Fisher, Andrew T. et al. (2004): Integrated Ocean Drilling Program, Expedition 301 scientific prospectus; Juan de Fuca hydrogeology; the hydrogeologic architecture of basaltic oceanic crust; compartmentalization, anisotropy, microbiology, and crustal-scale properties on the eastern flank of the Juan de Fuca Ridge, eastern Pacific Ocean

Leg/Site/Hole:
IODP 301
Identifier:
2007-088829
georefid

1932-9415
issn

10.2204/iodp.sp.301.2004
doi

Creator:
Fisher, Andrew T.
University of California, Santa Cruz, Earth Sciences Department, Santa Cruz, CA, United States
author

Urabe, Tetsuro
University of Tokyo, Japan
author

Klaus, Adam
Intergrated Ocean Drilling Program, United States
author

Identification:
Integrated Ocean Drilling Program, Expedition 301 scientific prospectus; Juan de Fuca hydrogeology; the hydrogeologic architecture of basaltic oceanic crust; compartmentalization, anisotropy, microbiology, and crustal-scale properties on the eastern flank of the Juan de Fuca Ridge, eastern Pacific Ocean
2004
Scientific Prospectus (Integrated Ocean Drilling Program)
IODP Management International, College Station, TX, United States
301
53 pp.
Integrated Ocean Drilling Program (IODP) Expedition 301 is part of a multidisciplinary experiment to evaluate formation-scale hydrogeologic properties (transmission and storage) within oceanic crust; determine how fluid pathways are distributed within an active hydrothermal system; establish linkages between fluid circulation, alteration, and geomicrobial processes; and determine relations between seismic and hydrologic anisotropy. During IODP Expedition 301, we will replace two existing subseafloor observatories and install two new observatories, creating a three-dimensional monitoring network. We will also core and sample basaltic upper crust and overlying sediments to assess physical, geochemical, and microbiological conditions and complete a series of downhole experiments (e.g., packer and downhole logging) in basement to assess hydrogeologic properties near the new boreholes. An additional basement hole will be drilled during a later expedition, allowing completion of controlled, long-term, cross-hole testing. Collectively, these operations and experiments will allow us to evaluate the extent to which oceanic crust is connected vertically and horizontally; the influence of these connections on fluid, solute, heat, and microbiological processes; and the importance of scaling on hydrologic properties.
English
Coverage:Geographic coordinates:
North:47.4600
West:-127.4600East: -127.4500
South:47.4500

Solid-earth geophysics; Applied geophysics; basaltic composition; basement; boreholes; circulation; cores; crust; downhole methods; drilling; East Pacific; Expedition 301; expeditions; flows; fluid phase; geophysical methods; geophysical profiles; geophysical surveys; hydrothermal conditions; Integrated Ocean Drilling Program; Juan de Fuca Ridge; marine drilling; marine methods; North Pacific; Northeast Pacific; oceanic crust; Pacific Ocean; planning; sampling; seismic methods; seismic profiles; surveys; well-logging;

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