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- W2368097968 abstract "The transfer structure knots along the middle-lower Yangtze River reaches are the focal points where the Tethys tectonic mechanism meets,links up and transforms with the Pacific tectonic mechanism,substantially including the Dabie Orogen,Tan-Lu Fault and Middle-lower Yangtze metallogenic belts,referred to as three major well-known tectonic units,which are typical of deep-seated process and surface response of eastern China mid-Cenozoic continental dynamics.It will greatly favour new breakthrough in continental dynamic theory and guide deep-seated ore prospecting in second metallogenic space to combine continental orogen,large faults and mining camp,aim at intra-plate deformation,kinetics and dynamics,build up systematic research frame for continental dynamics in the area,study the delicate transformation process between two major tectonic mechanisms,and analyze the deep process and shallow effect of intra-continental tectonic evolution and dynamics.." @default.
- W2368097968 created "2016-06-24" @default.
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- W2368097968 date "2010-01-01" @default.
- W2368097968 modified "2023-09-28" @default.
- W2368097968 title "FEATURES, ATTRIBUTES AND RESEARCH IMPLICATIONS OF TRANSFER STRUCTURE KNOTS ALONG THE MIDDLE-LOWER YANGTZE RIVER REACHES" @default.
- W2368097968 hasPublicationYear "2010" @default.
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