Abstract Details

CHANGES IN HYDROTHERMAL FLUID ORIGIN CONDITIONS LEADING UP TO THE NEXT ERUPTION AT 9 °50´N EAST PACIFIC RISE

MCDERMOTT, Jill1, DOWNING, Connor C.1, FORNARI, Daniel J.2, PARNELL-TURNER, Ross3 and BARREYRE, Thibaut4, (1)Department of Earth and Environmental Sciences, Lehigh University, Bethlehem, PA 18015, (2)Geology and Geophysics Department, Woods Hole Oceanographic Institution, 266 Woods Hole Rd, Woods Hole, MA 02543, (3)Scripps Institution of Oceanography, La Jolla, CA 92093-0225, (4)Department of Earth Science, University of Bergen, Bergen, 5020, Norway