Rhythmic layering and multiple intrusion in the Ferrar Dolerite of South Victoria Land, Antarctica
- 1 September 1971
- journal article
- other
- Published by Taylor & Francis in New Zealand Journal of Geology and Geophysics
- Vol. 14 (3) , 600-604
- https://doi.org/10.1080/00288306.1971.10421950
Abstract
The Ferrar Dolerite was studied in the northern part of the Boomerang Range, the Warren Range and at Mount Metschel in the Skelton Neve (Fig. 1) as part of the programme of the 1970-71 Victoria University Antarctic Expedition.Keywords
This publication has 3 references indexed in Scilit:
- ‘Mat’ Formation and Crystal Settling in MagmaNature, 1964
- Differentiation in Ferrar dolerites, AntarcticaNew Zealand Journal of Geology and Geophysics, 1962
- Form of diabase sheets in southeastern PennsylvaniaAmerican Journal of Science, 1952