Open AccessThe cooling history and the depth of detachment faulting at the Atlantis Massif oceanic core complex
Author(s) -
Schoolmeesters Nicole,
Cheadle Michael J.,
John Barbara E.,
Reiners Peter W.,
Gee Jeffrey,
Grimes Craig B.
Publication year - 2012
Publication title -
geochemistry, geophysics, geosystems
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.928
H-Index - 136
ISSN - 1525-2027
DOI - 10.1029/2012gc004314
Subject(s) - geology , zircon , massif , detachment fault , seafloor spreading , gabbro , oceanic crust , geochemistry , metamorphic core complex , mantle (geology) , crust , mid atlantic ridge , hydrothermal circulation , petrology , seismology , igneous rock , paleontology , subduction , tectonics , extensional definition
Oceanic core complexes (OCCs) are domal exposures of oceanic crust and mantle interpreted to be denuded to the seafloor by large slip oceanic detachment faults. We combine previously reported U‐Pb zircon crystallization ages with (U‐Th)/He zircon thermochronometry and multicomponent magnetic remanence data to determine the cooling history of the footwall to the Atlantis Massif OCC (30°N, MAR) and help establish cooling rates, as well as depths of detachment faulting and gabbro emplacement. We present nine new (U‐Th)/He zircon ages for samples from IODP Hole U1309D ranging from 40 to 1415 m below seafloor. These data paired with U‐Pb zircon ages and magnetic remanence data constrain cooling rates of gabbroic rocks from the upper 800 m of the central dome at Atlantis Massif as 2895 (+1276/−1162) °C Myr −1 (from ∼780°C to ∼250°C); the lower 600 m of the borehole cooled more slowly at mean rates of ∼500 (+125/−102) °C Myr −1 (from ∼780°C to present‐day temperatures). Rocks from the uppermost part of the hole also reveal a brief period of slow cooling at rates of ∼300°C Myr −1 , possibly due to hydrothermal circulation to ∼4 km depth through the detachment fault zone. Assuming a fault slip rate of 20 mm/yr (from U‐Pb zircon ages of surface samples) and a rolling hinge model for the sub‐surface fault geometry, we predict that the 780°C isotherm lies at ∼7 km below the axial valley floor, likely corresponding both to the depth at which the semi‐brittle detachment fault roots and the probable upper limit of significant gabbro emplacement.