ON INTEGRATIVE GEOTECTONICSChen Guoda(Changsha Institute of Geotectonics, Academia Sinica, 410003,Hunan, China)Xiang Jixi (The Chinese Academy of Geological Sciences, Beijing, China)integrative geotectonics, crustobod...ON INTEGRATIVE GEOTECTONICSChen Guoda(Changsha Institute of Geotectonics, Academia Sinica, 410003,Hunan, China)Xiang Jixi (The Chinese Academy of Geological Sciences, Beijing, China)integrative geotectonics, crustobody geotectonics,multi-origined and polygenetic compound resultantforce system, tectosphere, gradual change, mutation, catastrophismBased on historistic-causationist geotectonics proposed by Chen Guoda in1992, the authors attempt to further extend its contents and ranges, establish integrative geo-tectonics with wide ranges and higher synthesis. Integrative geotectonics is defined as a disci-pline to study very synthetically the whole history and causationistic relations of formation and evolution of the global tectonics (including the crustal and deep teetospheric structures) with the comprehensive analysis method. It is also called as "crustobody geotectonics" for its main geotectonic element is crustobody. Its characteristics are: (1) regarding the internal and exter-nal展开更多
The crustobody is a concept of tectonic element established for integrating the research airns, objects and methods of historic and dynamic geotectonics in order to study the tectonics of the earth in an all-round way...The crustobody is a concept of tectonic element established for integrating the research airns, objects and methods of historic and dynamic geotectonics in order to study the tectonics of the earth in an all-round way. It caTries the implications of both evolution and rnovernent, lying equal stress on both development viewpoint and connection viewpoint and giving consideration to both tirne and space. It has the nature, characteristics and functions of the above-mentioned two tectonic elements. On the one hand, though consisting of historic tectonic elernents such as geosynclinal, platform and geodepression (diwa) regions, it puts emphasis on their changing state in spatial rnigration, thus differing from them. On the other hand,though sirnilar in form to plate, a dynamic tectonic element, it places eruphasis on the changing state in its temporal evolution and has other distinguishing characteristics, thus differing from it.展开更多
Geosyncline-platform geotectonics is aimed at the reconstruction of the Earth’s tectonic evo-lution history, and belongs to the category of historic geotectonics. Plate tectonics exp1ores pri-marily the motion of lit...Geosyncline-platform geotectonics is aimed at the reconstruction of the Earth’s tectonic evo-lution history, and belongs to the category of historic geotectonics. Plate tectonics exp1ores pri-marily the motion of lithospheric blocks and belongs to the category of dynamic geotectoncis. Eachof them has its own advantages and strong points. However, both are difficult to meet the require-ments for an overall research on all-round tectonic problems- In order to make use of each one’sadvantages more effectively, an integrative, new type geotectonics called crustobody geotectonicsis here proposed. It is a branch of geotectonics which deals integratively with both evolution andmovement of the Earth’s crust by means of the concept of crustobody and the historic-dghamic in-tegrative analysis method.展开更多
文摘ON INTEGRATIVE GEOTECTONICSChen Guoda(Changsha Institute of Geotectonics, Academia Sinica, 410003,Hunan, China)Xiang Jixi (The Chinese Academy of Geological Sciences, Beijing, China)integrative geotectonics, crustobody geotectonics,multi-origined and polygenetic compound resultantforce system, tectosphere, gradual change, mutation, catastrophismBased on historistic-causationist geotectonics proposed by Chen Guoda in1992, the authors attempt to further extend its contents and ranges, establish integrative geo-tectonics with wide ranges and higher synthesis. Integrative geotectonics is defined as a disci-pline to study very synthetically the whole history and causationistic relations of formation and evolution of the global tectonics (including the crustal and deep teetospheric structures) with the comprehensive analysis method. It is also called as "crustobody geotectonics" for its main geotectonic element is crustobody. Its characteristics are: (1) regarding the internal and exter-nal
文摘The crustobody is a concept of tectonic element established for integrating the research airns, objects and methods of historic and dynamic geotectonics in order to study the tectonics of the earth in an all-round way. It caTries the implications of both evolution and rnovernent, lying equal stress on both development viewpoint and connection viewpoint and giving consideration to both tirne and space. It has the nature, characteristics and functions of the above-mentioned two tectonic elements. On the one hand, though consisting of historic tectonic elernents such as geosynclinal, platform and geodepression (diwa) regions, it puts emphasis on their changing state in spatial rnigration, thus differing from them. On the other hand,though sirnilar in form to plate, a dynamic tectonic element, it places eruphasis on the changing state in its temporal evolution and has other distinguishing characteristics, thus differing from it.
文摘Geosyncline-platform geotectonics is aimed at the reconstruction of the Earth’s tectonic evo-lution history, and belongs to the category of historic geotectonics. Plate tectonics exp1ores pri-marily the motion of lithospheric blocks and belongs to the category of dynamic geotectoncis. Eachof them has its own advantages and strong points. However, both are difficult to meet the require-ments for an overall research on all-round tectonic problems- In order to make use of each one’sadvantages more effectively, an integrative, new type geotectonics called crustobody geotectonicsis here proposed. It is a branch of geotectonics which deals integratively with both evolution andmovement of the Earth’s crust by means of the concept of crustobody and the historic-dghamic in-tegrative analysis method.
