TY - JOUR
T1 - Variation in styles of rifting in the Gulf of California
AU - Lizarralde, Daniel
AU - Axen, Gary J.
AU - Brown, Hillary E.
AU - Fletcher, John M.
AU - González-Fernández, Antonio
AU - Harding, Alistair J.
AU - Holbrook, W. Steven
AU - Kent, Graham M.
AU - Paramo, Pedro
AU - Sutherland, Fiona
AU - Umhoefer, Paul J.
N1 - Funding Information:
Acknowledgements We thank the captains and crew of the RV Maurice Ewing and RV New Horizon, the OBSIP teams, J. Urban, and A. Gorman for his efforts as Chief Scientist on the RV New Horizon. The Lamont Earth Observatory Marine Office and CICESE provided support before and during the experiment. This work was funded by a grant from the US NSF-MARGINS programme.
PY - 2007/7/26
Y1 - 2007/7/26
N2 - Constraints on the structure of rifted continental margins and the magmatism resulting from such rifting can help refine our understanding of the strength of the lithosphere, the state of the underlying mantle and the transition from rifting to seafloor spreading. An important structural classification of rifts is by width, with narrow rifts thought to form as necking instabilities (where extension rates outpace thermal diffusion) and wide rifts thought to require a mechanism to inhibit localization, such as lower-crustal flow in high heat-flow settings. Observations of the magmatism that results from rifting range from volcanic margins with two to three times the magmatism predicted from melting models to non-volcanic margins with almost no rift or post-rift magmatism. Such variations in magmatic activity are commonly attributed to variations in mantle temperature. Here we describe results from the PESCADOR seismic experiment in the southern Gulf of California and present crustal-scale images across three rift segments. Over short lateral distances, we observe large differences in rifting style and magmatism - from wide rifting with minor synchronous magmatism to narrow rifting in magmatically robust segments. But many of the factors believed to control structural evolution and magmatism during rifting (extension rate, mantle potential temperature and heat flow) tend to vary over larger length scales. We conclude instead that mantle depletion, rather than low mantle temperature, accounts for the observed wide, magma-poor margins, and that mantle fertility and possibly sedimentary insulation, rather than high mantle temperature, account for the observed robust rift and post-rift magmatism.
AB - Constraints on the structure of rifted continental margins and the magmatism resulting from such rifting can help refine our understanding of the strength of the lithosphere, the state of the underlying mantle and the transition from rifting to seafloor spreading. An important structural classification of rifts is by width, with narrow rifts thought to form as necking instabilities (where extension rates outpace thermal diffusion) and wide rifts thought to require a mechanism to inhibit localization, such as lower-crustal flow in high heat-flow settings. Observations of the magmatism that results from rifting range from volcanic margins with two to three times the magmatism predicted from melting models to non-volcanic margins with almost no rift or post-rift magmatism. Such variations in magmatic activity are commonly attributed to variations in mantle temperature. Here we describe results from the PESCADOR seismic experiment in the southern Gulf of California and present crustal-scale images across three rift segments. Over short lateral distances, we observe large differences in rifting style and magmatism - from wide rifting with minor synchronous magmatism to narrow rifting in magmatically robust segments. But many of the factors believed to control structural evolution and magmatism during rifting (extension rate, mantle potential temperature and heat flow) tend to vary over larger length scales. We conclude instead that mantle depletion, rather than low mantle temperature, accounts for the observed wide, magma-poor margins, and that mantle fertility and possibly sedimentary insulation, rather than high mantle temperature, account for the observed robust rift and post-rift magmatism.
UR - http://www.scopus.com/inward/record.url?scp=34547162818&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=34547162818&partnerID=8YFLogxK
U2 - 10.1038/nature06035
DO - 10.1038/nature06035
M3 - Article
C2 - 17653189
AN - SCOPUS:34547162818
SN - 0028-0836
VL - 448
SP - 466
EP - 469
JO - Nature
JF - Nature
IS - 7152
ER -