Skip to Main Content
Book Chapter

Tectonic, Volcanic, and Hydrological Controls on Rift Sedimentation

By
Published:
January 01, 2002

Abstract

In this synthesis of current models for the initiation and evolution of continental rift zones, we discuss how the thermo-mechanical properties of the continental lithosphere produce topographic relief and control rift architecture. Our aim is to identify the key processes and parameters controlling the geometry and kinematics of continental rift basins, thereby providing a theoretical framework for fault arrays within rift basins. Case studies of the East African and Baikal rifts are used to illustrate rifting processes and the importance of lithospheric rheology in determining basin form.

On the basis of theory and observations, we suggest a rift classification scheme based on the lithospheric strength at the rime of rifting. At the length scale of individual rift basins, lithospheric rheology also plays an important role. Lengths of border faults in cratonic parts of the East African and Baikal rifts are 80-120 km, whereas border faults that form in younger lithosphere or collapsing orogens are on the order of 30-60 km, indicating that the dimensions of rift basins are also controlled by the mechanical properties of the lithosphere. Variations in lithospheric thickness between continental domains probably have corresponding variations in thickness of the mechanical lithosphere. Once created, these lateral variations in rheology clearly will concentrate stress along terrane boundaries, suggesting that terrane boundaries are susceptible to later tectonic episodes. These results indicate that we can develop predictive models of the regional morphology and along-axis segmentation of active and ancient rift basins based on a relatively small data base: short, narrow basins with narrow uplifted flanks will form in young, hot, weak, lithosphere and be characterized by < 15 km seismogenic layer thickness/effective elastic thickness; long, wide, deep basins with broad uplifted flanks will develop in old, cold, strong continental lithosphere with seismogenic layer thickness/effective elastic thickness a 30 km.

You do not currently have access to this article.
Don't already have an account? Register

Figures & Tables

Contents

SEPM Special Publication

Sedimentation in Continental Rifts

Robin W. Renaut
Robin W. Renaut
Department of Geological Sciences, University of Saskatchewan, Saskatoon, Saskatchewan S7N 5E2, Canada
Search for other works by this author on:
Gail M. Ashley
Gail M. Ashley
Department of Geological Sciences, Rutgers University, Piscataway, New Jersey 08854-8066, U.S.A.
Search for other works by this author on:
SEPM Society for Sedimentary Geology
Volume
73
ISBN electronic:
9781565761957
Publication date:
January 01, 2002

GeoRef

References

Related

A comprehensive resource of eBooks for researchers in the Earth Sciences

Close Modal
This Feature Is Available To Subscribers Only

Sign In or Create an Account

Close Modal
Close Modal