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