Evolution of the East Pacific Rise between 3°S and 13°S since the Middle Miocene
Journal Article
·
· Geophysical Research Letters
Since Middle Miocene time seafloor spreading activity in the southeast Pacific has shifted westward from the Galapagos Rise, then the last active segment of the Farallon Ridge system in the South Pacific, to the East Pacific Rise. This shift was accomplished by three large jumps of fracture‐zone‐bound axial sections which progressed from south to north. The jumps spanned an average distance of 750 km and occurred 8.2, 6.4 and 5.7 m.y. ago respectively. Positioning of the newly‐formed axes along the EPR trend apparently was controlled by asthenospheric rather than lithospheric phenomena.
- Research Organization:
- Department of Atmospheric and Oceanic Science, The University of Michigan, Ann Arbor, Michigan 48100
- OSTI ID:
- 6920786
- Journal Information:
- Geophysical Research Letters, Journal Name: Geophysical Research Letters Journal Issue: 7 Vol. 5; ISSN 0094-8276
- Publisher:
- American Geophysical Union (AGU)
- Country of Publication:
- United States
- Language:
- English
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