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Elongate summit calderas as Neogene paleostress indicators in Antarctica
The orientations and ages of elongate summit calderas on major polygenetic volcanoes were compiled to
document Miocene to Pleistocene Sh (minimum horizontal stress) directions on the western and northern flanks of the
West Antarctic rift system. Miocene to Pleistocene summit calderas along the western Ross Sea show relatively
consistent ENE long axis trends, which are at a high angle to the Transantarctic Mountain Front and parallel to the
N77ºE Sh direction at Cape Roberts. The elongation directions of many Miocene to Pleistocene summit calderas in
Marie Byrd Land parallel the alignment of polygenetic volcanoes in which they occur, except several Pleistocene
calderas with consistent NNE to NE trends. The overall pattern of elongate calderas in Marie Byrd Land is probably due
to a combination of structurally controlled orientations and regional stress fields in which Sh is oriented NNE to NE at a
moderate to high angle to the trace of the West Antarctic rift system.
Suggested Citation
Paulsen, T., Wilson, T.J., 2007, Elongate summit calderas as Neogene paleostress indicators in Antarctica: U.S. Geological Survey Open-File Report 2007-1047-SRP-072, 6 p., https://doi.org/10.3133/ofr20071047SRP072.
ISSN: 2331-1258 (online)
Study Area
Publication type
Report
Publication Subtype
USGS Numbered Series
Title
Elongate summit calderas as Neogene paleostress indicators in Antarctica
Series title
Open-File Report
Series number
2007-1047-SRP-072
DOI
10.3133/ofr20071047SRP072
Year Published
2007
Language
English
Publisher
U.S. Geological Survey
Publisher location
Reston, VA
Description
6 p.
Larger Work Type
Report
Larger Work Subtype
USGS Numbered Series
Larger Work Title
Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. Santa Barbara, California, U.S.A.--August 26 to September 1, 2007