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log-spiral

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(A) Mbotyi Bay, here a half-graben is being excavated out as a log-spiral bay. Erosion is dominantly marine reworking. Source material: Umtata (3128) 250 000 geological map. (B) represents the cross-section A-A′. The Mbotyi Formation is presently mapped as Cretaceous but is more likely to be Upper Jurassic in age.
Published: 01 September 2018
Figure 2. (A) Mbotyi Bay, here a half-graben is being excavated out as a log-spiral bay. Erosion is dominantly marine reworking. Source material: Umtata (3128) 250 000 geological map. (B) represents the cross-section A-A′. The Mbotyi Formation is presently mapped as Cretaceous but is more
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The typical log-spiral morphology and location of the two strandline deposits (indicated in red and blue) relative to the current coastline and bedrock contours. The delineation of the strandline deposits was established from borehole intersections and represents occurrences of greater than 1-m thicknesses. The Orange Feldspathic Sands Mineralized 2 (OFSM2; hatched) is confined to the proximity of Strandline East, indicating their genetic relationship.
Published: 01 September 2015
Fig. 6 The typical log-spiral morphology and location of the two strandline deposits (indicated in red and blue) relative to the current coastline and bedrock contours. The delineation of the strandline deposits was established from borehole intersections and represents occurrences of greater
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Comparison between limit-equilibrium method (slices, circle, log-spiral, and arbitrary failure surface) and limit-analysis method.
Published: 01 June 2004
Figure 10 Comparison between limit-equilibrium method (slices, circle, log-spiral, and arbitrary failure surface) and limit-analysis method.
Journal Article
Published: 01 September 2018
South African Journal of Geology (2018) 121 (3): 227–236.
...Figure 2. (A) Mbotyi Bay, here a half-graben is being excavated out as a log-spiral bay. Erosion is dominantly marine reworking. Source material: Umtata (3128) 250 000 geological map. (B) represents the cross-section A-A′. The Mbotyi Formation is presently mapped as Cretaceous but is more...
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First thumbnail for: Submarine mass flow channels as an underlying cont...
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Published: 01 June 2004
Table 2 Safety Number Calculated by Different Methods and for Different Failure Surfaces Limit Equilibrium Slope (°) φ′ (°) Slice Circle Log-Spiral Limit Analysis (Log-Spiral) Limit Equilibrium (Arbitrary; This Study) 45 0 5.88 5.88 5.88 5.53 5.88 30
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Paleogeography of the Lonesome Point, Michigan, USA, strandplain complex from ca. 8–4 ka. Black line represents cross sections found in Figures 12C–12G. In panel E, plan view of shoreline east of Au Sable Point and Grand Marais includes log-spiral geometry labeled i, ii, and iii on the digital elevation model and repeated in the white panel, which illustrates consistency in dominant wind direction, wave refraction, and littoral drift through time.
Published: 13 December 2024
Figure 13. Paleogeography of the Lonesome Point, Michigan, USA, strandplain complex from ca. 8–4 ka. Black line represents cross sections found in Figures 12C – 12G . In panel E, plan view of shoreline east of Au Sable Point and Grand Marais includes log-spiral geometry labeled i, ii, and iii
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Key elements illustrating the genetic development ofa coastal heavy mineralplacerdeposit ofwhich the Namakwa Sands deposit is a good example. Sediment input via the Olifants River and Sout River (Figure 18) is distributed along the coast by longshore drift and the presence ofa log spiral beach, or locally known as af-bay at Brand-se-baaiplayed an instrumental role in establishing the two strandline deposits during different sea level stillstands along thepalaeo-coastline (Haq et al., 1987). Northerly shoaling waves were refracted around a southern headland, losing energy to carry its bed load around the bottom curve of the sheltering f-bay. Strong, influential coastal winds continuously reworked the strandline and primary dune deposits. Prevailing conditions and distribution of the strandlines and associated aeolian orange feldspathic sands are shown in (a) The conspicuous northeast trend, and the opposing southeast trend in mineralisation of the overlying dune deposits is the result of the three prevailing wind directions, namely the southwest, northwest and northeast winds in addition to topographic barriers. These winds did not operate simultaneously, but are seasonally controlled so that their resulting force together with the orientation of the topographic barriers shaped the mineralisation spatially. This is illustrated by the distribution of the Red Aeolian Sand beds (RAS) that cover the entire deposit (After Philander and Rozendaal, 2015b). (b) On a regional African scale not all these genetic elements are preserved and the extensive in-land mineralized dune fields typical of many deposits, are considered similar in origin to the GD-Epart of the Namakwa Sands deposit.
