REFERENCES

Bohrmann, G., Greinert, J., Suess, E., and Torres, M., 1998. Authigenic carbonates from the Cascadia subduction zone and their relation to gas hydrate stability. Geology, 26:647–650.

Johnson, J.E., Goldfinger, C., and Suess, E., 2003. Geophysical constraints on the surface distribution of authigenic carbonates across the Hydrate Ridge region, Cascadia margin. Mar. Geol., 202:79–120.

Lumsden, D.N., 1979. Discrepancy between thin section and X-ray estimates of dolomite in limestone. J. Sediment. Petrol., 49:429–436.

Sample, J.C., and Kopf, A., 1995. Isotope geochemistry of syntectonic carbonate cements and veins from the Oregon Margin: implications for the hydrogeologic evolution of the accretionary wedge. In Carson, B., Westbrook, G.K., Musgrave, R.J., and Suess, E. (Eds.), Proc. ODP, Sci. Results, 146 (Pt 1): College Station, TX (Ocean Drilling Program), 137–148.

Teichert, B.M.A., Gussone, N., Eisenhauer, A., and Bohrmann, G., 2005. Clathrites: archives of near-seafloor pore-fluid evolution (^44/40Ca, ¹³C, ¹⁸O) in gas hydrate environments. Geology, 33:213–216.

Tréhu, A.M, Bohrmann, G., Rack, F.R., Torres, M.E., et al., 2003. Proc. ODP, Init. Repts., 204 [Online]. Available from World Wide Web: <http://www-odp.tamu.edu/publications/204_IR/204ir.htm>. [Cited 2004-12-01]