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Zarembo Island

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Journal Article
Published: 31 March 2004
Canadian Journal of Earth Sciences (2004) 41 (4): 355–375.
...Jennifer Lindline; William A. Crawford; Maria Luisa Crawford Abstract The Zarembo Island volcanic rocks and the Burnett Inlet plutonic complex in central southeastern Alaska were investigated to determine if they are genetically related. The Zarembo Island volcanic suite consists of basalt...
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Mafic magmatic enclaves in flow-banded rhyolite, western Zarembo Island. The ovoid shape and preferred orientation of the inclusions suggest that the mafic enclaves were transported as plastic droplets of magma in the rhyolite flow. White specks on the outcrop are barnacles. Hammer for scale.
Published: 31 March 2004
Fig. 3. Mafic magmatic enclaves in flow-banded rhyolite, western Zarembo Island. The ovoid shape and preferred orientation of the inclusions suggest that the mafic enclaves were transported as plastic droplets of magma in the rhyolite flow. White specks on the outcrop are barnacles. Hammer
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Metre-wide andesite columns at Macnamara Point, southern Zarembo Island. The andesite layering is shallowly dipping to the northeast.
Published: 31 March 2004
Fig. 4. Metre-wide andesite columns at Macnamara Point, southern Zarembo Island. The andesite layering is shallowly dipping to the northeast.
Image
Outcrop view of subhorizontal volcanic layering, Zarembo Island. The very fine-grained fragmental lower unit is rich in clay and interpreted as an ash-fall deposit. The upper massive unit is a basalt flow. Hammer for scale.
Published: 31 March 2004
Fig. 5. Outcrop view of subhorizontal volcanic layering, Zarembo Island. The very fine-grained fragmental lower unit is rich in clay and interpreted as an ash-fall deposit. The upper massive unit is a basalt flow. Hammer for scale.
Image
Plot of alkali oxides versus SiO2 (in wt.%) comparing magma compositions represented in the Zarembo Island volcanic suite and in the Deer Island – Etolin Island intrusive complex. Descrimination style from LeBas et al. (1986). Rocks from the Zarembo Island – Burnett Inlet volcanic–plutonic complex define a generally bimodal suite with a gap in silica concentrations at 60–65 wt.%.
Published: 31 March 2004
Fig. 14. Plot of alkali oxides versus SiO 2 (in wt.%) comparing magma compositions represented in the Zarembo Island volcanic suite and in the Deer Island – Etolin Island intrusive complex. Descrimination style from LeBas et al. (1986). Rocks from the Zarembo Island – Burnett Inlet volcanic
Journal Article
Journal: Geology
Published: 01 December 2004
Geology (2004) 32 (12): 1061–1064.
.... 17901 - 17916 . Karl , S.M. , Haeussler , P.J. , and McCafferty , A. , 1999 , Reconnaissance geologic map of the Duncan Canal–Zarembo Island area, southeastern Alaska : U.S. Geological Survey Open-File Report 99-168 , 30 p. Klepeis , K.A. , and Crawford , M.L...
FIGURES
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(A) through (N). Photographs of outcrops and polished rock slabs from mineral occurrences of the Alexander Triassic metallogenic belt. A. Pervasive orange-black, hydrothermal iron and manganese alteration of the Nehenta limestone and carbonate debris flows in Nehenta Bay, southern Gravina Island. Note the pod-shaped occurrence of bladed white barite and minor sulfides to the right of the hammer. B. Altered gabbroic sill beneath barite-sulfide pod. Berg 17 occurrence, Sylburn peninsula, Annette Island. C. Massive vein of pink and white barite cutting clastic sedimentary rocks and limestone at the top of the Keku rhyolite. Note the botryoidal banding defined by fine galena. Northeastern shoreline of the Cornwallis peninsula on Kuiu Island, Keku Strait area, central southeastern Alaska. D. Mineralized Cornwallis limestone breccia from the Kuiu Zinc deposit on the Cornwallis peninsula. The matrix to the clast is composed of sphalerite, galena, and Fe-Mn carbonate. E. Mineralized limestone from the top of the open cut at the Taylor Creek occurrence, Duncan Canal, central southeastern Alaska. The sample contains pyrite, sphalerite, galena, and tetrahedrite in irregular veins and as replacements of limestone, with a white dolomite gangue. F. Nodular pyrite in limestone near the Taylor Creek open cut. This texture is interpreted to be the result of early diagenetic replacement of carbonate mud. G. Barite-galena–rich material from the Castle Island barite mine in the Duncan Canal area, central southeastern Alaska. H. Glacier Creek (Main) deposit in the Mount Henry Clay area, northern southeastern Alaska. The central, orange-white zone consists of quartz-sericite-carbonate schist with lenses of massive barite and lesser sulfides. The outcrop above and below consists of massive and pillowed basalt flows. I. Barite-sulfide lens at the Upper Cap occurrence in the Mount Henry Clay area, northern southeastern Alaska. Rocks overlying the lens are massive basalt flows. J. South side of Windy Peak at the Windy Craggy deposit in northwestern British Columbia. Light and dark subhorizontal layering comprises intercalated mafic sills and flows with calcareous black argillites. K. Typical pyritic massive sulfide with minor pyrrhotite and chalcopyrite in a quartz-carbonate gangue, from the north crosscut of the Windy Craggy deposit in northwestern British Columbia. The black elongate inclusion in the lower right part of the sample is an argillite clast. L. Pyrite- and sphalerite-rich massive sulfide from a boulder found at the Mount Henry Clay (Boulderado) occurrence in northern southeastern Alaska. M. Massive sulfide lens at the Frenchie deposit on Zarembo Island, central southeastern Alaska. Timbers in the adit are ~2 m high and are holding up a hanging wall of graphitic quartz-sericite schist. N. Samples from the Frenchie deposit. Left sample is dominantly pyritic with some chalcopyrite and characterizes the majority of the sulfide lens. The center sample is more sphalerite and galena rich; the right sample has significant barite typical of the distal portion of the lens.
