RSTT
3.2.0
Regional Seismic Travel Time
|
Cutil::Brents< F > | Class supports Brents zeroF and minF functions that finds the root of or minimum (maximum) of a provided function given an input range containing the root (or minimum or maximum) and a convergence tolerance |
Cutil::Brents< taup::TPZeroFunctional > | |
Cslbm::CrustalProfileStore | CrustalProfileStore supports pool allocation for CrustalProfile objects |
Cutil::DataBuffer | A byte array container used to hold binary data in the same manner as disk based file system |
Cutil::f1 | First MD5 algorithmic operation function object. Optimized from x & y | ~x & z |
Cutil::f2 | Second MD5 algorithmic operation function object |
Cutil::f3 | Third MD5 algorithmic operation function object |
Cutil::f4 | Fourth MD5 algorithmic operation function object |
Cslbm::GeoStack | Manages all information related to a single node in a Grid object |
▼CGeoTessModel | |
Cslbm::GeoTessModelSLBM | |
▼Cslbm::GreatCircle | Manages information related to a great circle path between two Locations on the Earth, including the ability to compute the total travel time from a seismic source to a receiver |
Cslbm::GreatCircle_Xg | Manages information related to a great circle path between two Locations on the Earth. Its computeTravelTime() methods compute travel times for Pg or Lg phases |
Cslbm::GreatCircle_Xn | Manages information related to a great circle path between two Locations on the Earth. It uses the Zhao method to compute travel times for Pn and Sn phases |
Cslbm::GreatCircleFactory | A factory class that will return the correct type of GreatCircle object for the specified phase |
▼Cslbm::Grid | A 2 dimensional, horizontal grid of GirdProfile objects |
Cslbm::GridGeoTess | |
Cslbm::GridSLBM | A 2 dimensional, horizontal grid of GirdProfile objects |
Cutil::IntegrateFunction< F > | Class supports numerical integration of an arbitrary function using a fourth order Simpsons rule for closed intervals. Open intervals at one end-point are handled by using Simpsons rule in a segmented sense to approach the unbounded limit in successive iterations each time dividing the difference to the unbounded limit by 10.0 |
Cutil::IntegrateFunction< taup::TPdDistdr< V > > | |
Cutil::IntegrateFunction< taup::TPdTaudr< V > > | |
▼Cslbm::InterpolatedProfile | A Profile object based on values interpolated from nearby GridProfile objects |
Cslbm::CrustalProfile | A profile through the Earth model that stores interface radius, and interval P or S wave velocity information about the crustal stack below either the source or the receiver |
▼Cslbm::LayerProfile | A Profile object based on values interpolated from nearby GridProfile objects |
Cslbm::LayerProfileG | A LayerProfile with mantle velocity gradient information |
Cslbm::QueryProfile | An InterpolatedProfile object that also has information about the the P and S wave velocity as a function of depth for all layers, and the velocity gradient in the mantle |
▼Cslbm::Location | The Location Class manages a single point in/on the Earth, which is described by the GRS80 ellipsoid |
▼Cslbm::GridProfile | Manages all information related to a single node in a Grid object |
Cslbm::GridProfileGeoTess | Manages all information related to a single node in a Grid object |
Cslbm::GridProfileSLBM | Manages all information related to a single node in a Grid object |
Cutil::MD50 | This code implements the MD5 message-digest algorithm. The algorithm is due to Ron Rivest. This code was written by Colin Plumb in 1993, no copyright is claimed. This code is in the public domain; do with it what you wish |
Cutil::md5step< f > | Primary MD5 algorithmic step function object. The function object is templated (class f) off of the four MD5 functions f1, f2, f3, and f4 defined below |
Cslbm::SLBMException | An Exception class for Grid and related objects |
▼Cslbm::SlbmInterface | The primary interface to the SLBM library, providing access to all supported functionality |
Cslbm::SlbmInterfaceToJNI | Adds functionality to SlbmInterface to support the Java Native Interface (JNI). The JNI allows libSLBM to be accessed using programs written in the Java programing language |
Ctaup::SplitDistance | Function object used by the Brents minF function to find the minimum (or maximum) of a retrograde layer. The function operator() defines a TauPSite::integrateDistance(...) function as the functional for finding the minimum for some ray parameter p. This object is only used in the TauPModel::findLimits(...) function when a retrograde layer is detected |
Ctaup::TauPException | An Exception class for TauP and related objects |
Ctaup::TauPSite | |
Ctaup::TPdDistdr< V > | Distance Integrand. Integrating this function over radius yields distance |
Ctaup::TPdTaudr< V > | |
▼Ctaup::TPVelocityLayer | Abstract base class velocity layer model inherited by all concrete velocity layer classes. The inheritance hierarchy for a typical velocity layer object, VL, is: |
▼Ctaup::VelocityIntegrate< VelocityCubic > | |
Ctaup::VelocityCubic | Cubic velocity model returns a cubicly modeled velocity between the top and bottom of the layer as a function of the radius |
▼Ctaup::VelocityIntegrate< VelocityPower > | |
Ctaup::VelocityPower | Power Law velocity model returns a power law modeled velocity between the top and bottom of the layer as a function of the radius. This object overrides the numerical distance and time integration with analytic definitions |
▼Ctaup::VelocityIntegrate< VelocityConst > | |
Ctaup::VelocityConst | Constant velocity model returns a single value for velocity irregardless of the input radius value. This object overrides the numerical distance and time integration with analytic definitions |
▼Ctaup::VelocityIntegrate< VelocityQuadratic > | |
Ctaup::VelocityQuadratic | Quadratic velocity model returns a quadraticly modeled velocity between the top and bottom of the layer as a function of the radius |
▼Ctaup::VelocityIntegrate< VelocityLinear > | |
Ctaup::VelocityLinear | Linear velocity model returns a linearly modeled velocity between the top and bottom of the layer as a function of the radius. This object overrides the numerical distance integration with an analytic definition |
Ctaup::VelocityIntegrate< V > | |
Ctaup::TPZeroFunctional | The primary layer search functional used by Brents zeroIn(...) function to find layers that contain a turning ray whose distance matches the distance between the source and receiver |
Ctaup::TravelTimeResult | A public container (struct) that holds the result of a specific ray that satisfied the source distance / depth! requirement. This object maintains all pertinent information related to the ray for subsequent retrieval and evaluation |
Cslbm::Triangle | |
Cslbm::UncertaintyPDU | A UncertaintyPDU object contains the raw data to calculate a path dependent modeling error in seconds as a function of distance in radians along a specific source-receiver path traced through the model |
Cslbm::UncertaintyPIU | A UncertaintyPIU object contains the raw data to calculate a modeling error in seconds as a function of distance in radians |
Ctaup::VZero< V > | A function object used to zero-in on the velocity at r that gives the input ray parameter (vzP). The operator() returns r - vzP * vzV(r) where r is input and vzP is set and vzV(r) is the velocity function. This function object is used when r cannot be solved for explicitly |