Crustal Structures under the Active Volcanic Areas of Central and Eastern Mediterranean (M-44)

摘要

Programs are being adapted to the UNIVAC 1000 computer and others are being developed for immediate utilization in processing MAGSAT data. The magnetization intensity, susceptability, Koeningsberger ratio, NMR stbility against alternated fields and temperature, and the Curie temperature were determined for some rock formations with mineralogical compositions stable to the intermediate for lower continental crust and to upper manele conditions. Attempts to residuate crustal anomalies from one selected profile passing through western mediterranean using procedures commonly used at NASA yielded dubious results because of uncertainties in the adoption of coefficients in the expression accounting for the effect of equatorial ring currents and the empirical approach used for other corrections. Instead, filtering techniques are to be applied to each profile once invesigator B tapes relative to the whole planet are received.