Conference Proceedings
PACRIM Congress 2008
Conference Proceedings
PACRIM Congress 2008
The PACMANUS Seafloor Sulfide Field, Eastern Manus Basin, Papua New Guinea
Discovered in 1991 by combined plume detection and bottom-tow photography (Binns and Scott, 1993) and for some years thereafter the highest tenor mineral occurrence known on the ocean floor, the PACMANUS hydrothermal field has since been surveyed and sampled in great detail by CSIRO and international research agencies (Binns et al, 1995; Auzende, Urabe and Scientific Party, 1996; Binns et al, 2002; Tivey et al, 2006). Since 2005 commercial surveys employing deep-tow geophysical packages and remotely-operated vehicles (ROVs) have been conducted by Nautilus Minerals Inc and partners within Papua New Guinea-granted offshore exploration licenses (Nautilus Minerals Inc, 2008)._x000D_
Two academic drilling programs have been conducted, one under the international Ocean Drilling Program (ODP) directed at deep structure (Shipboard Scientific Party, 2002; Binns, Barriga and Miller, 2007), and one using a 5 m capable seafloor diamond drill to investigate the immediate subsurface at one site (Petersen et al, 2005)._x000D_
AnEXTENDED ABSTRACTis available for download. A full-length paper was notprepared for this presentation.
Two academic drilling programs have been conducted, one under the international Ocean Drilling Program (ODP) directed at deep structure (Shipboard Scientific Party, 2002; Binns, Barriga and Miller, 2007), and one using a 5 m capable seafloor diamond drill to investigate the immediate subsurface at one site (Petersen et al, 2005)._x000D_
AnEXTENDED ABSTRACTis available for download. A full-length paper was notprepared for this presentation.
Contributor(s):
R A Binns, J M Parr, C J Yeats
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- Published: 2008
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- Unique ID: P200811014