Date: 2012-11-04 07:57:00Mid-ocean ridge Convergent boundary Seafloor spreading Iceland plume Mantle plume Geology Plate tectonics Cayman Trough | | Slice 28: Lower Tejas II – Lutetian – Bartonian – 49-37 Ma This was a time of active orogenesis, with the closure of oceanic basins in the AlpineHimalayan area, continental-oceanic collisions in the Andes, reorganization of Pacific platesAdd to Reading ListSource URL: www.dinodata.orgDownload Document from Source Website File Size: 51,75 KBShare Document on Facebook
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