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Journal Article
Journal: The Leading Edge
Published: 01 June 2023
The Leading Edge (2023) 42 (6): 414–420.
... FWI, especially when FWI reflectivity is interrogated. Figure 2. (a) V P model. (b) Acoustic RTM image. (c) V S model ( V P / V S = 2). (d) Elastic RTM image. Caesar-Tonga is a subsalt Miocene development in the Green Canyon protraction area that was discovered in 2006...
FIGURES | View All (8)
Image
Reservoir A dip line intersecting a well in southern <span class="search-highlight">Caesar</span>-Tonga with the ...
Published: 01 June 2023
Figure 6. Reservoir A dip line intersecting a well in southern Caesar-Tonga with the following. (a) Legacy streamer 35 Hz RTM. (b) 18 Hz RTM generated from sparse-node OBN and streamer data using elastic FWI. (c) 14 Hz elastic FWI velocity model. (d) Corendered 14 Hz elastic FWI velocity model
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Reservoir A dip line intersecting a well in northern <span class="search-highlight">Caesar</span>-Tonga with the ...
Published: 01 June 2023
Figure 7. Reservoir A dip line intersecting a well in northern Caesar-Tonga with the following. (a) Legacy streamer 35 Hz RTM. (b) 18 Hz RTM generated from sparse-node OBN and streamer data using elastic FWI. (c) 14 Hz elastic FWI velocity model. (d) Corendered 14 Hz elastic FWI velocity model
Image
Reservoir A dip line intersecting a well in southern <span class="search-highlight">Caesar</span>-Tonga with the ...
Published: 01 June 2023
Figure 8. Reservoir A dip line intersecting a well in southern Caesar-Tonga with the following. (a) Legacy streamer 35 Hz RTM. (b) 18 Hz RTM generated from sparse-node OBN and streamer data using elastic FWI. (c) 14 Hz elastic FWI velocity model. (d) Corendered 14 Hz elastic FWI velocity model
Image
( a ) HEC-RAS Storm Frank flood run (Run 1A) overlaid by the <span class="search-highlight">CAESAR</span>–Lisfloo...
Published: 23 March 2020
Fig. 10. ( a ) HEC-RAS Storm Frank flood run (Run 1A) overlaid by the CAESAR–Lisflood Storm Frank flood run (Run 1B) on the pre-storm DEM with observed trash lines. ( b ) Comparison of the Storm Frank flood runs from HEC-RAS (Run 2A) and CAESAR–Lisflood (Run 1C) on the post-storm DEM. Location
Journal Article
Published: 01 August 2009
European Journal of Mineralogy (2009) 21 (4): 715–723.
FIGURES | View All (9)
Journal Article
Published: 01 April 2008
Mineralogical Magazine (2008) 72 (2): 541–562.
FIGURES | View All (12)
Image
Spatiotemporal evolution of sediment remobilization. (A) Satellite (Pléiade...
Published: 27 July 2023
Figure 4. Spatiotemporal evolution of sediment remobilization. (A) Satellite (Pléiades) DEM of difference (DoD)–derived net surface change (Δ z ) September 2015–10 February 2021, caused primarily by the 7 February 2021 mass flow. (B) Measured (Pléiades) and modeled (CAESAR-Lisflood) Δ z
Journal Article
Journal: Geology
Published: 27 July 2023
Geology (2023) 51 (10): 924–928.
...Figure 4. Spatiotemporal evolution of sediment remobilization. (A) Satellite (Pléiades) DEM of difference (DoD)–derived net surface change (Δ z ) September 2015–10 February 2021, caused primarily by the 7 February 2021 mass flow. (B) Measured (Pléiades) and modeled (CAESAR-Lisflood) Δ z...
FIGURES | View All (4)
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Flow chart describing the digital elevation model (DEM) and discharge input...
Published: 23 March 2020
Fig. 3. Flow chart describing the digital elevation model (DEM) and discharge input and output for each flood model run using HEC-RAS and CAESAR–Lisflood. A CAESAR–Lisflood-simulated bed elevation DEM was input into Runs 2D and 3D. The output grain-size layer in Run 1B was used in Run 3D
Journal Article
Published: 23 March 2020
Scottish Journal of Geology (2020) 56 (2): 101–116.
