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• W2000903803 abstract "Research Article| September 01, 2003 Contrasting evolution of hydrothermal fluids in the PACMANUS system, Manus Basin: The Sr and S isotope evidence S. Roberts; S. Roberts 1School of Ocean and Earth Science, Southampton Oceanography Centre, University of Southampton, Southampton SO14 3ZH, UK Search for other works by this author on: GSW Google Scholar W. Bach; W. Bach 2Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA Search for other works by this author on: GSW Google Scholar R.A. Binns; R.A. Binns 3Commonwealth Scientific and Industrial Research Organisation Exploration and Mining, P.O. Box 136, North Ryde, NSW 1670, Australia Search for other works by this author on: GSW Google Scholar D.A. Vanko; D.A. Vanko 4Department of Physics, Astronomy and Geosciences, Towson University, Towson, Maryland 21252, USA Search for other works by this author on: GSW Google Scholar C.J. Yeats; C.J. Yeats 5Commonwealth Scientific and Industrial Research Organisation Exploration and Mining, P.O. Box 136, North Ryde, NSW 1670, Australia Search for other works by this author on: GSW Google Scholar D.A.H. Teagle; D.A.H. Teagle 6School of Ocean and Earth Science, Southampton Oceanography Centre, University of Southampton, Southampton SO14 3ZH, UK Search for other works by this author on: GSW Google Scholar K. Blacklock; K. Blacklock 7Commonwealth Scientific and Industrial Research Organisation Petroleum Resources, P.O. Box 136, North Ryde, NSW 1670, Australia Search for other works by this author on: GSW Google Scholar J.S. Blusztajn; J.S. Blusztajn 8Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA Search for other works by this author on: GSW Google Scholar A.J. Boyce; A.J. Boyce 9Scottish Universities Environmental Research Centre, Rankine Avenue, East Kilbride G70 0QF, UK Search for other works by this author on: GSW Google Scholar M.J. Cooper; M.J. Cooper 10School of Ocean and Earth Science, Southampton Oceanography Centre, University of Southampton, Southampton SO14 3ZH, UK Search for other works by this author on: GSW Google Scholar N. Holland; N. Holland 10School of Ocean and Earth Science, Southampton Oceanography Centre, University of Southampton, Southampton SO14 3ZH, UK Search for other works by this author on: GSW Google Scholar B. McDonald B. McDonald 11Commonwealth Scientific and Industrial Research Organisation Exploration and Mining, P.O. Box 136, North Ryde, NSW 1670, Australia Search for other works by this author on: GSW Google Scholar Geology (2003) 31 (9): 805–808. https://doi.org/10.1130/G19716.1 Article history received: 02 Apr 2003 rev-recd: 05 May 2003 accepted: 11 May 2003 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation S. Roberts, W. Bach, R.A. Binns, D.A. Vanko, C.J. Yeats, D.A.H. Teagle, K. Blacklock, J.S. Blusztajn, A.J. Boyce, M.J. Cooper, N. Holland, B. McDonald; Contrasting evolution of hydrothermal fluids in the PACMANUS system, Manus Basin: The Sr and S isotope evidence. Geology 2003;; 31 (9): 805–808. doi: https://doi.org/10.1130/G19716.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Ocean Drilling Program (ODP) Leg 193 investigated two sites of hydrothermal activity along the crest of the Pual Ridge in the eastern Manus Basin. A site of low-temperature diffuse venting, Snowcap (Site 1188), and a high-temperature black smoker site, Roman Ruins (Site 1189), were drilled to depths of 386 and 206 m below seafloor (mbsf), respectively. Although the two sites are <1000 m apart, the 87Sr/86Sr and δ34S signatures of anhydrite recovered at both sites are very different. The data suggest a complex interplay among hydrothermal fluid, magmatic fluid, and seawater during alteration and mineralization of the PACMANUS (Papua New Guinea–Australia–Canada–Manus) system. These new results significantly expand the subsurface data on seafloor hydrothermal systems and may begin to explain the earliest processes of multistage mineralization and alteration history that typify ancient massive sulfide systems. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2000903803 title "Contrasting evolution of hydrothermal fluids in the PACMANUS system, Manus Basin: The Sr and S isotope evidence" @default.
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