Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
10144949 | Earth and Planetary Science Letters | 2018 | 14 Pages |
Abstract
- A large region of 18-24 M.y. old seafloor is cooled by fluid flow through seamounts.
- Simulations indicate very high crustal permeability, 10â10 to 10â9Â m2.
- Outcrop-to-outcrop circulation at the field site is likely to be 1000-7000 kg/s.
- Outcrop-to-outcrop circulation is less important than single-outcrop circulation.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth and Planetary Sciences (General)
Authors
Rachel M. Lauer, Andrew T. Fisher, Dustin M. Winslow,