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Flanagan Fault

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Image
Published: 01 January 2000
F ig . 8. Plan projections of (a) the Charlotte and (b) the Flanagan faults, showing the position of orebodies adjacent to the faults and the distribution of alteration types in the fault zone rocks. Drill hole intersections are flagged as containing sericite (+ albite) + ankerite + pyrite
Image
Distribution of alteration haloes in a composite vertical section through the Charlotte orebody (Q Drill Section) above, and the Charlotte Deeps orebody (136 Drill Section) below, the Flanagan Fault. Both sections cut approximately through the center of the vein stockwork, but are offset out of the plane of the figure owing to the displacement of the Unit 8 granophyre along the early Flanagan Fault (modified from Mikucki & Heinrich 1993).
Published: 01 October 2004
F ig . 5. Distribution of alteration haloes in a composite vertical section through the Charlotte orebody (Q Drill Section) above, and the Charlotte Deeps orebody (136 Drill Section) below, the Flanagan Fault. Both sections cut approximately through the center of the vein stockwork
Image
Published: 01 January 2000
extent and thickness. With steady flux, relatively low effective pressures develop below the Flanagan fault.
Image
Published: 01 January 2000
. (d). Photomicrograph of a stockwork vein, Charlotte Deeps orebody, 29 level, showing crack-seal texture in fibrous quartz adjacent to wall-rock contact. Cross-polarized light. (e). Flanagan fault, 28 level, Charlotte Deeps orebody, viewed to the southeast. Flat stockwork veins cut the fault fabric
Image
Published: 01 January 2000
to the Charlotte fault (area f), shallowly dipping veins adjacent to the Flanagan fault (area e), and a single set parallel to the acute bisectrix of the conjugate sets in unit 9 (area a, and less well marked in area c).
Image
Published: 01 January 2000
adjacent to the Northern, Charlotte, and Charlotte Deeps orebodies. Cross hatching shows the projection of the Flanagan fault between the base of the Charlotte orebody and the top of the Charlotte Deeps orebody. The grid in this and subsequent figures is the Kalgoorlie mine grid, with grid north 39° W
Image
The Mount Charlotte deposit in (a) plan view at the 3 level, (b) cross section at 52850 m N, and (c) schematic northwest–southeast long section projected onto 19900 m E. Regions shaded dark grey depict the area of the gold orebodies. The Charlotte fault appears three times on the long section to show its positions adjacent to the Northern Charlotte, and Charlotte Deeps orebodies. Cross hatching shows the projection of the Flanagan Fault between the base of the Charlotte orebody and the top of the Charlotte Deeps orebody. Illustration from Ridley & Mengler (2000, Fig. 2), reprinted with permission of Economic Geology.
Published: 01 October 2004
section to show its positions adjacent to the Northern Charlotte, and Charlotte Deeps orebodies. Cross hatching shows the projection of the Flanagan Fault between the base of the Charlotte orebody and the top of the Charlotte Deeps orebody. Illustration from Ridley & Mengler (2000 , Fig. 2
Image
Fimiston (cont.) and Mt. Charlotte samples. a. Scan of two halves of GMO, a breccia composed primarily of Paringa Basalt and black shale clasts. The entire rock is mineralized with pyrite (py) and arsenopyrite (apy). b. Polished mount of GMO (GMO-002), showing abundant pyrite mineralization. Field of view is 2 cm. c. Quarter-cut drill core of carbonate-altered Golden Mile dolerite (GMD) with Mt. Charlotte-style pyrite euhedra, drill hole SE-6. d. Polished mount of 106755, which is mineralized GMD (unit 8) from the Flanagan fault zone at the underground Mount Charlotte mine. Lines across the pyrite crystals are laser burns (for Pb isotope analysis). Field of view is 2.5 cm.
Published: 01 August 2015
mineralization. Field of view is 2 cm. c. Quarter-cut drill core of carbonate-altered Golden Mile dolerite (GMD) with Mt. Charlotte-style pyrite euhedra, drill hole SE-6. d. Polished mount of 106755, which is mineralized GMD (unit 8) from the Flanagan fault zone at the underground Mount Charlotte mine. Lines
Journal Article
Journal: Economic Geology
Published: 01 January 2000
Economic Geology (2000) 95 (1): 85–98.
