White-box test generator tools rely only on the code under test to select test inputs, and capture the implementation’s output as assertions. If there is a fault in the implementation, it could get encoded in the generated tests. Tool evaluations usually measure fault-detection capability using the number of such fault-encoding tests. However, these faults are only detected, if the developer ca...

the zagros fold- thrust belt as a part of alpine- himalayan orogenic belt, is one of the most active continental collision zones on the earth, which extends from the tarus mountains in south eastern turkey to the minab fault in the east of the strait of hormoz in southern iran. structurally, its formation is related to the continuing convergent movement between the arabian plate to the southwes...

Process groups are a common abstraction for fault-tolerant computing in distributed systems. We present a security architecture that extends.Abstract Concerns about both security and fault-tolerance have had an important. Tion of fault tolerance will face some of the same problems, and benefit from. The security testing prototype is.A Secure and Fault-tolerant framework for Mobile. Of Computer ...

Changes in the physical landscape of SE Raasay at end last Quaternary glaciation are examined. The area is marked by a major fault system defining Beinn na Leac Fault Block, and field survey shows this to comprise rollover anticline SW, with extensional movement towards NE along an oblique transfer fault, Main Fault. was reactivated after Last Glacial Maximum. Survey distinctive ridge detached ...

In this paper, we investigate software fault detection and fault correction processes based on infinite server queuing model which incorporate testing effort functions. Some researches proposed in the literature to study fault detection and fault correction processes. However, most of them do not consider the amount of resources consumed during fault detection and fault correction processes. Th...

S U M M A R Y We investigate the representation of the radiated energy, E R, in earthquakes. In seismology E R is estimated from either far-field seismic waves or the stress and displacement on the fault plane. Although E R comes from the entire volume of the Earth, it can be expressed as an integral over the fault plane. However, the integrand cannot be given a simple physical meaning such as ...