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Burnett Inlet

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Journal Article

A bimodal volcanic–plutonic system: the Zarembo Island extrusive suite and the Burnett Inlet intrusive complex Available to Purchase

Jennifer Lindline, William A. Crawford, Maria Luisa Crawford
Published: 31 March 2004
Canadian Journal of Earth Sciences (2004) 41 (4): 355–375.
DOI: https://doi.org/10.1139/e04-009
...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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View PDF for article title, A bimodal volcanic–plutonic system: the Zarembo Island extrusive suite and the <span class="search-highlight">Burnett</span> <span class="search-highlight">Inlet</span> intrusive complex
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Densely packed mafic magmatic enclaves, Burnett Inlet.

Densely packed mafic magmatic enclaves, Burnett Inlet. Available to Purchase

Published: 31 March 2004
Fig. 12. Densely packed mafic magmatic enclaves, Burnett Inlet.
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Rb-Sr ISOTROPIC DATA FOR SELECTED BURNETT INLET IGNEOUS COMPLEX ROCKS, SOUT... Available to Purchase

Published: 01 August 2000
TABLE 2. Rb-Sr ISOTROPIC DATA FOR SELECTED BURNETT INLET IGNEOUS COMPLEX ROCKS, SOUTHEASTERN ALASKA
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Element-variation diagrams for Burnett Inlet Igneous Complex rocks. On facing page, weight % major-element oxides versus weight % SiO2. Above, concentrations of trace elements (ppm) versus weight % SiO2. Solid squares: gabbro–diorite, solid circles: enclaves, open squares, granite and alkali granite, open circles: felsic phase in composite zones.

Element-variation diagrams for Burnett Inlet Igneous Complex rocks. On faci... Available to Purchase

Published: 01 August 2000
F ig . 7. Element-variation diagrams for Burnett Inlet Igneous Complex rocks. On facing page, weight % major-element oxides versus weight % SiO 2 . Above, concentrations of trace elements (ppm) versus weight % SiO 2 . Solid squares: gabbro–diorite, solid circles: enclaves, open squares
Image
Element-variation diagrams for Burnett Inlet Igneous Complex rocks. On facing page, weight % major-element oxides versus weight % SiO2. Above, concentrations of trace elements (ppm) versus weight % SiO2. Solid squares: gabbro–diorite, solid circles: enclaves, open squares, granite and alkali granite, open circles: felsic phase in composite zones.

Element-variation diagrams for Burnett Inlet Igneous Complex rocks. On faci... Available to Purchase

Published: 01 August 2000
F ig . 7. Element-variation diagrams for Burnett Inlet Igneous Complex rocks. On facing page, weight % major-element oxides versus weight % SiO 2 . Above, concentrations of trace elements (ppm) versus weight % SiO 2 . Solid squares: gabbro–diorite, solid circles: enclaves, open squares
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Chondrite-normalized rare-earth-element diagrams for Burnett Inlet Igneous Complex rocks. Chondrite-normalization values from Nakamura (1974).

Chondrite-normalized rare-earth-element diagrams for Burnett Inlet Igneous ... Available to Purchase

Published: 01 August 2000
F ig . 8. Chondrite-normalized rare-earth-element diagrams for Burnett Inlet Igneous Complex rocks. Chondrite-normalization values from Nakamura (1974) .
Journal Article

POST-ACCRETION MAGMATISM WITHIN THE KUIU–ETOLIN IGNEOUS BELT, SOUTHEASTERN ALASKA Available to Purchase

Jennifer Lindline, William A. Crawford, Maria Luisa Crawford, Gomaa I. Omar
Published: 01 August 2000
The Canadian Mineralogist (2000) 38 (4): 951–974.
DOI: https://doi.org/10.2113/gscanmin.38.4.951
...TABLE 2. Rb-Sr ISOTROPIC DATA FOR SELECTED BURNETT INLET IGNEOUS COMPLEX ROCKS, SOUTHEASTERN ALASKA ...
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View PDF for article title, POST-ACCRETION MAGMATISM WITHIN THE KUIU–ETOLIN IGNEOUS BELT, SOUTHEASTERN ALASKA
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Schematic illustration of the formation and emplacement of the Burnett Inlet Igneous Complex. Numbers are discussed in text.

