Does intermediate spreading-rate oceanic crust result from episodic transition between magmatic and magma-dominated, faulting-enhanced spreading?—The Costa Rica Rift example-Reference-Cited by-同舟云学术

Does intermediate spreading-rate oceanic crust result from episodic transition between magmatic and magma-dominated, faulting-enhanced spreading?—The Costa Rica Rift example

Published:2019-04-18 Issue:3 Volume:218 Page:1617-1641
ISSN:0956-540X
Container-title:Geophysical Journal International
language:en
Short-container-title:

Author:

Wilson D J¹,Robinson A H¹,Hobbs R W¹,Peirce C¹^ORCID,Funnell M J¹

Affiliation:

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

Funder

Natural Environmental Research Council

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/gji/advance-article-pdf/doi/10.1093/gji/ggz184/28543201/ggz184.pdf

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4. Geologically current motion of 56 plates relative to the no-net-rotation reference frame;Argus;Geochem. Geophys. Geosys.,2011

5. Geothermal heating in the Panama Basin. Part I: hydrography of the basin;Banyte;J. geophys. Res.,2018

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