Published: 01 January 2008
in the lower right part of the sample is an argillite clast. L. Pyrite- and sphalerite-rich massive sulfide from a boulder found at the Mount Henry Clay (Boulderado) occurrence in northern southeastern Alaska. M. Massive sulfide lens at the Frenchie deposit on Zarembo Island, central southeastern Alaska
Image
(A) through (N). Photographs of outcrops and polished rock slabs from mineral occurrences of the Alexander Triassic metallogenic belt. A. Pervasive orange-black, hydrothermal iron and manganese alteration of the Nehenta limestone and carbonate debris flows in Nehenta Bay, southern Gravina Island. Note the pod-shaped occurrence of bladed white barite and minor sulfides to the right of the hammer. B. Altered gabbroic sill beneath barite-sulfide pod. Berg 17 occurrence, Sylburn peninsula, Annette Island. C. Massive vein of pink and white barite cutting clastic sedimentary rocks and limestone at the top of the Keku rhyolite. Note the botryoidal banding defined by fine galena. Northeastern shoreline of the Cornwallis peninsula on Kuiu Island, Keku Strait area, central southeastern Alaska. D. Mineralized Cornwallis limestone breccia from the Kuiu Zinc deposit on the Cornwallis peninsula. The matrix to the clast is composed of sphalerite, galena, and Fe-Mn carbonate. E. Mineralized limestone from the top of the open cut at the Taylor Creek occurrence, Duncan Canal, central southeastern Alaska. The sample contains pyrite, sphalerite, galena, and tetrahedrite in irregular veins and as replacements of limestone, with a white dolomite gangue. F. Nodular pyrite in limestone near the Taylor Creek open cut. This texture is interpreted to be the result of early diagenetic replacement of carbonate mud. G. Barite-galena–rich material from the Castle Island barite mine in the Duncan Canal area, central southeastern Alaska. H. Glacier Creek (Main) deposit in the Mount Henry Clay area, northern southeastern Alaska. The central, orange-white zone consists of quartz-sericite-carbonate schist with lenses of massive barite and lesser sulfides. The outcrop above and below consists of massive and pillowed basalt flows. I. Barite-sulfide lens at the Upper Cap occurrence in the Mount Henry Clay area, northern southeastern Alaska. Rocks overlying the lens are massive basalt flows. J. South side of Windy Peak at the Windy Craggy deposit in northwestern British Columbia. Light and dark subhorizontal layering comprises intercalated mafic sills and flows with calcareous black argillites. K. Typical pyritic massive sulfide with minor pyrrhotite and chalcopyrite in a quartz-carbonate gangue, from the north crosscut of the Windy Craggy deposit in northwestern British Columbia. The black elongate inclusion in the lower right part of the sample is an argillite clast. L. Pyrite- and sphalerite-rich massive sulfide from a boulder found at the Mount Henry Clay (Boulderado) occurrence in northern southeastern Alaska. M. Massive sulfide lens at the Frenchie deposit on Zarembo Island, central southeastern Alaska. Timbers in the adit are ~2 m high and are holding up a hanging wall of graphitic quartz-sericite schist. N. Samples from the Frenchie deposit. Left sample is dominantly pyritic with some chalcopyrite and characterizes the majority of the sulfide lens. The center sample is more sphalerite and galena rich; the right sample has significant barite typical of the distal portion of the lens.
Published: 01 January 2008
in the lower right part of the sample is an argillite clast. L. Pyrite- and sphalerite-rich massive sulfide from a boulder found at the Mount Henry Clay (Boulderado) occurrence in northern southeastern Alaska. M. Massive sulfide lens at the Frenchie deposit on Zarembo Island, central southeastern Alaska
Journal Article
Published: 29 September 2005
Canadian Journal of Earth Sciences (2005) 42 (6): 1097–1116.
... and biotite. On Wrangell Island to the north and on Woronkofski and Zarembo islands to the west outcrop 93–90 Ma rocks, hereafter referred to as the Northern plutons, chemically and petrographically similar to the eastern portions of the Bell Island pluton. These ∼90 Ma tonalite plutons are enriched...
