New packer experiments and borehole logs in upper oceanic crust: Evidence for ridge-parallel consistency in crustal hydrogeological properties

Author:

Becker Keir1,Fisher Andrew T.2,Tsuji Takeshi3

Affiliation:

1. Division of Marine Geology and Geophysics; RSMAS, University of Miami; 4600 Rickenbacker Causeway Miami Florida 33149 USA

2. Earth and Planetary Sciences Department; University of California; Santa Cruz California USA

3. International Institute for Carbon-Neutral Energy Research (WPI-I2CNER); Kyushu University; Fukuoka Japan

Funder

NSF

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference66 articles.

1. Ridge-flank alteration of upper ocean crust in the eastern Pacific: Synthesis of results for volcanic rocks of Holes 504B and 896A;Alt;Proc. Ocean Drill. Program Sci. Results,1996

2. Permeability, underpressures and convection in the oceanic crust near the Costa Rica Rift, eastern equatorial Pacific;Anderson;J. Geophys. Res.,1982

3. Permeability versus depth in the upper oceanic crust: In-situ measurements in DSDP Hole 504B, eastern equatorial Pacific;Anderson;J. Geophys. Res.,1985

4. Physical properties of young (3.5 m.y.) oceanic crust from the eastern flank of Juan de Fuca Ridge: Comparison of wireline and core measurements with global data;Bartetzko;J. Geophys. Res.,2008

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