10.1029-2018JE005826Figure211460011.pptx
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The postimpact KREEP material distribution. For our model, the global KREEP material was initially resided at the bottom of crust with a thickness of 20 km. The giant impact excavated the crustal, KREEP, and mantle material. The ejected KREEP material, deposited close to the basin rim, slumped back into the basin and was emplaced below crust. Point a and b represent the boundaries of transient crater (~1,800 km) and final crater (~2,700 km) from the impact site. See Figure 6 for the boundaries of transient crater and final crater on the global crustal thickness map.
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TRR170-DB
创建时间：
2022-06-02
