Burial metamorphism is likely to occur in sedimentary basins where sediments accumulate to significant depths, typically several kilometers. As sediments are buried, increased pressure and temperature conditions transform the original sedimentary rocks into metamorphic rocks. This process is common in regions with thick sedimentary layers, such as continental margins and rift valleys. Additionally, burial metamorphism can be associated with tectonic settings where subsidence and sedimentation rates are high.
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