Preaching in postmodern times : a peer mentoring preaching program for effective Biblical preaching within the emerging postmodern context

https://place.asburyseminary.edu/ecommonsatsdissertations/1209/thumbnail.jp

Magnetic studies for lunar samples Final technical progress report

Paleomagnetic studies of volcanic rock

Final technical report on the Surface Electrical Properties Experiment Part 3

This report consists of a series of reports, reprints and preprints that in themselves constitute a self-explanatory record of the work performed by the University of Toronto on the Surface Electrical Properties Experiment. Areas discussed include: data handling and processing, installation and external signal application, operation of the equipment, and digital output. Detailed circuit descriptions are included. A complete unified discussion of the electromagnetic response of a plane stratified structure is reported. A detailed and comprehensive analysis of the theoretical parts of the electromagnetic is given. The numerical problem of computing numbers of the electromagnetic field strengths is discussed. It is shown that the analysis of the conductive media is not very far removed from the theoretical analysis and the numerical difficulties are not as acute as for the low-loss problem.Submitted to MIT in fulfillment of the subcontract on NASA contract NAS9-1154

Final technical report on the Surface Electrical Properties Experiment Part 2

This report consists of a series of reports, reprints and preprints that in themselves constitute a self-explanatory record of the work performed by the University of Toronto on the Surface Electrical Properties Experiment. Areas discussed include: data handling and processing, installation and external signal application, operation of the equipment, and digital output. Detailed circuit descriptions are included. A complete unified discussion of the electromagnetic response of a plane stratified structure is reported. A detailed and comprehensive analysis of the theoretical parts of the electromagnetic is given. The numerical problem of computing numbers of the electromagnetic field strengths is discussed. It is shown that the analysis of the conductive media is not very far removed from the theoretical analysis and the numerical difficulties are not as acute as for the low-loss problem.Submitted to MIT in fulfillment of the subcontract on NASA contract NAS9-1154

Final technical report on the Surface Electrical Properties Experiment Part 1

This report consists of a series of reports, reprints and preprints that in themselves constitute a self-explanatory record of the work performed by the University of Toronto on the Surface Electrical Properties Experiment. Areas discussed include: data handling and processing, installation and external signal application, operation of the equipment, and digital output. Detailed circuit descriptions are included. A complete unified discussion of the electromagnetic response of a plane stratified structure is reported. A detailed and comprehensive analysis of the theoretical parts of the electromagnetic is given. The numerical problem of computing numbers of the electromagnetic field strengths is discussed. It is shown that the analysis of the conductive media is not very far removed from the theoretical analysis and the numerical difficulties are not as acute as for the low-loss problem.Submitted to MIT in fulfillment of the subcontract on NASA contract NAS9-1154

Surface electrical properties experiment, part 1

The work is reported which was performed on the Surface Electrical Properties Experiment Data Acquisition System. Areas discussed include: data handling and processing, installation and external signal application, operation of the equipment, and digital output. Detailed circuit descriptions are included

The resolution of a magnetic anomaly map expected from GRM data

Data from the MAGSAT mission were used to derive a global scalar magnetic anomaly map at an average altitude of about 400 km. It was possible to work with 2 data sets corresponding to dawn and dusk. The anomalies which were repeatable at dawn and at dusk was identified and the error limits of these anomalies were estimated. The repeatable anomalies were downward continued to about 10 km altitude. The anomalies over Canada were correlated quantitatively with bandpass filtered magnetic anomalies derived from aeromagnetic surveys. The close correlation indicates that the repeatable anomalies detected from orbit are due to geological causes. This correlation supports the geological significance of the global anomaly map