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Lily Bank

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Journal Article
Journal: AAPG Bulletin
Published: 01 January 2013
AAPG Bulletin (2013) 97 (1): 61–85.
... constrained. Yet, such understanding is essential to developing meaningful predictive conceptual models of three-dimensional architecture of ancient reservoir analogs. Integrating remote-sensing imagery, high-frequency seismic data, and core characterization from Lily Bank, a modern tidally dominated Bahamian...
FIGURES | View All (16)
Journal Article
Published: 01 December 1977
Journal of Sedimentary Research (1977) 47 (4): 1554–1581.
...A. C. Hine Abstract Study of the response of an active oolite sand shoal (Lily Bank), located along the northeastern margin of Little Bahama Bank, to its physical environment and the Holocene sea-level rise has provided a developmental sequence from initial formation to present maintenance...
Image
Morphology and currents of <span class="search-highlight">Lily</span> <span class="search-highlight">Bank</span>, northern Little Bahama <span class="search-highlight">Bank</span>.  A)  Reg...
Published: 01 February 2011
Figure 5 Morphology and currents of Lily Bank, northern Little Bahama Bank. A) Regional setting, illustrating the active shoal (outlined in dashed line) set back > 10 km from the shelf margin. Box outlined by solid line highlights area in part B. B) Remote sensing images illustrating
Image
—Detail of LANDSAT image of Little Bahama <span class="search-highlight">Bank</span> showing <span class="search-highlight">Lily</span> <span class="search-highlight">Bank</span> oolite sho...
Published: 01 March 1977
Fig. 10 —Detail of LANDSAT image of Little Bahama Bank showing Lily Bank oolite shoal. Lateral extent of shoal is limited to two large reentrants in bank edge separated by Matanilla Reef East. Slightly deeper reefs extend across reentrants. Linear sand ridges radiate away from central point
Image
Interpreted Holocene evolution of <span class="search-highlight">Lily</span> <span class="search-highlight">Bank</span> in the context of sea level cha...
Published: 01 January 2013
Figure 16 Interpreted Holocene evolution of Lily Bank in the context of sea level change (inset), based on the observations of this study and Hine (1977) . The study area is indicated by the red box in each section. (A) Early to mid-Holocene. Little Bahama Bank was an exposed platform bordering
Image
Remote-sensing images of the general <span class="search-highlight">Lily</span> <span class="search-highlight">Bank</span> study area on Little Bahama ...
Published: 01 January 2013
Figure 1 Remote-sensing images of the general Lily Bank study area on Little Bahama Bank (LBB) and the Lily Bank area (LANDSAT data; highlighted by yellow box in the inset). Note the difference between the active Lily Bank (highlighted by yellow arrows in this image) and inactive tidal sand
Image
Remote-sensing image of part of <span class="search-highlight">Lily</span> <span class="search-highlight">Bank</span>, illustrating distinct bar-form m...
Published: 01 January 2013
Figure 2 Remote-sensing image of part of Lily Bank, illustrating distinct bar-form morphologic end members: transverse shoulder bars (red box) and parabolic bars (yellow box). The image also shows subaqueous dunes (which appear as stripes) on the crests of bar forms. Satellite image courtesy
Image
Summary of the sedimentologic and stratigraphic interpretation of <span class="search-highlight">Lily</span> <span class="search-highlight">Bank</span>...
Published: 01 January 2013
Figure 14 Summary of the sedimentologic and stratigraphic interpretation of Lily Bank, based on seismic and core data. The cross section lines illustrate areas from a transverse shoulder bar ( Figure 4 ) and a parabolic bar ( Figure 5 ). Refer to Figure 3 for locations. (A) Large-scale
Image
Mutually evasive flow trajectories in the parabolic bars of <span class="search-highlight">Lily</span> <span class="search-highlight">Bank</span>, Baha...
Published: 01 March 2008
Figure 17 Mutually evasive flow trajectories in the parabolic bars of Lily Bank, Bahamas. These flow patterns set up a net circular pattern on the shoals, which may be how the ooids are kept in a high-energy environment without being flushed from the system. Modified from Rankey et al. (2006
Image
—Photomicrograph of ooids from <span class="search-highlight">Lily</span> <span class="search-highlight">Bank</span>. Grains are coated thinly. Nuclei ...
