#Quake ii intro software
#Quake ii intro code

A general description is provided in Benito et al. Scientific participation (SSHAC levels) and review processДocumentation describing model preparation The major earthquakes were published in Benito et al.

(1993) with recents contributions of data from each Central America country. After Bitterman, the protagonist of Quake II, near-singlehandedly dealt a major blow to the Strogg.

#Quake ii intro software

The game was developed by Raven Software using the id Tech 4 engine (the engine created for Doom ), and it's set in the Strogg arc as a follow-up to the events of Quake II. he catalogue used is based on the ones proposed by Rojas et al. Quake IV is the fourth entry in the Quake series, released in 2005. Click the show map layers icon to view different source models and base layer maps. The map below depicts the annual occurrence rate per source (between minimum and maximum magnitudes) for the different source models included in the hazard model. In the active shallow crust the source zones are modelled as NRML areaSource, while in the subduction region the source zones are modelled as NRML complexFaultSource representing both, interface and intraslab sources. The source model is implemented in a unique source model file in NRML format representing the different typology and tectonic region type defined in the original model. The PSHA model is implemented using basically the information published in Benito et al. A detailed description of the source zones is included in Benito et al. The crustal zones (h в‰¤ 25 km) have been modeled with a 2D geometry, while a 3D geometry was considered for interface (25 km 60 km), with exception of the interface zone related to the north PanamГЎ belt (flat zone at 50km of depth). As a result, maps in terms of peak ground acceleration (PGA) and spectral accelerations SA (T) for periods of 0.1, 0.2, 0.5, 1, and 2s were obtained, as well as uniform hazard spectra (UHS) for six major cities of the region.ДЄ regional seismogenic zonation with three tectonic regimes (active shallow crustal, subduction interface, and subduction intraslab) was defined.ДЄll the source zones were defined as area sources.

#Quake ii intro code

The original seismic hazard calculation was made using CRISIS2007 code in a grid of 0.1 x 0.1 degrees (aprox 10 km), for return periods of 200, 1000, and 2500 years. After a comparison with local strong motion data (statistical analysis of residuals) a set of GMPEs associated with the tectonic regimes present in the region (active shallow crust, volcanic, subduction interface, and subduction intraslab) were defined. The seismotectonic models proposed in the previous phase (RESIS-I) were revised and two seismogenic zonations proposed (see details below). In this context a parametric earthquake catalog for the region was compiled and homogenized to moment magnitude, Mw. As part of the RESIS-II cooperation project a PSHA model has been developed by a seismic-hazard team from Costa Rica, Guatemala, Honduras, Nicaragua, el Salvador, Panama, Norway and Spain (Benito et al., 2010, 2012).