Rapid Cooling of the Crust and Mantle at Hess Deep is Consistent with the Sheeted Sill Model for Accretion of Oceanic Crust


Nadine Lynne Grambling, Brown University, Department of Earth, Environmental and Planetary Sciences, Providence, United States, Nicholas J Dygert, University of Tennessee, Knoxville, TN, United States and Marlon M Jean, University of Rochester, Rochester, United States
Back to: Crustal Formation, Fluid–Rock Reactions, and Subsurface Microbial Communities in the Samail Ophiolite: Results from the Oman Drilling Project and Related Research II