Education Concept of Earths Expansion: Main Grounds, Space-Geodetic and Paleomagnetic Evidence, Metallogenic Consequences

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Education Concept of Earths Expansion: Main Grounds, Space-Geodetic and Paleomagnetic Evidence, Metallogenic Consequences
Author Yury V Chudinov
Published 1999
Publisher Brill Academic Publishers
Pages 166
ISBN 9067642991

PART 1: EDUCTION CONCEPT OF EARTH'S EXPANSION
EARTH'S EXPANSION
Spreading in mid-oceanic ridges as evidence for Earth's expansion
Reconstructions of former position of continents
Eduction instead of subduction
Objections against Earth's expansion
EVIDENCES FOR EDUCTION FROM GEOLOGY AND GEOPHYSICS
Deep-sea drilling results
Seismofocal zones and eduction
Tectonic nature of seismofocal zones
Structure of seismofocal zones as provided by seismological data
Explanation of seismological data according to the subduction and eduction viewpoints
Main geological phenomena at the continent-ocean margins from eduction and subduction points of view
DEVELOPMENT OF THE EARTH ACCORDING TO EDUCTION CONCEPT OF ITS EXPANSION
Preliminary tectonic comments
The causes of folding
Three types of the Earth's lithosphere

PART 2: GEODETIC AND PALEOMAGNETIC EVIDENCES OF THE EARTH'S EXPANSION
INTRODUCTION
A. DETERMINATION OF THE ANCIENT EARTH'S SIZE BY PALEOMAGNETIC DATA
POSSIBILITIES OF PALEOMAGNETIC DETERMINATIONS
Materials
Geological limits in application of paleomagnetic methods of determination of the ancient Earth's size
METHODS FOR DETERMINING THE ANCIENT EARTH'S RADII SUGGESTED BEFORE 1968
The Egyed method
Cox and Doell determinations
The Bilinski method
Khramov et al. determinations
Methods of spherical triangles
The method of comparing intersections of paleomeridians and position of virtual van Hilten's poles
J. Hospers and S.C. van Andel determinations
The Ward statistic method
PALEOMAGNETIC DATA ON EARTH EXPANSION
The result view
The Chudinov-Tertitski method and its results
Possibilities of determining the Earth size changing by paleomagnetic data
B. DATA OF THE SPACE GEODESY
SPACE GEODESY AND PLATE TECTONICS
Methods of obtaining data and principles of their processing
The plate model content
The plate model for space geodesy
Space geodesy for the plate model
DEPENDENCY OF CORRELATION BETWEEN PREDICTED AND ESTIMATED VALUES IN SPACE GEODETIC CALCULATIONS ON RANDOM CONDITIONS. VELOCITY VECTORS OF PLATE'S MOTION
Data of space geodetic calculations in literature
Dependency of connections between predicted and estimated velocity vectors of stations on direction of predicted displacement
Graphics of the correlation of absolute values of predicted by the plate tectonics and conceived estimated vectors
VECTORS OF PLATE DISPLACEMENTS COMPARED WITH THE GEOLOGICAL DATA
Areas of active join of continents and oceans
Plate velocity vectors in some regions
MEASUREMENTS OF DISTANCES BETWEEN STATIONS AS EVIDENCES OF EARTH'S EXPANSION
Influence of the neglected Earth expansion on the results of cosmogeodetic calculations
Determination of distances between stations
Changes of distances between stations, predicted on the basis of the plate tectonics and conceived estimated, compared with consequences from the eduction model of the Earth expansion
The plate model and great circles of the Earth sphere
Minimum values of possible expansion of the Earth
Estimation of neglected Earth's expansion from changes of distances between stations
Geometrical estimation of the error of neglected expansion of the Earth
Comparison of indirect estimations of the Earth's expansion velocity by space geodetic data with estimations obtained by other methods
CONCLUSION

PART 3: ABOVE-SEISMOFOCAL ORE ZONATION AS A CONSEQUENCE OF EDUCTION
RECONSTRUCTION OF ORE-BEARING ABOVE-SEISMOFOCAL ZONES AND THEIR INNER ARRANGEMENT
Reconstruction of location of ancient seismofocal zones
Above-paleoseismofocal ore zones within ore belts
Succession of above-seismofocal ore zones within ore belts
ORIGIN OF ORE-BEARING ZONES
Changes in character of ore compounds in ore zones
Boiling points of ore compounds
The fabric of ore formation due to eduction
Eduction verus subduction
CONCLUSION

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