Obduction occurs at convergent plate boundaries in which one plate remains at a constant level and the other plate is forced up over that plate.
Obduction refers to the process in plate tectonics where one tectonic plate is forced over the edge of another, usually due to a collision. This often leads to the uplifting and emplacement of rocks from the lower plate onto the upper plate.
The process by which a tectonic plate consisting of less heavy rock rides up over a heavier plate is known as subduction. The opposite of this process is called obduction.
The process you are referring to is known as subduction, where a heavier tectonic plate sinks beneath a less dense plate due to differences in density and composition. This process often leads to the formation of deep ocean trenches and volcanic arcs.
When continental and oceanic lithospheres collide, the denser oceanic plate is usually subducted beneath the less dense continental plate due to the difference in density. This can lead to the formation of volcanic arcs on the overriding continental plate and deep-sea trenches where the oceanic plate is subducted. The collision can also result in mountain building and the formation of complex geological structures.
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Post-mortem examination, necropsy, autopsia cadaverum or obduction.
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An autopsy, also known as a post-mortem examination, necropsy, or obduction, is a medical procedure that consists of a thorough examination of a corpse to determine the cause and manner of death and to evaluate any disease or injury that may be present.
The process by which a tectonic plate consisting of less heavy rock rides up over a heavier plate is known as subduction. The opposite of this process is called obduction.
The process you are referring to is known as subduction, where a heavier tectonic plate sinks beneath a less dense plate due to differences in density and composition. This process often leads to the formation of deep ocean trenches and volcanic arcs.
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Subduction (where one plate is forced beneath another less dense plate - may occur at oceanic-oceanic and oceanic-continental boundaries), obduction (where oceanic plate is forced over a continental plate) and orogenesis where two continental plates collide and mountains are formed (e.g. the Himalayas).
When continental and oceanic lithospheres collide, the denser oceanic plate is usually subducted beneath the less dense continental plate due to the difference in density. This can lead to the formation of volcanic arcs on the overriding continental plate and deep-sea trenches where the oceanic plate is subducted. The collision can also result in mountain building and the formation of complex geological structures.
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Mean is the average.
Mean