The formation of SiO₂-rich melts within the deep oceanic crust by hydrous partial melting of gabbros

By Koepke Juergen   Berndt Jasper   Feig Sandrin   Holtz Francois  

Contributions to Mineralogy and Petrology, Vol. 153, Iss. 1, 2007-01 ,pp. : 67-84

Springer Publishing Company

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Hypersolidus deformation in the lower crust of the Josephine ophiolite: evidence for kinematic decoupling between the upper and lower oceanic crust

By Yoshinobu A.S.   Harper G.D.  

Journal of Structural Geology, Vol. 26, Iss. 1, 2004-01 ,pp. : 163-175

Elsevier

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The reaction mechanism of fluid-induced partial melting of gabbro in the oceanic crust

By Wolff Paul Eric   Koepke Jürgen   Feig Sandrin T.  

European Journal of Mineralogy, Vol. 25, Iss. 3, 2013-06 ,pp. : 279-298

E. Schweizerbart'sche Verlagsbuchhandlung

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Hydration and dehydration in the lower margin of a cold mantle wedge: implications for crust-mantle interactions and petrogeneses of arc magmas

By Chen Yi  

International Geology Review, Vol. 55, Iss. 12, 2013-09 ,pp. : 1506-1522

Taylor & Francis Ltd

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Altered mafic lower continental crust as a source for low δ 18 O-granodiorites (Damara orogen, Namibia)?

By Jung S.   Mezger K.   Hoernes S.   Hoffbauer R.  

Mineralogy and Petrology, Vol. 91, Iss. 1-2, 2007-09 ,pp. : 1-10

Springer Publishing Company

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