Open AccessDownhole variation of lithium and oxygen isotopic compositions of oceanic crust at East Pacific Rise, ODP Site 1256
Author(s) -
Gao Y.,
Vils F.,
Cooper K. M.,
Banerjee N.,
Harris M.,
Hoefs J.,
Teagle D. A. H.,
Casey J. F.,
Elliott T.,
Laverne C.,
Alt J. C.,
Muehlenbachs K.
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 - 10.1029/2012gc004207
Subject(s) - geology , oceanic crust , seafloor spreading , dike , crust , basalt , geochemistry , hydrothermal circulation , seamount , volcanic rock , subduction , volcano , geophysics , seismology , tectonics
Bulk rock lithium and oxygen isotope compositions from ODP Site 1256 were analyzed to investigate the seawater circulation in the upper oceanic crust formed at the East Pacific Rise (EPR). The upper extrusive basalts have δ 18 O values from +6.1‰ to +9.2‰, reflecting alteration of oceanic crust by seawater at low temperatures (<200–250°C). Bulk rocks from the sheeted dike complex and plutonic section have overall lower δ 18 O values (+3.0‰–+5.5‰). In the sheeted dike complex bulk rock δ 18 O values gradually decrease with depth, and then increase toward the fresh MORB δ 18 O value after reaching a minimum of +3.0‰ at ∼1350 m below seafloor (mbsf). The entire sampled crust is dominated by rocks with low lithium contents relative to fresh MORBs except for a few localized Li enrichment. The upper volcanic zone is characterized by a spread of δ 7 Li from low to high values relative to average unaltered MORB values ( δ 7 Li = +3.4 ± 1.4‰). The presence of rocks with low δ 7 Li values in the upper crust most likely indicates zones of upwelling of relatively hot (∼200–250°C) hydrothermal fluids. In the sheeted dike complex, bulk rock δ 7 Li values show wide range of variation, but exhibit a general trend from enriched to depleted values at ∼1280 mbsf and then return to that for fresh MORB within the upper tens of meters of the plutonic section at the bottom of the after reaching a minimum at ∼1350 mbsf ( δ 7 Li = −1.6‰). The downhole pattern of δ 7 Li principally reflects variations in water‐rock ratio (w/r) together with a downhole increase of temperature. Seawater flow in the upper volcanic zone is likely to be channeled with generally small but variable w/r ratios. The w/r ratios increase rapidly with depth in the lower volcanic section into the sheeted dike complex indicating water dominated pervasive hydrothermal flow due to intensive upwelling of hydrothermal fluids.