Schematic illustration of the formation and emplacement of the Burnett Inle... Available to Purchase

Published: 01 August 2000
F ig . 15. Schematic illustration of the formation and emplacement of the Burnett Inlet Igneous Complex. Numbers are discussed in text.
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WHOLE-ROCK GEOCHEMISTRY AND MODAL DATA FOR REPRESENTATIVE SAMPLES OF THE BU... Available to Purchase

Published: 01 August 2000
TABLE 1. WHOLE-ROCK GEOCHEMISTRY AND MODAL DATA FOR REPRESENTATIVE SAMPLES OF THE BURNETT INLET IGNEOUS COMPLEX, SOUTHEASTERN ALASKA
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Whole-rock Rb–Sr isotope data for selected gabbroic (solid squares) and granitic (open squares) rocks from the Burnett Inlet Igneous Complex. Data for the granitic rocks form an isochron indicating a crystallization age of 22.47 million years and a y-intercept (SIR) of 0.7047.

Whole-rock Rb–Sr isotope data for selected gabbroic (solid squares) and gra... Available to Purchase

Published: 01 August 2000
F ig . 4. Whole-rock Rb–Sr isotope data for selected gabbroic (solid squares) and granitic (open squares) rocks from the Burnett Inlet Igneous Complex. Data for the granitic rocks form an isochron indicating a crystallization age of 22.47 million years and a y -intercept (SIR) of 0.7047.
Image
A. Outcrop view of abundant mafic magmatic enclaves in granite, southwestern Burnett Inlet. Note various sizes and shapes of enclaves and the serrated edge of lower enclave. B. Pillow-like mafic magmatic enclaves with intervening leucocratic material from within gabbro unit, southeast Deer Island.

A. Outcrop view of abundant mafic magmatic enclaves in granite, southwester... Available to Purchase

Published: 01 August 2000
F ig . 3. A. Outcrop view of abundant mafic magmatic enclaves in granite, southwestern Burnett Inlet. Note various sizes and shapes of enclaves and the serrated edge of lower enclave. B. Pillow-like mafic magmatic enclaves with intervening leucocratic material from within gabbro unit, southeast
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A. Outcrop view of abundant mafic magmatic enclaves in granite, southwestern Burnett Inlet. Note various sizes and shapes of enclaves and the serrated edge of lower enclave. B. Pillow-like mafic magmatic enclaves with intervening leucocratic material from within gabbro unit, southeast Deer Island.

A. Outcrop view of abundant mafic magmatic enclaves in granite, southwester... Available to Purchase

Published: 01 August 2000
F ig . 3. A. Outcrop view of abundant mafic magmatic enclaves in granite, southwestern Burnett Inlet. Note various sizes and shapes of enclaves and the serrated edge of lower enclave. B. Pillow-like mafic magmatic enclaves with intervening leucocratic material from within gabbro unit, southeast
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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.%.

Plot of alkali oxides versus SiO 2 (in wt.%) comparing magma compositions ... Available to Purchase

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
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Map of lithotectonic units in southeastern Alaska after Wheeler et al.(1991) and location of the Kuiu–Etolin magmatic belt (Brew 1994, Brew &amp; Morrell 1983, Brew et al. 1984). A box encloses the Burnett Inlet Igneous Complex. Larger towns and features are noted (K: Ketchikan, W: Wrangell, P: Petersburg, S: Sitka, J: Juneau, Q: Quartz Hill).

Map of lithotectonic units in southeastern Alaska after Wheeler et al. (1... Available to Purchase

Published: 01 August 2000
F ig . 1. Map of lithotectonic units in southeastern Alaska after Wheeler et al. (1991) and location of the Kuiu–Etolin magmatic belt ( Brew 1994 , Brew & Morrell 1983 , Brew et al. 1984 ). A box encloses the Burnett Inlet Igneous Complex. Larger towns and features are noted (K
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A through E. Frequency distribution of the lengths of confined spontaneous fission tracks in apatite. Ages and frequency-distribution data are shown in upper left-hand corner of histograms. AGE: fission track age determined by external detector method, X: mean fission-track length, SD: standard deviation, SE: standard error for average, N: number of grains. F. Apparent cooling history for the Burnett Inlet Igneous Complex. Closure temperature – age curve is best fit to available data. Uncertainties in ages and closure temperatures are shown by error bars through symbols. Sources of age data: K/Ar ages: Douglass et al.(1989); Rb/Sr whole-rock age: this study; apatite FT ages: this study. Closure temperatures: biotite K/Ar: 280°C ± 40; hornblende K/Ar: 530°C ± 40; whole-rock Rb/Sr: 700°C ± 75; apatite fission-track: 105°C ± 10 (Gleadow &amp; Brooks 1979, Harrison et al. 1979, Harrison &amp; McDougall 1980). Closure temperature values are considered broadly applicable to relatively high rates of cooling.

