An Elemental Analysis of the Glacial Deposits of the Vestfold Hills, Antarctica

Related publications

• Chapter 11: Antarctica at the Last Glacial Maximum, Deglaciation and the Holocene Antarctic Climate Evolution. Developments in Earth & Environmental Science, 2008 (Ref: 13917)
  Authors:

  Wright A.P.White D.Gore D.B.Siegert M.J.
  Category 1: Peer-reviewed literature

  : Recent technological advances in the study and dating of both land and marine glacial geologic features combined with improvements in both glaciological and post-glacial isostatic rebound modelling have led to significant improvements in our knowledge and understanding of the Antarctic Ice Sheets…

• An atlas of surficial salts of the Vestfold Hills, East Antarctica: composition, distribution and origin ANARE Report, 2000 (Ref: 9479)
  Authors:

  Gore D.B.Nichols G.T.Lehmann C.E.R.Burgess J.S.Baird A.S.&Creagh D.C.
  Category 1: Peer-reviewed literature

  A regional chemical boundary termed the ‘salt line ’,in the Vestfold Hills of East Antarctica, was investigated using X-ray diffraction and electron probe analyses of surficial salts, and conductivity of surficial sediments. West of the salt line, halite and thenardite are abundant.

• Fossils in Till at Vestfold and Bunger Hills -Contrasts in Distribution and Abundance , 2001 (Ref: 9916)
  Authors:

  Lehmann C.E.R.Gore D.B.Bell K.
  Category 3: Abstract
• Geomorphological Processes and Quaternary Sediments of the Vestfold Hills, East Antarctica, 1995 (Ref: 7347)
  Authors:

  Gore D.B.
  Category 3: Thesis, higher degree
• Regional contrasts in weathering and glacial sediments suggests long term subaerial exposure of the Vestfold Hills, East Antarctica The Antarctic Region: geological evolution and processes, 1997 (Ref: 8904)
  Authors:

  Gore D.B.&Colhoun E.A.
  Category 1: Peer-reviewed literature

  Vestfold Hills, East Antarctica exhibits marked contrasts in the weathering surface, glacial sediments and terrain between its eastern and western parts. The boundary between these zones coincides with a regional chemical boundary termed the salt line.