complex. Late Triassic ocean spreading correlated with platform subsidence and the formation of a long-persisting peritidal passive-margin platform. Incipient drowning occurred from the Sinemurian to the late Middle Jurassic. This subsidence correlated with intra-oceanic subduction and plate convergence that led to supra-subduction calc-alkaline magmatism and the formation of a primitive volcanic arc. During the Middle Jurassic, plate collision caused arc uplift above the carbonate compensation depth (CCD) in the oceanic realm, and related thrust-faulting, on the platform, led to sub-aerial exposures. Patch-reefs developed there during the Late Oxfordian to Kimmeridgian. Advanced oceanic nappe-loading caused platform drowning below the CCD during the Tithonian, which is documented by intercalations of reefal turbidites with non-carbonate radiolarites. Radiolarites and bypass-turbidites, consisting of siliciclastic greywacke, terminate the platform succession beneath the emplaced oceanic nappe during late Tithonian to Valanginian time.