Published: 01 March 2017
Figure 19. Key elements illustrating the genetic development ofa coastal heavy mineralplacerdeposit ofwhich the Namakwa Sands deposit is a good example. Sediment input via the Olifants River and Sout River ( Figure 18 ) is distributed along the coast by longshore drift and the presence ofa log
Journal Article
Published: 01 September 1976
Journal of Sedimentary Research (1976) 46 (3): 738–742.
..., correspond to sedimentary populations (Visher, 1969). A spiral curve is formed by several arches of which we know the equations. These arches are homologues of the straight lines of sedimentary populations in log-probability curves. The logarithmic spiral gives: first, an equation for the size analysis...
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Relationship between growth rate and supersaturation for fluorapatite plotted on a log-log scale. The change in the empirical order of the growth rate, n , indicates a change in the dominant growth mechanism from spiral to birth-and-spread. [Modified after Van Cappellen and Berner (1991).]
Published: 01 January 2002
Figure 13. Relationship between growth rate and supersaturation for fluorapatite plotted on a log-log scale. The change in the empirical order of the growth rate, n , indicates a change in the dominant growth mechanism from spiral to birth-and-spread. [Modified after Van Cappellen and Berner
Journal Article
Published: 01 August 1994
American Mineralogist (1994) 79 (7-8): 700–711.
.... These data indicate that spiral growth operated as a growth-controlling process for the Ostwald ripening, which occurred during the late stages of illitization. However, the normalized particle-size distribution curves fitted to a log-normal distribution curve better than the theoretical profile calculated...
Series: AAPG Studies in Geology
Published: 01 January 1993
DOI: 10.1306/St38577C13
EISBN: 9781629811048
... (drilling mud characteristics), drilling time logs (bit penetration rates), etc. The term cable, as used in the foregoing comment, should be clarified. Cables, in their most familiar form, are strong, flexible "ropes" made of spiraled metal strands. "Wireline" denotes a special form of metal stranded cable...
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Figure 4. Bilogarithmic plot of the septal area on phragmocone volume (PV). Septal area was approached by (1) its upper limit (SP2/π, upper dotted line); (2) the cross-sectional area (CSA, lower dotted line); and (3) the average between both limits (SAA, solid line). The plotted points correspond exclusively to the values obtained for SAA. Note that (1) although SAA is obtained as the average between CSA and SP2/π, its logarithmic transformation is closer to the upper limit; and that (2) the slope adjusted for Log CSA on Log PV (0.619 ± 0.007) is statistically different from 2/3 ≈ 0.67, the expected slope for isometry. This is due to the fact that, in the sample of species analyzed here, there is a weak (although statistically significant) inverse correlation between the degree of involution and the size of phragmocones. Using WD as an inverse index of shell involution (where W and D are Raup's parameters in the logarithmic spiral model [Raup 1966]), the correlation between WD and Log PV is 0.312 (p = 3.24 10−8), which means that the larger phragmocones are comparatively more evolute (i.e., with a lower ratio of cross-sectional area to phragmocone volume)
Published: 01 January 2005
involution (where W and D are Raup's parameters in the logarithmic spiral model [ Raup 1966 ]), the correlation between WD and Log PV is 0.312 ( p = 3.24 10 −8 ), which means that the larger phragmocones are comparatively more evolute (i.e., with a lower ratio of cross-sectional area to phragmocone
Journal Article
Journal: AAPG Bulletin
Published: 01 June 2004
AAPG Bulletin (2004) 88 (6): 781–799.
...Figure 10 Comparison between limit-equilibrium method (slices, circle, log-spiral, and arbitrary failure surface) and limit-analysis method. ...
FIGURES
First thumbnail for: Analysis of submarine slumping in the Gabon contin...
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Journal Article
Published: 01 March 2015
Journal of Environmental and Engineering Geophysics (2015) 20 (1): 71–79.
... B. 2002 , Archimedean-spiral and log-spiral antenna comparison: Detection and remediation technologies for mines and mine-like targets : Proceedings of SPIE , 4742 : 230 – 236 . Lestari A.A...
