Cambro-Ordovician orogenic magmatism in Northern Victoria Land
Entry ID: ghezzo_cambro_ordovician_magmatism

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Summary
Abstract: The Transantarctic Mountains expose the uplifted roots of the Ross- Delamerian orogenic system, that was active on the East Antarctic- Australia craton margin during Cambrian-Ordovician time. Granitoid magmas extensively intruded the Antarctic sector of the orogen , that results segmented in crustal sectors, structurally, chronologically and geochemically diverse.
Several studies carried out on ... View entire text
Related URL
Description: Italian National Antarctic Museum web site
Geographic Coverage
Spatial coordinates   
  N: -74.7   S: -74.7   E: 164.1   W: 164.1
Min Altitude: 0 Max Altitude: 3500

Temporal Coverage
Start Date: 1985-01-01
Stop Date: 2005-05-31
ISO Topic Category
Data Set Progress
IN WORK
Data Center
Dipartimento di Scienze Della Terra, Universita Degli Studi di Siena, Italy Supplemental Info
Data Center URL: http://www.dst.unisi.it/

Data Center Personnel
Name: CLAUDIO GHEZZO
Phone: +39 577233928
Fax: +39 577233938
Email: Ghezzo at unisi.it
Contact Address:
via Laterina 8
City: Siena
Postal Code: 53100
Country: Italy
Distribution
Distribution Media: Scientific publications
Personnel
Role: INVESTIGATOR
Phone: +39 577233928
Fax: +39 577233938
Email: Ghezzo at unisi.it
Contact Address:
via Laterina 8
City: Siena
Postal Code: 53100
Country: Italy
Publications/References
- ROCCHI S. , G. DI VINCENZO, C. GHEZZO (2004) - 'The Terra Nova Intrusive Complex (Victoria Land)' - Terra Antartica Reports, Vol.10, 1 – 49.
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Creation and Review Dates
DIF Creation Date: 2008-04-21
Last DIF Revision Date: 2008-04-24
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