Seismic tomography and mantle circulation - Models of mantle convection: one or several layers
Seismic tomography and mantle circulation - Models of mantle convection: one or several layers
About this item
Full title
Author / Creator
Publisher
London: The Royal Society
Journal title
Language
English
Formats
Publication information
Publisher
London: The Royal Society
More information
Scope and Contents
Contents
Numerical model calculations are used to determine if convection in the Earth’s mantle could be organized in two or more layers with only limited mass exchange in between. The seismic discontinuity at 670 km depth and the top of the D"-layer at the bottom of the mantle are considered as candidates for internal boundaries. If the 670 km discontinuit...
Alternative Titles
Full title
Seismic tomography and mantle circulation - Models of mantle convection: one or several layers
Authors, Artists and Contributors
Author / Creator
Identifiers
Primary Identifiers
Record Identifier
TN_cdi_istex_primary_ark_67375_V84_K8P10KN7_D
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_istex_primary_ark_67375_V84_K8P10KN7_D
Other Identifiers
ISSN
0080-4614
E-ISSN
2054-0272
DOI
10.1098/rsta.1989.0045
