地洼学说的发展与未来

THE DEVELOPMENT AND FUTURE OF DIWA THEORY

Following the Geosyacline Area and the Platform Area, a new geotectonic unit, Diwa Area and its studies, Diwa Theory, was developed in 1956 by Chert Guoda. From the research that followed, branch theories were subsequently proposed, such as "Progression law with transformation between mobile and stable regions of the earth's crust", "Theory of Diwa (progressive) ore formation", "Concept of tectonic system", "Concept of crustobody", "Hypothesis of mantle creep-flow and geothermal energy coacervation-diffusion alternation ", "Metallogenic tectonics'and "Tectonogeochemistry". So a rather complete theoretical system on geotectonics and metallogenesis has been composed. On the basis of a scientific synthesis of these branches and the inclusion of the advantages of "Geosyncline Theory", "Plate-tectonics" and "Geomechanics". Prof. Chert has recently worked out an open developing program whose principal content is "Historistic-Causationist Geotectonics" . Thus the research on Diwa Theory has been pushed to a much higher theoretical state.