Transform fault effect on mantle melting in the MARK area – Technische Informationsbibliothek (TIB)

When choosing delivery via TIB-Portal by clicking 'Order' Royalty mentioned below is applicable as part of the total price When choosing delivery via TIB-Portal by clicking 'Order' Royalty mentioned below is applicable as part of the total price Average compositions and analyses range for clinopyroxene, olivines, orthopyroxene, and spinel from the MARK area at DSDP Site 45-395A, and ODP Site 153-920, supplement to: Ghose, Indraneel, Cannat, Mathilde, Seyler, Monique (1996): Transform fault effect on mantle melting in the MARK area (Mid-Atlantic Ridge south of the Kane transform). Geology, 24(12), 1139-1142 Seismic velocities of lower crustal and upper mantle rocks from the slow-spreading Mid-Atlantic Ridge, south of the Kane Transform Zone (MARK) Slow cooling of middle and lower oceanic crust inferred from multicomponent magnetizations of gabbroic rocks from the Mid‐Atlantic Ridge south of the Kane fracture zone (MARK) area Seafloor geomagnetic vector anomaly of the intersection of the Mid‐Atlantic Ridge and the Kane Transform Fault: Implications for magnetization of the oceanic crust Seafloor geomagnetic vector anomaly of the intersection of the Mid-Atlantic Ridge and the Kane Transform Fault: Implications for magnetization of the oceanic crust Source.


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Last Modified: April 18, 2016 @ 12:08 pm