Extinct spreading on the Cocos Ridge

Author:

Meschede M.1,Barckhausen U.2,Worm H.‐U.3

Affiliation:

1. Institute of Geology, University of Tuebingen, Sigwartstr. 10, D‐72076 Tuebingen, Germany,

2. Institute of Geophysics, University of Goettingen, Herzberger Landstr. 180, D‐37075 Goettingen, Germany,

3. Institute of Geophysics, University of Goettingen, Herzberger Landstr. 180, D‐37075 Goettingen, Germany

Publisher

Wiley

Subject

Geology

Reference31 articles.

1. Heat flow near a fossil ridge on the north flank of the Galapagos Spreading Center

2. 2A. Astorga, J.A. Fernandez, G. Barboza, L. Campos, J. Obando, A. Aguilar, and L.G. Obando , 1989, Cuencas sedimentarias de Costa Rica: evolucion Cretacico Superior-Cenozoica y potencial de hidrocarburos , Symposium of Energy and Mineral Potentials, Central American-Caribbean Region, San Jose, Costa Rica, Circum Pacific Council.

3. Magnetic signature of upper plate structures and subducting seamounts at the convergent margin off Costa Rica

4. 5R. Batiza , 1986, Failed rifts. In: The Eastern Pacific Ocean and Hawaii (E.L. Winterer, D.M. Hussong and R.W. Decker, eds). The Geology of North America, Vol. N, Ch. 11, pp. 177 -186. The Geological Society of America, Boulder, CO.

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