Thesis icon

Thesis

The evolution of Late Quaternary alluvial landscapes in northern Oman

Abstract:

Dryland fans predominately preserve signals of Late Quaternary (350-0 ka) climatic variability within their stratigraphy because of hydrological changes in their feeding catchments. Their morpho-dynamics are also the product of various other non-climatic controls, such as catchment morphology, geology and depositional setting. The mountain front fans of the Hajar Mountains, south-east Arabia, have been shown to aggrade under more sustained streamflow during periods of insolation maxima whi...

Expand abstract

Actions


Access Document


Files:

Authors


More by this author
Institution:
University of Oxford
Division:
SSD
Department:
SOGE
Sub department:
Geography
Research group:
Oxford Luminescence Dating Laboratory
Oxford college:
St Cross College
Role:
Author
ORCID:
https://orcid.org/0000-0002-1411-8486

Contributors

Institution:
University of Oxford
Division:
SSD
Department:
SOGE
Sub department:
Geography
Role:
Supervisor
ORCID:
0000-0001-6867-5504
Institution:
Oxford Brookes University
Role:
Supervisor
Institution:
University of Oxford
Division:
SSD
Department:
SOGE
Sub department:
Geography
Research group:
Oxford Luminescence Dating Laboratory
Role:
Supervisor
Institution:
University of Oxford
Division:
SSD
Department:
SOGE
Sub department:
Geography
Research group:
Oxford Luminescence Dating Laboratory
Role:
Supervisor
ORCID:
0000-0003-1043-0998


More from this funder
Funder identifier:
https://ror.org/0439y7842
Grant:
EP/L016036/1
Programme:
Science and Engineering in Arts, Heritage and Archaeology Centre for Doctoral Training (SEAHA CDT)


DOI:
Type of award:
DPhil
Level of award:
Doctoral
Awarding institution:
University of Oxford

Terms of use



Views and Downloads






If you are the owner of this record, you can report an update to it here: Report update to this record

TO TOP