Axial morphology along the Southern Chile Rise
Blackman, Donna K.
German, Christopher R.
Thurber, Andrew R.
Henig, A. S.
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Morphology of four spreading segments on the southern Chile Rise is described based on multi-beam bathymetric data collected along the axial zones. The distribution of axial volcanoes, the character of rift valley scarps, and the average depths vary between Segment 1 in the south, terminating at the Chile Triple Junction, and Segment 4 in the north, which are separated by three intervening transform faults. Despite this general variability, there is a consistent pattern of clockwise rotation of the southern-most axial volcanic ridge within each of Segments 2, 3, and 4, relative to the overall trend of the rift valley. A combination of local ridge-transform intersection stresses and regional tectonics may influence spreading axis evolution in this sense.
Author Posting. © The Author(s), 2012. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Marine Geology 315-318 (2012): 58-63, doi:10.1016/j.margeo.2012.06.001.
Suggested CitationPreprint: Blackman, Donna K., Appelgate, B., German, Christopher R., Thurber, Andrew R., Henig, A. S., "Axial morphology along the Southern Chile Rise", 2012-06, https://doi.org/10.1016/j.margeo.2012.06.001, https://hdl.handle.net/1912/5470
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