...Fig. 10. ( a ) HEC-RAS Storm Frank flood run (Run 1A) overlaid by the CAESAR–Lisflood Storm Frank flood run (Run 1B) on the pre-storm DEM with observed trash lines. ( b ) Comparison of the Storm Frank flood runs from HEC-RAS (Run 2A) and CAESAR–Lisflood (Run 1C) on the post-storm DEM. Location...
FIGURES | View All (13)
Journal Article
Published: 01 September 2006
Bulletin of the Seismological Society of America (2006) 96 (4B): S159–S182.
...Guo-Quan Wang; Guo-Qing Tang; Caesar R. Jackson; Xi-Yuan Zhou; Qing-Liang Lin Abstract The U.S. Geological Survey Parkfield Dense Seismograph Array ( upsar ) recorded successfully strong ground motions during the 2004 Parkfield earthquake ( M 6.0) and its aftershock series after waiting for 15...
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Journal Article
Published: 01 June 2006
Bulletin of the Seismological Society of America (2006) 96 (3): 821–845.
...Guo-Quan Wang; Guo-Qing Tang; David M. Boore; G. Van Ness Burbach; Caesar R. Jackson; Xi-Yuan Zhou; Qing-Liang Lin Abstract Significant surface waves were recorded in the western coastal plain ( wcp ) of Taiwan during the 1999 Chi-Chi, Taiwan, earthquake and its series of aftershocks. We study...
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Journal Article
Journal: GSA Bulletin
Published: 01 March 2013
GSA Bulletin (2013) 125 (3-4): 556–577.
...Fabrizio Marra; Ersilia D’Ambrosio; Gianluca Sottili; Guido Ventura Abstract Geochemical investigations on samples of pumice and lava extracted from the mortars and concretes of the Forum of Caesar and the Forum and Markets of Trajan are presented and integrated with previous analyses of lava...
FIGURES | View All (12)
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Representative well log of Reservoir A, the primary producing oil reservoir...
Published: 01 June 2023
Figure 3. Representative well log of Reservoir A, the primary producing oil reservoir at Caesar-Tonga. A representative gamma-ray log (left) and shaded resistivity log (right) are shown to indicate lithology and oil saturation, respectively. The minor horizontal lines represent intervals of 50 ft
Image
Example of comparison of ( a ) the DEM of Difference (DoD) based on LiDAR d...
Published: 23 March 2020
Fig. 8. Example of comparison of ( a ) the DEM of Difference (DoD) based on LiDAR data and ( b ) the modelled DoD from CAESAR–Lisflood at site C1. Ovals highlight localised correlations between observed and modelled geomorphic change.
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True vertical subsea depth well section, spanning south to north through ke...
Published: 01 June 2023
Figure 5. True vertical subsea depth well section, spanning south to north through key Caesar-Tonga wells with sonic data. This display compares elastic-FWI-derived velocities driven exclusively by seismic data (red) with sonic-logging-tool-derived velocities (black). Note that by excluding
Journal Article
Journal: Geology
Published: 01 May 2003
Geology (2003) 31 (5): 451–454.
..., the spatial resolution of these studies is too coarse to provide sufficient resolution, and they dealt with single-point sources of contamination. Here we present a new model, called TRACER, that integrates a two-dimensional catchment-slope and fluvial model (CAESAR, see Coulthard and Macklin, 2001...
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Journal Article
Journal: GSA Bulletin
Published: 30 September 1928
GSA Bulletin (1928) 39 (3): 703–768.
...REGINALD A. DALY Abstract Introduction Since the time of the Cæsars “something new” has ever been coming “out of Africa.” Nowadays geologists are there finding novelties, impressive, even spectacular, and each one thought-provoking. The Great Rift and volcanoes of the east, the Atlas structures...
Journal Article
Journal: Geology
Published: 01 January 2010
Geology (2010) 38 (1): 87–90.
... are then discussed. The simulations are performed with the CAESAR computational landscape evolution model ( Coulthard et al., 2002 ; Van De Wiel et al., 2007 ). The key features of this grid-based model are subevent time steps, multiple flow routing, multiple grain-size erosion and deposition, and slope...
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