Do we have any ways to drill through oceanic crust?

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Discussion Overview

The discussion centers around the feasibility and methods of drilling through the oceanic crust to enhance understanding of its composition and structure. Participants explore various techniques and the limitations of current technology in reaching significant depths beneath the ocean floor.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested

Main Points Raised

  • Some participants suggest that understanding the oceanic crust is important, but current technology may not be sufficient to drill through its full thickness, which is generally around 10 km.
  • Others propose that drilling the first few layers could provide valuable insights, despite the challenges involved.
  • One participant mentions that natural earthquakes and seismic surveying are primary methods for studying the first few kilometers of the crust, noting that these methods can indicate layer thickness and velocity factors.
  • There is a correction regarding the average thickness of oceanic crust, clarifying that it is about 10 km, contrary to earlier claims about it being tens of miles thick.
  • Participants discuss the greatest depths achieved in drilling, with one noting that the deepest drilled well is often misrepresented due to differences between measured and true vertical depths.
  • A suggestion is made to consider geological features like the Mid-Atlantic rift in Iceland as a natural exposure of crustal processes, although this is acknowledged as a limited perspective.
  • There is mention of a planned drilling project off Costa Rica aimed at retrieving gabbro from a depth of around 2 km.

Areas of Agreement / Disagreement

Participants express differing views on the capabilities of current drilling technology and the significance of various drilling depths. There is no consensus on the best methods or the implications of the drilling depths discussed.

Contextual Notes

Participants highlight limitations in current drilling technology and the complexities involved in interpreting seismic data. There are also unresolved questions regarding the accuracy of depth measurements in drilling reports.

Simfish
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So that we could understand it?
 
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If I understand it correctly, the crust is tens of miles thick. We have no technology that even comes close to being able to drill that far.
 
Well, how about just the first few layers just so that we can know about it better?
 
Using natural earthquakes and the use of seismic surveying are the 2 major ways of determining layers for the first ~ 5 km of crust.
Tho it doesn't specifically tell you what those layers are made of it does tell you about the thickness of each layer, depth below surface and velocity factor of each layer ( from which you can make educated guesses of the type of rock the different layers are)

When i was doing my BSc in geology at Uni, part of the course was learning to interpret seismic surveys

just a little correction... phinds commented on the crust being 10's of miles thick, whilst this is correct for the thickest parts of continental crust, it isn't for oceanic crust which avg's ~ 10km (6 miles) thick. Which is what you originally asked about.

cheers
Dave
 
Last edited:
Wikipedia came up with some interesting facts.

the greatest depth drilled so far is ~ 12,289m 12km ... 7.5 miles ! awesome
there appeares to be a number of drill sites around the world that have got between 5 and 12 km

cheers
Dave
 
davenn said:
the greatest depth drilled so far is ~ 12,289m 12km ... 7.5 miles ! awesome
That is somewhat misleading. I believe you are quoting the figures for a Qatar well that reached total depth in 2008. This is an extended reach well, so that the true vertical depth (TVD) is considerably less than the measured depth (MD) - the depth quoted. The horizontal portion of the well is around 10km, so TVD will be not much more than 1km.

The only slightly shorter (12,262 m MD) Kola well remains - to my knowledge - the deepest TVD achieved to date.
 
davenn said:
just a little correction... phinds commented on the crust being 10's of miles thick, whilst this is correct for the thickest parts of continental crust, it isn't for oceanic crust which avg's ~ 10km (6 miles) thick. Which is what you originally asked about.

Thank you for that correction. I did not realize there was such a significant variation.
 
You could just walk around on Iceland, where the Mid-Atlantic rift is on the surface !

Okay, sorry, that's a bit facetious, because you won't get the complex chemical changes due saline hydrothermal circulation etc etc...

IIRC, there's a drill-ship hoping to retrieve gabbro from ~2km depth off Costa Rica this Summer. Borek's post's search parameters have it in the top ten Google hits...
 
  • #10
Ophiolite said:
That is somewhat misleading. I believe you are quoting the figures for a Qatar well that reached total depth in 2008. This is an extended reach well, so that the true vertical depth (TVD) is considerably less than the measured depth (MD) - the depth quoted. The horizontal portion of the well is around 10km, so TVD will be not much more than 1km.

The only slightly shorter (12,262 m MD) Kola well remains - to my knowledge - the deepest TVD achieved to date.

NO, I was quoting the Kola ! :) give or take a few metres, Not familiar with the Qatar one

Dave
 

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