The intrusive magmatism of the Ross Orogeny, Victoria Land, Antarctica
Entry ID: rocchi_magmatism_ross_orogeny

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Summary
Abstract: The Transantarctic Mountains are the uplifted roots of the Ross-Delamerian orogen, that was active on the East Antarctic-Australia craton margin during Cambrian-Ordovician time. Magmas of mantle, crustal and hybrid origin extensively intruded the Antarctic sector of the orogen, that results segmented in crustal sectors, by major discontinuities. The field work on intrusive rocks includes ... View entire text
Related URL
Description: Italian National Antarctic Museum web site
Geographic Coverage
Spatial coordinates   
  N: -67.2   S: -74.67   E: 172.97   W: 149.21

Temporal Coverage
Start Date: 1985-01-01
Stop Date: 2005-12-31
ISO Topic Category
Data Set Progress
IN WORK
Originating Center
Data Center
Dipartimento di Science Della Terra, Universita di Pisa, Italy Supplemental Info
Data Center URL: http://www.dst.unipi.it/

Data Center Personnel
Name: SERGIO ROCCHI
Phone: +39 050 2215710
Fax: +39 050 2215800
Email: rocchi at dst.unipi.it
Contact Address:
Via S. Maria 53
City: Pisa
Postal Code: 56126
Country: Italy
Personnel
Role: INVESTIGATOR
Phone: +39 050 2215710
Fax: +39 050 2215800
Email: rocchi at dst.unipi.it
Contact Address:
Via S. Maria 53
City: Pisa
Postal Code: 56126
Country: Italy
Creation and Review Dates
DIF Creation Date: 2008-04-21
Last DIF Revision Date: 2008-04-24
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