Ben Sumpter.GeoGlossary
Research / Geoscience / Language

Obduction

Emplacement of oceanic lithosphere over another lithospheric body, commonly onto continental margins.

Language and route: Modern English geological construction with Latin ob- (toward/against/over) and ductio/ducere (leading), formed in contrast to subduction. Modern English geological construction with Latin ob- (toward/against/over) and ductio/ducere (leading), formed in contrast to subduction

Literal gloss: leading over / thrusting over

The name and its history

Plate-tectonic literature of late 1960s–1970s; individual first user unverified · in established use by early 1970s

What does the word literally mean?
Immediate linguistic pathway: Modern English geological construction with Latin ob- (toward/against/over) and ductio/ducere (leading), formed in contrast to subduction. Relevant original form: ob- + ductio (ob- + ductio); conventional gloss ‘leading over / thrusting over’. The linguistic gloss should not be mistaken for the original scientist’s stated motive unless directly demonstrated.
What did the original author mean?
Oceanic rocks recognised on continents demanded a mechanism different from ordinary consumption of oceanic lithosphere by subduction.
Why was the name needed?
To account for how dense ocean-floor and mantle rocks could be preserved high in mountain belts instead of descending into the mantle.
What evidence supported the original concept?
Ophiolite contacts, mapped thrust sheets, metamorphic soles and plate-scale reconstructions; early models disputed gravity sliding versus compressive transport.
How has geology changed the concept?
Modern mechanisms encompass collision, subduction initiation and complex emplacement; an ophiolite occurrence does not prescribe one obduction history.

Further historical context

Oceanic rocks recognised on continents demanded a mechanism different from ordinary consumption of oceanic lithosphere by subduction.

To account for how dense ocean-floor and mantle rocks could be preserved high in mountain belts instead of descending into the mantle.

Ophiolite contacts, mapped thrust sheets, metamorphic soles and plate-scale reconstructions; early models disputed gravity sliding versus compressive transport.

Modern mechanisms encompass collision, subduction initiation and complex emplacement; an ophiolite occurrence does not prescribe one obduction history.

Editorial qualification

Latin analysis gives lexical formation, not proven authorial coinage; original first-use page unresolved.

Related names

Ophiolite · Thrust fault · Nappe · Serpentinite

Sources

  1. Ophiolite obduction (1976), Tectonophysics — Geological mechanism controversies with citations to earlier obduction analyses
  2. Dewey & Bird (1970), Mountain belts and the new global tectonics — Contemporary plate-tectonic mountain-belt synthesis; not verified term coining
  3. Dewey & Bird (1971), Origin and emplacement of the ophiolite suite — Identified original 1971 plate-tectonic interpretation, abstract accessible; not first coining
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