Volcanoes, fluids, and life at mid-ocean ridge spreading centers
DS Kelley, JA Baross, JR Delaney - Annual Review of Earth and …, 2002 - annualreviews.org
▪ Abstract The recent recognition of a potentially vast, unexplored hot microbial biosphere
associated with active volcanism along the global mid-ocean ridge network has …
associated with active volcanism along the global mid-ocean ridge network has …
Subduction fluxes of water, carbon dioxide, chlorine, and potassium
RD Jarrard - Geochemistry, Geophysics, Geosystems, 2003 - Wiley Online Library
The alteration of upper oceanic crust entails growth of hydrous minerals and loss of
macroporosity, with associated large‐scale fluxes of H2O, CO2, Cl−, and K2O between …
macroporosity, with associated large‐scale fluxes of H2O, CO2, Cl−, and K2O between …
Analysis and mapping of an updated terrestrial heat flow data set
F Lucazeau - Geochemistry, Geophysics, Geosystems, 2019 - Wiley Online Library
The number of heat flow measurements at the Earth surface has significantly increased
since the last global analysis (Pollack et al., 1993, https://doi. org/10.1029/93RG01249), and …
since the last global analysis (Pollack et al., 1993, https://doi. org/10.1029/93RG01249), and …
Seismic evidence for overpressured subducted oceanic crust and megathrust fault sealing
Water and hydrous minerals play a key part in geodynamic processes at subduction zones,,
by weakening the plate boundary, aiding slip and permitting subduction—and indeed plate …
by weakening the plate boundary, aiding slip and permitting subduction—and indeed plate …
Carbon dioxide cycling and implications for climate on ancient Earth
NH Sleep, K Zahnle - Journal of Geophysical Research …, 2001 - Wiley Online Library
The crustal Urey cycle of CO2 involving silicate weathering and metamorphism acts as a
dynamic climate buffer. In this cycle, warmer temperatures speed silicate weathering and …
dynamic climate buffer. In this cycle, warmer temperatures speed silicate weathering and …
Fluid involvement in normal faulting
RH Sibson - Journal of Geodynamics, 2000 - Elsevier
Evidence of fluid interaction with normal faults comes from their varied role as flow barriers
or conduits in hydrocarbon basins and as hosting structures for hydrothermal mineralisation …
or conduits in hydrocarbon basins and as hosting structures for hydrothermal mineralisation …
An inverted continental Moho and serpentinization of the forearc mantle
Volatiles that are transported by subducting lithospheric plates to depths greater than 100
km are thought to induce partial melting in the overlying mantle wedge, resulting in arc …
km are thought to induce partial melting in the overlying mantle wedge, resulting in arc …
Mapping permeability over the surface of the Earth
T Gleeson, L Smith, N Moosdorf… - Geophysical …, 2011 - Wiley Online Library
Permeability, the ease of fluid flow through porous rocks and soils, is a fundamental but
often poorly quantified component in the analysis of regional‐scale water fluxes …
often poorly quantified component in the analysis of regional‐scale water fluxes …
[HTML][HTML] On the global distribution of hydrothermal vent fields
ET Baker, CR German - Mid-Ocean Ridges: Hydrothermal …, 2004 - pmel.noaa.gov
The" magmatic budget hypothesis" proposes that variability in magma supply is the primary
control on the large-scale hydrothermal distribution pattern along oceanic spreading ridges …
control on the large-scale hydrothermal distribution pattern along oceanic spreading ridges …
Iron and sulfide oxidation within the basaltic ocean crust: implications for chemolithoautotrophic microbial biomass production
W Bach, KJ Edwards - Geochimica et Cosmochimica Acta, 2003 - Elsevier
Microbial processes within the ocean crust are of potential importance in controlling rates of
chemical reactions and thereby affecting chemical exchange between the oceans and …
chemical reactions and thereby affecting chemical exchange between the oceans and …