An integration to optimally constrain the thermal structure of oceanic lithosphere

[1] The evolution through time of the oceanic lithosphere is a substantial, incompletely resolved geodynamical problem. Consensus remains elusive regarding its thermal structure, physical properties, and the best model through which to unify observational constraints. We robustly reevaluate all thre...

Full description

Saved in:
Bibliographic Details
Main Authors: Bruno Goutorbe, John Hillier
Format: Default Article
Published: 2013
Subjects:
Other earth sciences not elsewhere classified
Oceanic lithosphere
Thermal models
Seismic tomography
Heat flow
Age-depth curves
Earth Sciences not elsewhere classified
Online Access:https://hdl.handle.net/2134/15395
Tags: Add Tag
No Tags, Be the first to tag this record!

Similar Items