Constraints on crustal structure of adjacent OCCs and segment boundaries at 13°N on the Mid-Atlantic Ridge

Author:

Peirce C1ORCID,Reveley G1,Robinson A H1,Funnell M J1,Searle R C1,Simão N M1,MacLeod C J2,Reston T J3

Affiliation:

1. Department of Earth Sciences, Durham University, South Road, Durham, DH13LE, UK

2. School of Earth and Ocean Sciences, Cardiff University, Park Place, Cardiff, CF103AT, UK

3. School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B152TT, UK

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Reference129 articles.

1. The rate of detachment faulting at Atlantis Bank, SW Indian Ridge;Baines;Earth planet. Sci. Lett.,2008

2. A new hydrothermal field at 13°30’N on the Mid-Atlantic Ridge;Beltenev;InterRidge News,2007

3. Lower crustal variability and the crust/mantle transition at the Atlantis Massif oceanic core complex;Blackman;Geophys. Res. Lett.,2010

4. Isostatic compensation of tectonic features of the Mid-Atlantic Ridge: 25–27°30’S;Blackman;J. geophys. Res.,1991

5. Seafloor mapping and sampling of the MAR 30° N oceanic core complex - MARVEL (Mid-Atlantic ridge vents in extending lithosphere);Blackman;InterRidge News,2001

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