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《Geoscience》 1991-03
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Lou Hai Yu Qinfan(China University of Geosciences, Beijing)  
quantitative correlation analysis is one of the integral interpretation methods of gravity and magnetic anomalies. Based on Poisson's theorem, a moving - window linear regression analysis is preformed between suitable derivatives of anomalous potential fields. Then, areas with different pat-terns of anomaly correlation can be distinguished between each other, and useful information about terrane boundary and crust structure can be derived. From the results of this method, we gain some new idea about the crust structure on the geoscience transect from Yadong to Golmud, Qinghai-Ti-bet plateau.
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