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SuSu Knolls hydrothermal field

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Journal Article
Journal: Economic Geology
Published: 01 December 2014
Economic Geology (2014) 109 (8): 2207-2226.
... high sulfidation epithermal mineralization. The SuSu Knolls hydrothermal field is a good example of a modern, high sulfidation, Cu-Au submarine hydrothermal system. Swath bathymetric mapping and video imagery show that the peaks of both North Su and South Su are spines, or ridges, steeply rising 40...
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Journal Article
Journal: Economic Geology
Published: 01 January 2007
Economic Geology (2007) 102 (1): 55-73.
...Elitsa Hrischeva; S. D. Scott; Ryan Weston Abstract Short sediment cores were examined from the active SuSu Knolls hydrothermal field in the eastern Manus back-arc basin, Papua New Guinea, in order to explain the origin of the currently accumulating metalliferous sediments. The mineralogy...
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Image
Map of the <b>SuSu</b> <b>Knolls</b> <b>hydrothermal</b> <b>field</b> showing the active Suzette, North...
Published: 01 January 2007
F ig . 2. Map of the SuSu Knolls hydrothermal field showing the active Suzette, North Su and South Su vent sites (redrawn and modified from Binns, 2004 , and Nautilus Minerals Inc., unpub.). The locations of the two cores and the dredge taken at the Suzette site are also shown.
Journal Article
Published: 01 August 2001
The Canadian Mineralogist (2001) 39 (4): 957-978.
...Roger Moss; Steven D. Scott Abstract Three of the five hydrothermal vent fields currently known in the Manus back-arc basin of Papua New Guinea are enriched in gold. Samples of precipitates from the PACMANUS and Susu Knolls hydrothermal fields in eastern Manus Basin contain up to 56.8 ppm gold...
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Image
Bathymetry (20-m contour intervals) and geology of the <b>SuSu</b> <b>Knolls</b> hydrothe...
Published: 01 December 2014
Fig. 2 Bathymetry (20-m contour intervals) and geology of the SuSu Knolls hydrothermal field. Bathymetry modified from Binns et al. (1997) .
Journal Article
Journal: Economic Geology
Published: 01 June 2017
Economic Geology (2017) 112 (4): 741-773.
... mechanisms, or maturity of the deposits ( Hannington et al., 1986 ). Local enrichment in metals may arise from seafloor oxidation: for instance, Au is concentrated by a factor of three in oxidized Cu chimneys from the Snake Pit hydrothermal field, Mid-Atlantic Ridge ( Fouquet et al., 1993b ). Ancient massive...
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Journal Article
Journal: Economic Geology
Published: 01 December 2014
Economic Geology (2014) 109 (8): 2227-2242.
... by transform fault zones to the east and west ( Crook et al., 1990 ; Binns and Scott, 1993 ). The active and inactive vent fields in the Suzette area are located at the northwestern end of a NW-trending edifice which contains the three, 1- to 1.5-km-diameter dacite domes comprising SuSu Knolls ( Binns et...
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Journal Article
Journal: Economic Geology
Published: 01 February 2019
Economic Geology (2019) 114 (1): 165-176.
... formed due to previous subduction ( Binns and Scott, 1993 ). A large number of hydrothermal fields have developed in the eastern Manus basin, with major hydrothermal fields including PACMANUS (Papua New Guinea-Australia-Canada-Manus basin), Desmos, and SuSu Knolls ( Fig. 1B ) ( Binns et al., 1995 , 2007...
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Journal Article
Journal: Economic Geology
Published: 01 September 2005
Economic Geology (2005) 100 (6): 1085-1096.
... fields and extensive sulfide deposits are found at PACMANUS, Desmos, and Susu knolls ( Sakai, 1990 ; Binns and Scott, 1993 , Scott and Binns, 1995 ; Auzende et al., 1996a , b ; Gamo et al., 1996 ; Gemmell et al., 1996 ; Binns et al., 1997 ). At PACMANUS, the focus of this study, hydrothermal...
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Journal Article
Journal: Economic Geology
Published: 01 August 2002
Economic Geology (2002) 97 (5): 1079-1100.
... Manus basin, back-arc extension occurs in remnant island-arc crust formed during earlier southward subduction along the Manus trench system ( Fig. 1A ). Active hydrothermal fields and extensive sulfide deposits ( Fig. 1B ) found at PACMANUS, Desmos, and Susu Knolls have been well studied ( Binns...
