Abstract
Multidisciplinary studies of the slow-spreading (<30 mm a-1) ridge axis in the MARK Area define a number of discrete spreading cells in each of which the style of seafloor spreading is distinctly different. In some cells, episodic magmatism and asymmetrical detachment faulting occur, whereas in others, a more continuous magma supply and symmetrical, steep, normal faulting dominate. Oblique-slip fault zones that link the cells are a kinematic requirement of such along-strike variations and are similar to the accommodation or transfer zones of continental rifts. -Authors
Original language | English (US) |
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Pages (from-to) | 107-116 |
Number of pages | 10 |
Journal | Unknown Journal |
State | Published - 1992 |
Externally published | Yes |
ASJC Scopus subject areas
- General Environmental Science
- General Earth and Planetary Sciences