87,346 research outputs found
The effects of fault geometry and kinematic parameters on 3D fold morphology: insights from 3D geometric models and comparison with the Dushanzi anticline, China
No full textAuthor: Zhigang Li, Wei Chen, Dong Jia, Chuang Sun, Wenjun Zheng, Peizhen Zhang, Weitao Wang, Tao Li, Jianguo Xiong
Corresponding author: Zhigang Li ([email protected]); Wei Chen ([email protected]); Chuang Sun ([email protected])
This supporting information includes the supplementary 3 figures and 6 tables.
Figure S1. Uninterpreted petroleum seismic reflection across the Dushanzi Anticline. See the interpreted section in Figure 6.
Figure S2. Perspective views of the layer and fault pointsets and models generated from the pseudo-3D forward geometric modeling using trishear 3D software and 3D structural modeling using GoCAD software. The model comprises five sedimentary layers (with layer height of 150, 175, 200, 225, and 250 units) and a fault surface. Contours of the top surface (layer 5, 250 units) are at intervals of 20 units. See the perspective view of the horizon and fault models in Figure 3, the plan view of the layer 5 in Figure 4.
Figure S3. Perspective views of the horizon and fault picks and models generated from 3D seismic interpretation and field measures. The 30 m digital elevation model, five horizon layers (the base of Lower Cretaceous, Paleogene, Lower Neogene, Lower Pleistocene, and Holocene) and two fault surfaces (the Dushanzi and Halaande faults), and secondary fault scarps are indicated. See the final structural models of the Dushanzi Anticline in Figures 7 and 8.
Table S1. The measured results of series A models when the fault ramp angles are increased from 10° to 30° with 2° step.
Table S2. The measured results of series B models when the trishear angles are increased from 60° to 120° with 6° step.
Table S3. The measured results of series C models when the P/S ratios are increased from 0 to 3 with 0.3 step.
Table S4. The measured results of series D models when the shortening/fault length are increased from 0.05 to 0.15 with 0.01 step.
Table S5. The measured results of series E models when the layer height/fault length are increased from 0.05 to 0.2 with 0.015 step.
Table S6. The measured results of series F models when the displacement gradient angles are increased from 12.5° to 25° with 1.25° step
Variations on the Author
Full text link“Variations on the Author” discusses two of Eduardo Coutinho’s recent films (Um Dia na Vida, from 2010, and Últimas Conversas, posthumously released in 2015) and their contribution to the general question of documentary authorship. The director’s filmography is characterized by a consistent yet self-effacing form of authorial self-inscription: Coutinho often features as an interviewer that rather than express opinions propels discourses; an interviewer that is good at listening. This mode of self-inscription characterizes him as an author who is not expressive but who is nonetheless markedly present on the screen. In Um Dia na Vida, however, Coutinho is completely absent form the image, while Últimas Conversas, on the contrary, includes a confessional prologue that moves the director from the margins to the center of his films. This article examines the ways in which these works stand out in the filmography of a director who offers new insights into the notion of cinematic authorship
The effects of fault geometry and kinematic parameters on 3D fold morphology: insights from 3D geometric models and comparison with the Dushanzi anticline, China
No full textAuthor: Zhigang Li, Wei Chen, Dong Jia, Chuang Sun, Wenjun Zheng, Peizhen Zhang, Weitao Wang, Tao Li, Jianguo Xiong
Corresponding author: Zhigang Li ([email protected]); Wei Chen ([email protected]); Chuang Sun ([email protected])
This supporting information includes the supplementary 3 figures and 6 tables.
Figure S1. Uninterpreted petroleum seismic reflection across the Dushanzi Anticline. See the interpreted section in Figure 6.
Figure S2. Perspective views of the layer and fault pointsets and models generated from the pseudo-3D forward geometric modeling using trishear 3D software and 3D structural modeling using GoCAD software. The model comprises five sedimentary layers (with layer height of 150, 175, 200, 225, and 250 units) and a fault surface. Contours of the top surface (layer 5, 250 units) are at intervals of 20 units. See the perspective view of the horizon and fault models in Figure 3, the plan view of the layer 5 in Figure 4.
Figure S3. Perspective views of the horizon and fault picks and models generated from 3D seismic interpretation and field measures. The 30 m digital elevation model, five horizon layers (the base of Lower Cretaceous, Paleogene, Lower Neogene, Lower Pleistocene, and Holocene) and two fault surfaces (the Dushanzi and Halaande faults), and secondary fault scarps are indicated. See the final structural models of the Dushanzi Anticline in Figures 7 and 8.
Table S1. The measured results of series A models when the fault ramp angles are increased from 10° to 30° with 2° step.
Table S2. The measured results of series B models when the trishear angles are increased from 60° to 120° with 6° step.
Table S3. The measured results of series C models when the P/S ratios are increased from 0 to 3 with 0.3 step.
Table S4. The measured results of series D models when the shortening/fault length are increased from 0.05 to 0.15 with 0.01 step.
