Journal article
The Germania Land deformation zone and related structures, North-east Greenland
Rapport - Gronlands Geologiske Undersogelse (1964), Vol.162, pp.113-127
1994
DOI: 10.34194/rapggu.v162.8253
Abstract
The Germania Land deformation zone in North-East Greenland consists of two subparallel, NW-striking strands of mylonites and cataclasites. The quasiplastic mylonites formed under low grade (biotite zone) conditions following high grade Caledonian metamorphism. Displacements on the Germania Land deformation zone and parallel zones at Danmarkshavn were predominantly dextral strike slip. Along with the similar, but sinistral, Storstrømmen shear zone, these zones record a late Caledonian phase of orogen-parallel movement. The Germania Land deformation zone is also the locus of Carboniferous normal faulting and basin development.
Details
- Title: Subtitle
- The Germania Land deformation zone and related structures, North-east Greenland
- Creators
- Joseph M Hull - Seattle Central Community College, Division of Science & Mathematics Seattle, WA USA United StatesJane A Gilotti - New York State Museum USA United States
- Contributors
- A. K Higgins (Editor) - Geological Survey of Greenland Copenhagen DNK Denmark
- Resource Type
- Journal article
- Publication Details
- Rapport - Gronlands Geologiske Undersogelse (1964), Vol.162, pp.113-127
- DOI
- 10.34194/rapggu.v162.8253
- ISSN
- 0418-6559
- eISSN
- 2597-2944
- Publisher
- Gronlands Geologiske Undersogelse
- Alternative title
- Geology of North-east Greenland
- Language
- English
- Date published
- 1994
- Academic Unit
- Earth and Environmental Sciences
- Record Identifier
- 9984240791302771
Metrics
37 Record Views