A. Schreider

发表

Paleointensity of the geomagnetic field in the last half-million years in regions of the Red Sea and south of the Mid-Atlantic Ridge

A. Schreider, V. Trukhin, V. Maksimochkin, 2010 .

Did a change in tectonic regime occur between the Phanerozoic and earlier Epochs?

N. Sneeuw, G. Panza, F. Krumm, 2012, Rendiconti Lincei.

Reprint of “Magmatism, structure and age of Dove Basin (Antarctica): A key to understanding South Scotia Arc development”

J. Galindo‐Zaldívar, P. Ruano, L. Somoza, 2014 .

Development of deep extensional basins associated with the sinistral transcurrent fault zone of the Scotia-Antarctic plate boundary

J. Galindo‐Zaldívar, J. Rodríguez-Fernández, A. Maldonado, 2007 .

Extensional deformation and development of deep basins associated with the sinistral transcurrent fault zone of the Scotia–Antarctic plate boundary

J. Galindo‐Zaldívar, F. Bohoyo, E. Suriñach, 2007 .

Geophysical Evidence of a Relict Oceanic Crust in the Southwestern Scotia Sea

F. Coren, F. Coren, A. Schreider, 1997 .

A model of oceanic development by ridge jumping: Opening of the Scotia Sea

J. Galindo‐Zaldívar, L. Somoza, F. Lobo, 2014 .

Propagating rift during the opening of a small oceanic basin: The Protector Basin (Scotia Arc, Antarctica)

J. Galindo‐Zaldívar, A. Maldonado, F. Bohoyo, 2006 .

Gorringe Ridge gravity and magnetic anomalies are compatible with thrusting at a crustal scale

J. Galindo‐Zaldívar, A. Maldonado, A. Schreider, 2003 .