Table S5. The measured results of series E models when the layer height/fault length are increased from 0.05 to 0.2 with 0.015 step.
Table S6. The measured results of series F models when the displacement gradient angles are increased from 12.5° to 25° with 1.25° step
[Newspaper Clipping: Author Claims Evidence of Second JFK Assassin #1]
No full textNewspaper article titled "Author Claims Evidence of Second JFK Assassin." The article states that author Richard J. Whalen concluded "that there is circumstantial evidence to support the theory of a second assassin in the shooting of President John F. Kennedy.
Also By The Same Author: AKTiveAuthor, a Citation Graph Approach to Name Disambiguation
No full textThe desire for definitive data and the semantic web drive for inference over heterogeneous data sources requires co-reference resolution to be performed on those data. In particular, name disambiguation is required to allow accurate publication lists, citation counts and impact measures to be determined. This paper describes a graph-based approach to author disambiguation on large-scale citation networks. Using self-citation, co-authorship and document source analyses, AKTiveAuthor clusters papers, achieving precision of 0.997 and recall of 0.818 over a test group of eight surname clusters
John F. Kennedy telegram to Roosevelt
No full textJersey Homesteads (later the Borough of Roosevelt) was established in the 1930s as an agro-industrial cooperative community. It was established specifically for urban Jewish garment workers, many of whom had emigrated from Europe. President John F. Kennedy sent a telegram to the citizens of Roosevelt, New Jersey, apologizing for not being able to attend the memorial dedication in honor of former President Franklin Delano Roosevelt. (Jersey Homesteads became Roosevelt in 1945 in honor of the president.) President Kennedy expressed his gratitude to the people of Roosevelt for constructing the memorial, and commented that it will serve as a constant reminder of Roosevelt's good works
Logarithmic variance profiles and the corresponding f-1 spectra of temperature fluctuations in turbulent Rayleigh-Bénard convection
No full textWe report experimental results for the temperature variance 2(z) and the corresponding frequency spectra P(f) in turbulent Rayleigh-Bénard convection (RBC) in a cylindrical sample of aspect ratioT= D/L = 1:00 (D = 1:12 m is the diameter and L = 1:12 m the height). The measurements were conducted in the Rayleigh-number range 1011 < Ra < 1:35 1014 and Pr ' 0:8. For Ra = 1:35x1014, 2(z) could be described well by a logarithmic dependence on the vertical position z in a range of z 1 < z < z 2 with z 1 ' 70 and z 2 = 0:1L. Here L=(2Nu) is the thickness of a thin thermal sublayer adjacent to the horizontal plate where the heat flux (denoted by the Nusselt number Nu) is carried mostly by thermal diffusion. In the log layer, we found that the temperature spectra had a significant frequency range over which P(f) f with close to 1. As Ra decreased, increased so that the log layer became thinner. At Ra = 2:05 1011, z 2 < z 1 and therefore there was no range for a log layer. Correspondingly, the temperature spectrum near the horizontal plate did not have the f1 scaling form either
Maine author Franklin F. Gould recalls his first glimpse of the outside world
No full textMaine author Franklin F. Gould recalls his first glimpse of the outside world as he relates how, as a young farm boy in the late 1800\u27s, he drove his father\u27s horses on an errand to an icebound river
Mapping the Discipline of the Olympic Games An Author-Cocitation Analysis
Full text linkThe authors conducted an author cocitation analysis on prominent authors writing about the Olympics during the 1990s. Author cocitation is an established bibliometric technique that can be used to measure the relative similarities of topics written about by the cited authors. This enables a visual representation of the “intellectual space” of the discipline, in this case the Olympics, to be created for the period under review. So core and peripheral research areas are identified, along with their major contributors. The representation appears as a two-dimensional cluster-enhanced map. Subject expertise was then applied to the results to place labels on the generated clusters of authors and their topics
Sous-facteurs de L(F∞) d'indice 4cos2π/n,n≥3
No full textLet Q be a factor of type II1, λ a number in the Jones discrete series {4cosπ/m:m≥3}, and {ei} the Jones projections associated with λ. Denote by A2n and A1n the finite-dimensional von Neumann algebras generated, respectively, by {1,e2,⋯,en} and {1,e1,⋯,en}, with the corresponding traces. The author shows that, for n sufficiently large, the index of the inclusion An=(Q⊗A2n)∗A2nA1n⊂(Q⊗A2n+1)∗A2n+1A1n+1=An+1 is equal to λ (here ∗ denotes the reduced, amalgamated free product of the algebras in question). Using the random matrix model of Voiculescu, he proves that if Q is the von Neumann algebra L(F∞) of the free group with infinitely many generators, then An is isomorphic to L(F∞).
The two facts together imply the existence, for any λ in the Jones discrete series, of an irreducible subfactor of L(F∞) of index λ. This constitutes the first example of a nonhyperfinite, non-Γ II1 factor such that its Jones invariant is fully computable (the existence of nonirreducible subfactors of L(F∞) for any index ≥4 is a simple consequence of known results)
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