Published: 01 March 1977
Fig. 13 —Photomicrograph of ooids from Lily Bank. Grains are coated thinly. Nuclei are pellets, skeletal fragments, and aggregate grains (sample 26–2, Fig. 2B ).
Image
—Aerial photograph of <span class="search-highlight">Lily</span> <span class="search-highlight">Bank</span> oolite shoal featuring large, flood- or ban...
Published: 01 March 1977
Fig. 12 —Aerial photograph of Lily Bank oolite shoal featuring large, flood- or bank-oriented spillover lobes mantled by sand waves. Viewer is looking east. Spillover lobes are approximately 100 to 200 m wide and 2 to 3 m thick.
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1980
AAPG Bulletin (1980) 64 (8): 1281–1282.
... the reservoir was deposited in an oolite bar or beach environment similar to present-day deposition at the Lily Bank oolitic shoal in the Bahamas. The trap at Spring Garden field is formed by the updip pinch-out of porous oolitic limestone into a tight micritic lime mud on a structural nose. The field has...
Image
Morphologies of microborings present in ooid cortices:  A)  untreated ooid ...
Published: 01 March 2010
image of part E, note the coarser texture of the cement compared to the cortex needles; G) biofilm-like substance (arrow) associated with the microboring and cement; and H) biofilms-like substance present in microboring with aragonite needles contained within it. Sample locations: A) Lily Bank, B
Image
A)  Transmitted-light image highlighting the presence of microborings throu...
Published: 01 March 2010
Figure 3 A) Transmitted-light image highlighting the presence of microborings throughout the cortex in an ooid from Lily Bank. B) Reflected-light image illustrating unfilled microborings and partially cement-filled borings in the outer cortex and cement-filled borings in the inner cortex.
Image
Locations of seismic lines (red and yellow) and cores (black and blue) acro...
Published: 01 January 2013
Figure 3 Locations of seismic lines (red and yellow) and cores (black and blue) across the linear shoulder bars (LBR) and linear parabolic bars (LBP) of Lily Bank. Yellow seismic lines are shown as Figures 4 and 5 ; blue cores are shown as Figures 7–9 and 11–13 . Satellite image courtesy
Journal Article
Published: 01 May 2000
Scottish Journal of Geology (2000) 36 (1): 33–37.
FIGURES
Image
Some locations of current ooid formation in the Bahamian Archipelago: (1) L...
Published: 01 March 2010
Figure 1 Some locations of current ooid formation in the Bahamian Archipelago: (1) Lily Bank, (2) Double Breasted Cay, (3) Abaco Tidal Deltas, (4) Bimini, (5) Cat Cay, (6) Brown Cay, (7) Berry Islands, (8) Joulter's Shoal, (9) Schooner Keys, (10) Exuma Tidal Deltas, (11) Head of the Tongue
Series: GCSSEPM
Published: 01 December 2006
DOI: 10.5724/gcs.06.26.0849
EISBN: 978-0-9836096-4-3
... in this report are from this region). Tidal range is unknown in this area, but flow velocities can exceed 150 cm (59 in.)/sec ( Ball, 1967 ; Palmer, 1979 ). Figure 2. Location map of focus areas showing Lily Bank marine sand belt, tidal deltas in the Abaco Islands, and the tidal sand ridges...
Image
Paired transmitted-light (left) and reflected-light (right) images of ooids...
Published: 01 March 2010
the same, with unfilled micro-borings on the outer portion of the ooid cortex and aragonite-cement-filled microborings (brighter white color in reflected light) in the inner cortex. Sample locations: A–D) Lily Bank, E–H) Schooner Cay, I–J) Ambergris Cay.
Image
—Schematic cross section, based on data from five subbottom profiles across...
Published: 01 March 1977
-edge reef. On lagoon side is zone of coalescing reef pinnacles. Behind pinnacles is thick zone of coral-algal (reef-derived) sediment. On flat Pleistocene rock surface is back-reef pellet-aggregate sand. Relict bed forms and blowouts commonly cut into this sea-grass zone. Lily Bank oolite shoal has