How much time is needed for plate tectonics to subdue everything?

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SUMMARY

The discussion centers on the longevity of fossil records in relation to plate tectonics, specifically addressing the misconception that all Earth crust is subducted within 500 million years. It is established that approximately 95% of subduction involves oceanic crust, with limited continental crust subduction occurring primarily in regions like the Indian subcontinent. The conversation highlights that the process of subduction is statistical, meaning some materials are subducted earlier while others remain for much longer periods, contributing to the presence of fossils dating back 3.8 billion years.

PREREQUISITES
  • Understanding of plate tectonics and subduction processes
  • Knowledge of oceanic versus continental crust characteristics
  • Familiarity with geological time scales and fossilization
  • Awareness of tectonic collision zones, particularly in the context of the Indian subcontinent
NEXT STEPS
  • Research the mechanisms of oceanic crust subduction and its efficiency
  • Explore geological studies on the age of the oldest oceanic crust
  • Investigate the statistical nature of tectonic processes and material turnover
  • Examine case studies of continental crust interactions, especially in collision zones
USEFUL FOR

Geologists, Earth scientists, and students interested in plate tectonics, fossil records, and the dynamics of Earth's crust will benefit from this discussion.

Marco Masi
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I read of fossile records as old as 3.8 billion years. How can this be? Since I thought that it takes about 500 mio. years for plate tectonics to force all the Earth crust into the subduction zones into the mantle. No evidence should be left. I'm confused...
 
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You really think tectonic activity is 100% efficient?
 
Marco Masi said:
I read of fossile records as old as 3.8 billion years. How can this be? Since I thought that it takes about 500 mio. years for plate tectonics to force all the Earth crust into the subduction zones into the mantle. No evidence should be left. I'm confused...

you are coming from a mistaken understanding.
~ 95% of subduction is oceanic crust NOT continental crust

There are very few places around the world where continental crust is being subducted or anything similar to that. One of those places is the Indian sub-continent as it pushes into the Euro-Asian continent.
There is a mixture of subduction and just straight out collision.Dave
 
Even if the mean turnover time were of the order of 500 Ma, this is to a large extent a statistical process. I.e. there is lot of material which is subduced earlier and some material which is not subduced at all.
 

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