JJPF (the Java/Jini Parallel Framework) is a framework that can run stream parallel applications on several parallel-distributed architectures. JJPF is actually a distributed execution server. It uses JINI to recruit the computational resources needed to compute parallel applications. Parallel applications can be run on JJPF provided they exploit parallelism accordingly to an arbitrary nesting ...

Abstract Faults and fractures are a critical store pathway for groundwater in Ireland’s limestone bedrock aquifers either directly as conductive structures or indirectly the locus development of karst conduits. From quantitative analysis post-Devonian faults range lithological sequences, this report describes principal characteristics Cenozoic strike-slip joints, youngest most intrinsically wit...

T he Bight Basin is a major frontier basin of Jurassic–Cretaceous age, which is currently undergoing renewed exploration interest. Although only limited data is available for understanding the petroleum systems in the basin, several observations indicate that poor fault seal integrity may represent a key exploration risk. The presence of a paleo-oil column in the Jerboa-1 well, interpreted gas ...

The evolution of oroclines is often driven by the interplay subduction and indentation associated with complex patterns deformation transfer from shortening to strike-slip extension. We study kinematics mechanics in an orocline a backarc-convex geometry, European Carpatho-Balkanides Mountains. Within this orocline, kinematic Serbian Carpathians segment less understood. results demonstrate that ...

We present a velocity and strain rate model for the northern Walker Lane derived from a compilation of geodetic velocities and corrected for transient effects owing to historic earthquakes on the Central Nevada seismic belt. We fi nd that from 37°N to 40°N, the Walker Lane is characterized by an ~100-km-wide zone with near-constant strain rates associated with ~10 mm yr total motion across the ...

structural evolution of alborz has already been mentioned by many researchers all over the world. central alborz is located in the bending of the eastern and the western alborz. damavand volcano is situated in the bending part along the great and active faults such as mosha, north of baijan, ask, nava and ira. the nava and ira faults are in the eastern side of damavand volcano with a trend of e...