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Journal Article
Journal: Economic Geology
Published: 01 January 2008
Economic Geology (2008) 103 (1): 89–115.
... in the lower right part of the sample is an argillite clast. L. Pyrite- and sphalerite-rich massive sulfide from a boulder found at the Mount Henry Clay (Boulderado) occurrence in northern southeastern Alaska. M. Massive sulfide lens at the Frenchie deposit on Zarembo Island, central southeastern Alaska...
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Journal Article
Published: 01 March 2009
The Journal of Geology (2009) 117 (2): 156–173.
... ), and the emplacement of the Burnett Inlet intrusive complex and Zarembo Island volcanics from ∼26 to 17 Ma (Crawford and Crawford 1991 ; Lindline et al. 2004 ). This timing agrees with K-Ar biotite ages of 25.6–17.3 Ma (Brew et al. 1984 ) from shallow-level plutonic rocks on Kupreanof, Zarembo, and Etolin...
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Journal Article
Published: 01 April 2001
Bulletin of the Seismological Society of America (2001) 91 (2): 381–396.
... )〉 of oscillations on the surface, which is in agreement with the theory of nonlinear wave interactions ( Zarembo and Krasil'nikov, 1966 ), and they are presented in Table 1 . This means that horizontal displacements of points on the surface in positive and negative directions are different, that is, subsurface...
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Journal Article
Published: 01 December 2006
Bulletin of the Seismological Society of America (2006) 96 (6): 2131–2145.
... , 218 – 244 . Zarembo , L. K. , and V. A. Krasil’nikov ( 1966 ). Introduction to Nonlinear Acoustics , Nauka , Moscow . Zvolinskii , N. V. ( 1982 ). Wave processes in non-elastic media , Prob. Eng. Seism. 23 , 4 – 19 . As known, there are three basic mechanisms...
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Journal Article
Published: 22 January 2013
Canadian Journal of Earth Sciences (2013) 50 (6): 678–691.
...., Haeussler, P.J., and McCafferty, A. 1999. Reconnaissance geologic map of the Duncan Canal-Zarembo Island area, southeastern Alaska. U.S. Geological Survey Open-File Report 99-168, scale 1:250,000. Lanphere, M.A., MacKevett, E.M., and Stern, T.W. 1964. Potassium-argon and lead-alpha ages of plutonic rocks...
Journal Article
Published: 27 January 2004
Canadian Journal of Earth Sciences (2004) 41 (1): 87–102.
... and implications for Late Cretaceous to early Eocene tectonics in southeastern Alaska and British Columbia . Geological Society of America Bulletin , 106 : 715 – 728 . Karl S.M. Haeussler P.J. McCafferty A. 1999 . Reconnaissance geologic map of the Duncan Canal-Zarembo Island area, south...
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Journal Article
Published: 01 February 2016
American Mineralogist (2016) 101 (2): 297–310.
...-plutonic system: the Zarembo Island extrusive suite and the Burnett Inlet intrusive complex . Canadian Journal of Earth Sciences , 41 , 355 – 375 . Lipman P.W. Christiansen R.L. O’Connor J.T. ( 1966 ) A compositionally zoned ash-flow sheet in southern Nevada . United States...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 October 2013
Lithosphere (2013) 5 (5): 521–536.
...>2.0.CO;2 . Lindline J. Crawford W.A. Crawford M.L. , 2004 , A bimodal volcanic–plutonic system: The Zarembo Island extrusive suite and the Burnett Inlet intrusive complex : Canadian Journal of Earth Sciences , v. 41 , no. 4 , p. 355 – 375 , doi:10.1139/e04-009...
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Journal Article
Published: 18 July 2016
Canadian Journal of Earth Sciences (2016) 53 (12): 1458–1475.
... and Admiralty nomenclature, but include stratigraphy from the St. Elias mountains of northwest British Columbia and southwest Yukon in the regional discussion. The Admiralty subterrane, the focus of this paper, is found on Admiralty Island, the western half of Kupreanof Island, and possibly on parts of Zarembo...
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Journal Article
Published: 21 March 2018
Canadian Journal of Earth Sciences (2018) 55 (6): 545–570.
... Grenville Province . Canadian Journal of Earth Sciences , 51 ( 6 ): 558 – 572 . 10.1139/cjes-2013-0170 . Lindline , J. , Crawford , W.A. , and Crawford , M.L. 2004 . A bimodal volcanic–plutonic system: the Zarembo Island extrusive suite and the Burnett Inlet intrusive complex...
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Journal Article
Journal: SEG Discovery
Published: 01 July 1996
SEG Discovery (1996) (26): 1–44.
... loading facilities. To date Cominco has invested over $500 million in Red Dog, including $290 million in the WestMin drilled the Frenchie prospect VMS on Zarembo Island. mine and mill; $30 million in pre-lease exploration, and the They are also active on Admiralty Island in an area believed...