A through E. Frequency distribution of the lengths of confined spontaneous ... Available to Purchase

Published: 01 August 2000
: standard deviation, SE: standard error for average, N: number of grains. F. Apparent cooling history for the Burnett Inlet Igneous Complex. Closure temperature – age curve is best fit to available data. Uncertainties in ages and closure temperatures are shown by error bars through symbols. Sources of age
Journal Article

NEW NOMENCLATURE FOR ORDOVICIAN ROCK UNITS OF TH E EASTERN AND SOUTHERN QUEEN ELIZABETH ISLANDS, ARCTIC CANADA Available to Purchase

J. William Kerr
Published: 01 March 1967
Bulletin of Canadian Petroleum Geology (1967) 15 (1): 91–113.
DOI: https://doi.org/10.35767/gscpgbull.15.1.091
... (Thorsteinsson and Glenister, 1963, p . 587) 2,70 0 Devon Island 22 Burnett Inlet (Glenister, 1963a, p . 182) 1,040 + 21 Herschel Bay and Rigby Bay (Glenister and Thorsteinsson , 1963, p . 197) 820 + 18 Naughton Dome (Greiner, 1963, p . 208) 1,040-1 - 14 Prince Alfred Bay (Thorsteinsson, 1963b, p . 224) 2,200...
View PDF for article title, NEW NOMENCLATURE FOR ORDOVICIAN ROCK UNITS OF TH E EASTERN AND SOUTHERN QUEEN ELIZABETH ISLANDS, ARCTIC CANADA
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Journal Article

THE MIDDLE-UPPER DEVONIAN CLASTIC WEDGE OF THE FRANKLINIAN GEOSYNCLINE Available to Purchase

Ashton F. Embry, J. Edward Klovan
Published: 01 December 1976
Bulletin of Canadian Petroleum Geology (1976) 24 (4): 485–639.
DOI: https://doi.org/10.35767/gscpgbull.24.4.485
... Inlet Fm and Parry Islands Fm is almost always readily recognizable on airphotos. 568 ASHTON EMBRY and J. EDWARD KLOVAN o 0 61B 770M ~ ~ 0 c~ PARRY ISLANDS FORMATION AT SURFACE OR IN SUBSUR- FACE 2C~KM I I Fig. 36. Distribution and thickness of Parry Islands Fro. About 320 m (1,050 ft) of the Burnett...
View PDF for article title, THE MIDDLE-UPPER DEVONIAN CLASTIC WEDGE OF THE FRANKLINIAN GEOSYNCLINE
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Journal Article

Neogene tilting of crustal panels near Wrangell, Alaska Available to Purchase

Chris Butzer, Robert F. Butler, George E. Gehrels, Cameron Davidson, Kristin O'Connell, Maria Luisa Crawford
Journal: Geology
Published: 01 December 2004
Geology (2004) 32 (12): 1061–1064.
DOI: https://doi.org/10.1130/G20855.1
... igneous belt, southeastern Alaska: Canadian Mineralogist , v. 38 p. 951 - 974 . 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: Canadian Journal of Earth...
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Journal Article

Revisiting groundwater carbon fluxes to the ocean with implications for the carbon cycle Available to Purchase

Shuang Zhang, Noah J. Planavsky
Journal: Geology
Published: 13 November 2019
Geology (2020) 48 (1): 67–71.
DOI: https://doi.org/10.1130/G46408.1
... that groundwater fluxes may be a critical component of water and element budgets ( Church, 1996 ; Cai et al., 2003 ; Burnett et al., 2003 ; Moore et al., 2008 ; Schopka and Derry, 2012 ; Duvert et al., 2018 ). Therefore, carbon dioxide consumption through water-rock reaction in the subsurface system might...
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Journal Article

Melvillipteris quadriseriata gen. et sp. nov., a new plant assigned to Rhacophytales from the Upper Devonian (Famennian) of Arctic Canada Available to Purchase

JIN-ZHUANG XUE, JAMES F. BASINGER
Published: 14 October 2015
Geological Magazine (2016) 153 (4): 601–617.
DOI: https://doi.org/10.1017/S0016756815000746
... of the Cape Fortune Member near Beverley Inlet, conodont assemblages in the lower part of the section represent the crepida Zone of the early Famennian. As the beds bearing our fossil plants occur in the upper part of the Burnett Point Member, and c . 30m below the base of the Cape Fortune...
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View PDF for article title, Melvillipteris quadriseriata gen. et sp. nov., a new plant assigned to Rhacophytales from the Upper Devonian (Famennian) of Arctic Canada
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