...F ig . 8. Plan projections of (a) the Charlotte and (b) the Flanagan faults, showing the position of orebodies adjacent to the faults and the distribution of alteration types in the fault zone rocks. Drill hole intersections are flagged as containing sericite (+ albite) + ankerite + pyrite...
FIGURES | View All (11)
Image
Published: 01 January 2000
F ig . 4. Orientation of faults, shear zones, and fault slickenline lineations on the 29 level, Charlotte Deeps orebody, Mount Charlotte. Distinction between Flanagan and Charlotte sets is based on orientation and slickenline pitch.
Journal Article
Published: 01 October 2004
The Canadian Mineralogist (2004) 42 (5): 1383–1404.
...F ig . 5. Distribution of alteration haloes in a composite vertical section through the Charlotte orebody (Q Drill Section) above, and the Charlotte Deeps orebody (136 Drill Section) below, the Flanagan Fault. Both sections cut approximately through the center of the vein stockwork...
FIGURES | View All (14)
Image
Published: 01 January 2000
with respect to angle of the plane from σ 1 and σ 3 . The Flanagan and Charlotte fault sets are shown as fields. Squares = northeast-dipping shear zone, filled = mineralized, gray-tone = weakly mineralized, open = nonmineralized; thick dashed lines = schematic Mohr envelopes for intact rock and fault zones
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1999
AAPG Bulletin (1999) 83 (3): 410–432.
... currents, and that the main controls on the geometry of the reservoir body were sedimentary processes ( Harding et al., 1990 ; Mattingly and Bretthauer, 1992 ; Newton and Flanagan, 1993 ). Figure 1 —Location map of the Alba field in Block 16/26 and distribution of faulted Tertiary slope and basin...
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Journal Article
Published: 01 June 2002
Petroleum Geoscience (2002) 8 (2): 99–107.
... attention ( Cosgrove & Hillier 2000 ) or have been generically described as ‘massive sandstones’ ( Lonergan et al. 2000 ). Injected sandstones in the Alba Field are well known ( Newton & Flanagan 1993 ; Lonergan et al . 2000 ), but a recent review of the core record reveals a much greater...
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Journal Article
Published: 01 June 2002
Petroleum Geoscience (2002) 8 (2): 141–149.
... (400 m long by 30 m wide) emanate from the margins of the Alba channel sandstone along fault planes. An analogy is drawn between these dykes, and the peripheral dykes formed at the margins of laccoliths as a result of the flexing and subsequent fracturing of the overlying strata. ‘Decompacting...
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Journal Article
Journal: Interpretation
Published: 05 June 2014
Interpretation (2014) 2 (4): SJ1–SJ8.
... of estimating the depth to basement from magnetic data rely on the simple assumption that the geometry of the causative source has an infinite depth extent ( Flanagan and Bain, 2013 ). This assumption ignores the fact that the thickness of the magnetized layer will be depth limited by either the crust-mantle...
FIGURES | View All (8)
Journal Article
Journal: The Leading Edge
Published: 01 October 2018
The Leading Edge (2018) 37 (10): 774–779.
... the theoretical magnetic response of some typical sedimentary structures. Corresponding author: [email protected] M ETER READER — C OORDINATED BY J ERRY H ENSEL © 2018 by The Society of Exploration Geophysicists 2018 faults Gulf of Mexico magnetics magnetization filtering...
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Journal Article
Published: 01 January 2009
Seismological Research Letters (2009) 80 (1): 31–39.
... of scenarios including variations in rupture directivity and path-propagation effects. Large ( M W > 6.0) damaging earthquakes are infrequent, and near-fault observations of ground-motion time series are limited to sparse numbers of recording stations. Consequently the database of recorded ground motions...
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Journal Article
Published: 10 November 2015
Bulletin of the Seismological Society of America (2015) 105 (6): 3203–3208.
... structure, such as tomographic analysis, can provide high-resolution regional and global velocity models that improve the relative and absolute locations of hypocenters (e.g., Aki and Lee, 1976 ; Koch, 1985 ; Johnson and Vincent, 2002 ; Murphy et al. , 2005 ; Flanagan et al. , 2007 ). To locate...
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Journal Article
Published: 01 October 2006
Bulletin of the Seismological Society of America (2006) 96 (5): 1779–1794.
..., when dealing with free-surface topography and nonplanar fault surfaces, the finite-element method is far superior to the widely used finite-difference method. Among different finite-element implementations, the explicit finite-element method with second-order elements and one-point integration...
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