Uplift and denudation in the continental area of China linked to climatic effects: evidence from apatite and zircon fission track data
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Research suggests that uplift and denudation in the continental area of China may be linked to climatic effects, with evidence from apatite and zircon fission track data. The dynamics of the North China craton and the formation of various landforms in China are being studied, with some research focusing on the role of tectonic activity and glaciations. The relationship between climatic effects and geological processes in China is a complex one, with multiple factors and regions being investigated.
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