青云翻译

Mak Weng River ce relatively obvious negative anomaly, slightly larger than the value of lakes and rivers in δce, weakly positive anomaly. Ce in the weathering profile in Guizhou rock - soil transition zone of strong negative anomalies, while the upper layer is the basic performance of the positive

Maiwenghe Ce negative relatively obvious, δ Ce value slightly larger than the rivers in the Lake, is weak is the exception. Ce in the weathering profile in Central Guizhou in transitional zone of rock-soil is strongly negative, while the upper soil layer is manifested as exception (few normal range)

Mai Wenghe the Ce negative anomaly is relatively obvious, in the lake δCe the value is bigger than the rivers slightly, assumes weakly exceptionally.In Guizhou Province makes decent in the section plane Ce in the crag - earth intermediate belt for the intense negative anomaly, but upside soil layer

Mak River Ce negative abnormal functioning relatively obvious, lakes, rivers, slightly more than a weak Ce value is unusual. Gom weathered Ce profiles in the rock - the transition zone for strong negative anomalies, and upper layer is essentially are unusual (a few tricks, and therefore a few normal

Maiwenghe Ce negative relatively obvious, δ Ce value slightly larger than the rivers in the Lake, is weak is the exception. Ce in the weathering profile in Central Guizhou in transitional zone of rock-soil is strongly negative, while the upper soil layer is manifested as exception (few normal range)