Previous Page  228 / 352 Next Page
Information
Show Menu
Previous Page 228 / 352 Next Page
Page Background

SánchezMartínez,S.,Gerdes,A.,Arenas,R.,Abati,J.,2012.

TheBazarOphioliteofNWIberia:

arelict oftheIapetus-Tornquist Oceanin theVariscansuture. TerraNova24, 283

–

294.

Sommer, M., Hüneke, H., Meschede, M., Cobiella-Reguera, J., 2011.

Geodynamic model of

the northwestern Caribbean: scaled reconstruction of Late Cretaceous to Late Eocene

plate boundary relocation in Cuba. Neues Jahrbuch für Geologie und Paläontologie,

Monatschefte 259, 299

–

312.

Stamp

fl

i, G.M., Borel, G.D., 2002.

A plate tectonic model for the Paleozoic and Mesozoic

constrained by dynamic plate boundaries and restored synthetic oceanic isochrons.

Earth and Planetary Science Letters 196, 17

–

33.

ten Brink, U.S., Coleman, D.F., Dillon, W.P., 2002.

The nature of the crust under Cayman

Trough from gravity. Marine and Petroleum Geology 19, 971

–

987.

Warren, C.J., Beaumont, C., Jamieson, R.A., 2008.

Modelling tectonic styles and

ultra-high pressure (UHP) rock exhumation during the transition from oceanic

subduction to continental collision. Earth and Planetary Science Letters 267,

129

–

145.

Weil, A.B., Gutiérrez-Alonso, G., Johnston, S.T., Pastor-Galán, D., 2012.

Kinematic

constraints on buckling a lithospheric-scale orocline along the northern margin of

Gondwana: a geologic synthesis. Tectonophysics 582, 25

–

49.

763

R. Arenas et al. / Gondwana Research 25 (2014) 756

–

763

8. TWO STAGE COLLISION

212