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- W2382396989 abstract "In order to study the Pre-Cenozoic tectonics of the northern South China Sea,we have calculated the RTP(Reduction To the Pole) anomaly,apparent magnetization and pseudo-gravity anomaly with the latest shipboard magnetic data in the north of the South China Sea(SCS).Then the density and magnetic susceptibility along three OBS profiles were determined.The result shows that high magnetic anomaly belt(HMAB) of Dongsha Uplift is the continuation of the volcanic belt in the coastal area of Zhejiang and Fujian provinces,and is dislocated by F10 fault trending NW which may be the old transformation boundary.F2 fault trending NW is the south boundary of the HMAB,and limits the north boundary of underplating.F3 fault is a weak zone before the crustal extension and thinning,and deep thermal state is different on its two sides, which may reveal the location of the Late Mesozoic subduction.The magnetization of magnetic layer reduces in the magnetic quiet zone between F2 fault and F3 fault.We ascribe the reducing magnetization to the hydrothermal alteration while high temperature mantle materials being underplated.However,in the south side of F3 fault,the magnetization increases and magnetic source blocks of the magnetic quiet zone are fragmented,the cause of weak positive magnetic anomalies on the surface is mainly due to the suppression between positive and negative magnetic anomalies under oblique magnetization.The unique characteristics of the magnetic layer in the area may indicate the existence of ancient oceanic crust." @default.
- W2382396989 created "2016-06-24" @default.
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- W2382396989 date "2011-01-01" @default.
- W2382396989 modified "2023-09-28" @default.
- W2382396989 title "The characteristics of magnetic anomalies:Implications for Pre-Cenozoic tectonics of the northern South China Sea" @default.
- W2382396989 hasPublicationYear "2011" @default.
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