No spreading across the southern Juan de Fuca ridge axial cleft during 1994-1996

Physics – Geophysics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

9

Geodesy And Gravity: Crustal Movements-Interplate, Marine Geology And Geophysics: Instruments And Techniques, Tectonophysics: Plate Motions-Present And Recent, Geodesy And Gravity: Instruments And Techniques

Scientific paper

Direct-path acoustic measurements between seafloor transponders observed no significant extension (-10+/-14mm/yr) from August 1994 to September 1996 at the southern Juan de Fuca Ridge (44°40' N and 130°20' W). The acoustic path for the measurement is a 691-m baseline straddling the axial cleft, which bounds the Pacific and Juan de Fuca plates. Given an expected full-spreading rate of 56 mm/yr, these data suggest that extension across this plate boundary occurs episodically within the narrow (~1 km) region of the axial valley floor, and that active deformation is occurring between the axial cleft and the plate interior. A cleft-parallel 714-m baseline located 300 m to the west of the cleft on the Pacific plate monitored system performance and, as expected, observed no motion (+5+/-7mm/yr) between the 1994 and 1996 surveys.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

No spreading across the southern Juan de Fuca ridge axial cleft during 1994-1996 does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with No spreading across the southern Juan de Fuca ridge axial cleft during 1994-1996, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and No spreading across the southern Juan de Fuca ridge axial cleft during 1994-1996 will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1459263

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.