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Extreme hydrothermal conditions at an active plate-bounding fault.

Nature

Sutherland R, Townend J, Toy V, Upton P, Coussens J, Allen M, Baratin LM, Barth N, Becroft L, Boese C, Boles A, Boulton C, Broderick NGR, Janku-Capova L, Carpenter BM, Célérier B, Chamberlain C, Cooper A, Coutts A, Cox S, Craw L, Doan ML, Eccles J, Faulkner D, Grieve J, Grochowski J, Gulley A, Hartog A, Howarth J, Jacobs K, Jeppson T, Kato N, Keys S, Kirilova M, Kometani Y, Langridge R, Lin W, Little T, Lukacs A, Mallyon D, Mariani E, Massiot C, Mathewson L, Melosh B, Menzies C, Moore J, Morales L, Morgan C, Mori H, Niemeijer A, Nishikawa O, Prior D, Sauer K, Savage M, Schleicher A, Schmitt DR, Shigematsu N, Taylor-Offord S, Teagle D, Tobin H, Valdez R, Weaver K, Wiersberg T, Williams J, Woodman N, Zimmer M.
PMID: 28514440
Nature. 2017 Jun 01;546(7656):137-140. doi: 10.1038/nature22355. Epub 2017 May 17.

Temperature and fluid pressure conditions control rock deformation and mineralization on geological faults, and hence the distribution of earthquakes. Typical intraplate continental crust has hydrostatic fluid pressure and a near-surface thermal gradient of 31 ± 15 degrees Celsius per...

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