Subsurface structure of a submarine hydrothermal system in ocean crust formed at the East Pacific Rise, ODP/IODP Site 1256

Author:

Alt Jeffrey C.1,Laverne Christine2,Coggon Rosalind M.,Teagle Damon A. H.3,Banerjee Neil R.4,Morgan Sally,Smith-Duque Christopher E.3,Harris Michelle3,Galli Laura1

Affiliation:

1. Department of Geological Sciences; University of Michigan; 1000 North University Avenue,; Ann Arbor; Michigan; 48109-1005; USA

2. Laboratoire de Pétrologie Magmatique, Faculté des Sciences de Marseille Saint Jérome; Université Paul Cézanne Aix-Marseille III; Case 441,; F-13397; Marseille CEDEX 20; France

3. School of Ocean and Earth Science, National Oceanography Centre, Southampton; University of Southampton; European Way,; Southampton; SO14 3ZH; UK

4. Department of Earth Sciences; University of Western Ontario; London, Ontario; N6A 5B7; Canada

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference83 articles.

1. Geophys. Monogr. Ser.;Alt,1995

2. The mineralogy and isotopic composition of sulfur in Layer 3 gabbros from the Indian Ocean, ODP Hole 735B;Alt;Proc. Ocean Drill. Program Sci. Results,1991

3. Chemical compositions of secondary minerals from Site 1256 basement, ODP Leg 206 [online];Alt;Proc. Ocean Drill. Program Sci. Results,2006

4. Spec. Pap. Geol. Soc. Am.;Alt,2000

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