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:
Related Expeditions:
IODP 301
Identifier:
ID:
2007-088829
Type:
georefid
ID:
1932-9415
Type:
issn
ID:
10.2204/iodp.sp.301.2004
Type:
doi
Creator:
Name:
Fisher, Andrew T.
Affiliation:
University of California, Santa Cruz, Earth Sciences Department, Santa Cruz, CA, United States
Role:
author
Name:
Urabe, Tetsuro
Affiliation:
University of Tokyo, Japan
Role:
author
Name:
Klaus, Adam
Affiliation:
Intergrated Ocean Drilling Program, United States
Role:
author
Identification:
Title:
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
Year:
2004
Source:
Scientific Prospectus (Integrated Ocean Drilling Program)
Publisher:
IODP Management International, College Station, TX, United States
Volume:
301
Issue:
Pages:
53 pp.
Abstract:
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.
Language:
English
Genre:
Serial
Rights:
URL:
Coverage: Geographic coordinates: North:47.4600 West:-127.4600 East:
-127.4500 South:47.4500
Keywords: 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;
.