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Series: Economic Geology
Published: 01 January 2005
DOI: 10.5382/AV100.06
EISBN: 9781934969519
... mapping, and in some cases drilling, indicates that a number of deposits contain 1 to 5 million tons (Mt) of massive sulfide (e.g., TAG hydrothermal field on the Mid-Atlantic Ridge, deposits of the Galapagos Rift, and at 13°N on the East Pacific Rise). Two sediment-hosted deposits, at Middle Valley...
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Journal Article
Journal: Geology
Published: 01 September 2003
Geology (2003) 31 (9): 805-808.
... element contents of anhydrite from the PACMANUS subseafloor hydrothermal system , Manus Basin, Papua New Guinea : Mineralium Deposita (in press) . Binns , R.A. , Scott , S.D. , Gemmell , J.B. , and Crook , K.A.W.C. , Shipboard Party, 1997 , The SuSu Knolls hydrothermal field...
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Journal Article
Journal: Economic Geology
Published: 01 January 2001
Economic Geology (2001) 96 (1): 91-107.
... wall ( Auzende et al., 1996a , b ; Gena et al., 1998 ). The Susu Knolls hydrothermal field is situated to the east of the PACMANUS hydrothermal field and consists of three distinct vent sites, each near the crest of a knoll, at the southwestern end of Tumai Ridge ( Fig. 2 ). T ABLE 4...
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Journal Article
Journal: Economic Geology
Published: 01 December 2014
Economic Geology (2014) 109 (8): 2261-2292.
... Fe oxyhydroxides ( Fig. 2C ) and possible weak hydrothermal venting ( Fig. 2D ). The two fields of lobate lava flows noted above also coincide with high backscatter, as do the fissure-associated ridges on the southeastern flank of the cone ( Fig. 1D ). The equivalent magnetization map for Clark...
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Journal Article
Journal: Economic Geology
Published: 01 December 2014
Economic Geology (2014) 109 (8): 2079-2101.
... of the shallow-marine environment, but available data on Hg is limited at present. † Corresponding author: e-mail, tmonecke@mines.edu Another large hydrothermal system in the Okinawa trough is the Iheya North Knoll vent field, which is located at a water depth of 970 to 1,000 m. The field has...
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Image
The 1996 upper and lower particulate plumes and 1997 upper plume emanating ...
Published: 01 January 2007
F ig . 3. The 1996 upper and lower particulate plumes and 1997 upper plume emanating from the SuSu Knolls hydrothermal field. Data are from the 1996 PACMANUS III cruise report ( Parr and Binns, 1997 ) and the unpublished 1997 PACMANUS IV cruise report. Heavy contours outline the vent sites
Journal Article
Journal: Economic Geology
Published: 01 December 2004
Economic Geology (2004) 99 (8): 1711-1725.
... component in the hydrothermal fluid (Gemmell et al. 1996; J. B. Gemmell. unpub. data). Samples from another hydrothermal site in the eastern Manus basin, SuSu Knoll, have δ 34 S values of sulfides –3 to 0 per mil ( n = 13) for sulfides and –7 to +2 per mil ( n = 13) for native sulfur...
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Series: Reviews in Economic Geology
Published: 01 January 2016
DOI: 10.5382/Rev.18.11
EISBN: 9781629490922
... 180 Hatoma knoll, Okinawa trough 7 182 Pacmanus, Manus basin 23-4,000 98-5,717 187 Solwara 1, Manus basin 85-800 178-750 188 SuSu, Manus basin 13-160 105-13,000...
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Image
Regional setting (inset) after  Benes et al. (1994)  and geology of the eas...
Published: 01 January 2007
F ig . 1. Regional setting (inset) after Benes et al. (1994) and geology of the eastern Manus back-arc basin after Binns et al. (1995) . The locations of the two major hydrothermal fields, PACMANUS and SuSu Knolls, as well as the sediment cores used in this study are shown.
Journal Article
Journal: Economic Geology
Published: 01 December 2014
Economic Geology (2014) 109 (8): 2073-2077.
... dominated by seawater-derived hydrothermal fluids (e.g., the modern system at the Clark volcano and parts of the East Diamante field), to more focused, acid, magmatic-hydrothermal systems (e.g., SuSu knolls of the Manus basin and the Palinuro volcano of the Aeolian arc). The type of mineralization formed...
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