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《Chinese Journal of Geophysics》 1994-03
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WANG MAO-JI Aero-geophysical and Remote Sensing Center, Beijing 100083)  
The aim of this paper is to discuss the gravity and magnetic interpretation of Heishui-Quanzhou Geoscience Transect of South China.In addition to the conventional 2.5D gravity and magnectic inversion method, the isodensity line algorithm for constructing gradient-layer density model was adopted so as to resolve the details of crustal density, and calculate the free surface of mantle for analysing lateral heterogeneities of the upper mantle density. Modelling of geopotential field anomalies reveals the upper crustal structures within the depth of 10km and the distribution of upper mantle density. The upper mantle of South China Orogenic Belt is characterized by low density related to the reconstruction of the upper mantle, while that of the Sichuan Basin by higher density being the primitive mantle, and the boundary between Yantze Craton and South China Orogenic Belt coincides with the boundary of upper mantle density.The combined analysis of Bouger gravity anomaly, surface rock density and topography data enabled us to distinguish the zones of density inversion connected with the deep criteria of endogenic mineralization as the most prospective regions for further investigations deposits.
【CateGory Index】: P631.24
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