IODP Proceedings    Volume contents     Search
iodp logo

doi:10.2204/iodp.proc.304305.201.2009

Data report: an electron backscatter diffraction study of a gabbroic shear zone, IODP Expedition 304/3051

Angela Halfpenny2, 3 and David Prior2

Abstract

Integrated Ocean Drilling Program Expedition 304/305 was designed to investigate the formation and evolution of oceanic core complexes by drilling through the Atlantis Massif oceanic core complex. Characterization of shear zone microstructures from the Atlantis Massif provides information about the area’s deformation history and insight into the formation of oceanic core complexes. Plastic deformation was recognized in only 3% of the recovered core volume. The majority of the shear zones are located in gabbroic lithologies. Using orientation contrast imaging and electron backscatter diffraction, petrofabrics and microstructures were compared between the center and the edge of a gabbroic shear zone collected from IODP Hole U1309D. Analysis of the crystallographic preferred orientation, internal deformation, and grain size variations of feldspar was also performed.

1 Halfpenny, A., and Prior, D., 2009. Data report: an electron backscatter diffraction study of a gabbroic shear zone, IODP Expedition 304/305. In Blackman, D.K., Ildefonse, B., John, B.E., Ohara, Y., Miller, D.J., MacLeod, C.J., and the Expedition 304/305 Scientists, Proc. IODP, 304/305: College Station, TX (Integrated Ocean Drilling Program Management International, Inc.). doi:10.2204/​iodp.proc.304305.201.2009

2 Department of Earth and Ocean Sciences, University of Liverpool, Merseyside L69 3GP, United Kingdom.

3 Present address: Research School of Earth Sciences, Australian National University, Mills Road, ACT 0200, Australia. Correspondence author: Angela.halfpenny@anu.edu.au

Initial receipt: 3 February 2008
Acceptance: 25 July 2008
Publication: 30 January 2009
MS 304305-201