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Evolution of Paraticinella eubejaouaensis (Randrianasolo and Anglada, 1998), at DSDP Leg 79, Site 545, off Morocco, plotted against core log with recovery (from Hinz and others, 1984, modified) and planktonic foraminiferal zones (after Leckie and others, 2002). 1.Hedbergella trocoidea, Sample 545-50-1, 33 cm. 2.H. trocoidea, Sample 545-50-1, 33 cm. 3.P. eubejaouaensis, Sample 545-46-CC. 4.P. eubejaouaensis, sample 545-44-CC. 5.P. eubejaouaensis, Sample 545-43-CC. 6.P. eubejaouaensis, Sample 545-42-3, 75 cm. Scale bars = 100 μm; left = umbilical view; center = side view; right = spiral view. G.a. = Globigerinelloides algerianus Zone; H. = Hedbergella; P.= Paraticinella; R.= Rotalipora.
Published: 01 April 2009
F igure 3. Evolution of Paraticinella eubejaouaensis ( Randrianasolo and Anglada, 1998 ), at DSDP Leg 79, Site 545, off Morocco, plotted against core log with recovery (from Hinz and others, 1984 , modified) and planktonic foraminiferal zones (after Leckie and others, 2002 ). 1
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Geographic location, lithologic log, and outcrop view: (1) geographic distribution of Hybonoticeras (dots) and Mazapilites (stars) in Mexico and western Cuba; inset shows new records in San Luis Potosí State; (2) lithologic log of section AL-5 (levels 0–6) with records of ammonites (spirals), genus Hybonoticeras (H, large filled circles), H. authariformis n. sp. [M] (diamonds), genus Mazapilites (M, stars), haploceratines (black squares), perisphinctines (gray squares), bivalves (bilobate symbols), and serpulids (cylinders); faunal spectra (pie diagrams) shown for the complete section and characteristic beds, with numbers in brackets indicating the total fauna for each bed, and black and gray colors for benthics and ammonites, respectively; rectangle indicates the precise horizon of the combined record of Hybonoticeras and Mazapilites; (3) outcrop view of the studied section AL-5 located near Alamitos de los Díaz, known in the geological literature as Rancho Los Alamitos, 23o39'1.6''N, 100o50'54.7''W. Mexican states: Camp. = Campeche Shelf; Chih. = Chihuahua; Coah. = Coahuila; Dgo. = Durango; NL = Nuevo León; Pue. = Puebla; Qro. = Queretaro; SLP = San Luís Potosí; Son. = Sonora; Tamps. = Tamaulipas; Ver. = Veracruz; Zac. = Zacatecas.
Published: 01 May 2018
Figure 1. Geographic location, lithologic log, and outcrop view: ( 1 ) geographic distribution of Hybonoticeras (dots) and Mazapilites (stars) in Mexico and western Cuba; inset shows new records in San Luis Potosí State; ( 2 ) lithologic log of section AL-5 (levels 0–6) with records
Journal Article
Published: 01 August 2001
Clays and Clay Minerals (2001) 49 (4): 300–309.
... particles exhibited various spiral growth patterns, i.e. circular, malformed circular, or polygonal single unit-cell layer spirals, polygonal parallel step spiral, or interlaced spiral patterns. The polygonal parallel step spiral and interlaced spiral patterns are formed by two single unit-cell layers...
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Journal Article
Journal: The Leading Edge
Published: 01 December 2015
The Leading Edge (2015) 34 (12): 1488–1493.
... data. Rock-physics modeling shows a relationship between elastic properties and seismic anisotropy and between elastic properties and reservoir properties, such as porosity and fracture density. Figure 2. (a) Well-log section from offset well confirming local fracturing and sonic anisotropy...
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First thumbnail for: Application of prestack orthotropic AVAz inversion...
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Journal Article
Journal: Paleobiology
Published: 01 November 2021
Paleobiology (2021) 47 (4): 648–665.
... and Raup. It is based on an explicit assumption that shells are isometric and grow exponentially, and an implicit assumption that the external form of the shell follows the internal shape, which implies that the parameters of the spiral could be reconstructed from the external whorl profile...
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First thumbnail for: Going round the twist—an empirical analysis of she...
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Journal Article
Journal: Geophysics
Published: 22 May 2013
Geophysics (2013) 78 (3): WB17–WB29.
... applications are identified, including: (1) prescribing the maximum radius of 3D VSP spirals; (2) a novel annular-spiral 3D VSP geometry to reduce acquisition time and cost; (3) a novel azimuthal-walkaway geometry for presurvey acquisition; (4) identifying optimal data for rapid postacquisition quality control...
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First thumbnail for: Optimal nonlinear design of marine borehole seismi...
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