Titlebook: Joint Interpretation of Geophysical and Geological Data Applied to Lithospheric Studies; P. Giese,D. Roeder,R. Nicolich Book 1991 Kluwer A

現(xiàn)任者

,Fine Modeling of the Elastic and Anelastic Parameters of the Earth’s Crust by Means of Complete Synl selected geometrical phases in structural models which may contain also lateral dishomogeneties. An interesting alternative approach is represented by the superposition of normal modes which allows the exact synthesis of both geometrical and non geometrical phases and hence a more complete structural modeling.

反復(fù)拉緊

Enhanced Interpretation of Crustal Sections with the Thrustbelt Program,. The program generates cross-sections which are automatically balanced. It is shown that profiles produced by the program present more information than is immediately apparent from the geological and geophysical input data. The program is applicable for sedimentary belts as well as for the entire crust.

來自于

Crop-Ecors Activity in the Western Alps,flection line, recorded in 1986 and completed in 1987. The preliminary results and the geological constraints indicate the existence of a crustal accretion prism below the Western Alps and three lithospheric thrusts may be envisaged.

APRON

喪失

An Introduction to Geophysical Databases and Two Examples of the Use for Crustal Studies,emperature conditions. Secondly, SEDABA (.ction .ta .se) will be described. This database can be used for the quick and effective access and manipulation of vertical sections (e.g. interpreted seismic and geological sections).

細(xì)胞膜

Geophysical and Geological Parameters Being Important for Modeling,ory seismic data with stratigraphic flield data (Case study: Serre, S. Calabria) can provide the necessary data base to construct a seismic model for the earth’s crust of a particular geological area.

Fortuitous

A Seismic Tomography Program for Geological Investigations,e system of linear equations. To regularize the solution in areas of bad resolution, options are available to minimize the norm of the solution, its gradient, or a combination of these two. In general, minimization of the gradient will give best results.

憤慨一下

MANIA

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