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71.
Diffractions not only carry important information about small-scale subsurface structures, they also possess unique properties, which make them a powerful tool for seismic processing and imaging. Since a point diffractor scatters an incoming wave to all directions, a diffraction event implies better illumination than a reflection, because the rays travel through larger parts of the subsurface. Furthermore, unlike the reflection case, in which the emergence location of the reflected wave depends on the source position, in the case of non-Snell scattering, up-going and down-going raypaths are decoupled. Based on this decoupling, we introduce a diffraction traveltime decomposition principle, which establishes a direct connection between zero-offset and finite-offset diffraction wavefield attributes. By making use of this approach, we are able to enhance diffractions and obtain high-quality diffraction wavefield attributes at arbitrary offsets in the prestack domain solely based on zero-offset processing without any further optimization of attributes. We show the accuracy of the method by fitting diffraction traveltimes, and on simple waveform data. Application to complex synthetic data shows the ability of the proposed approach to enhance diffractions and provide high-quality wavefield attributes even in sparsely illuminated regions such as subsalt areas. The promising results reveal a high potential for improved prestack data enhancement and further applications such as efficient diffraction-based finite-offset tomography. 相似文献
72.
Benjamin Bernard Benjamin van Wyk de Vries Hervé Leyrit 《Bulletin of Volcanology》2009,71(9):1041-1056
Debris avalanches associated with volcanic sector collapse are usually high-volume high-mobility phenomena. Debris avalanche
deposit remobilisation by cohesive debris flows and landslides is common, so they can share textural characteristics such
as hummocks and jigsaw cracks. Distinguishing original deposits from reworked products is critical for geological understanding
and hazard assessment because of their different origin, frequency and environmental impact. We present a methodology based
on field evidence to differentiate such epiclastic breccias. Basal contact mapping constrained by accurate altitude and location
data allows the reconstruction of deposit stratigraphy and geometry. Lithological analysis helps to distinguish the different
units. Incorporation structures, kinematic indicators and component mingling textures are used to characterise erosion and
transport mechanisms. We apply this method to the enigmatic sequence at Perrier (French Massif Central), where four units
(U1–U4) have been interpreted either as debris flow or debris avalanche deposits. The sequence results from activity on the
Monts Dore Volcano about 2 Ma ago. The epiclastic units are matrix supported with an almost flat top. U2 and U3 have clear
debris flow deposit affinities such as rounded clasts and intact blocks (no jigsaw cracks). U1 and U4 have jigsaw cracked
blocks with matrix injection and stretched sediment blocks. U1 lacks large blocks (>10 m wide) and has a homogenous matrix
with an upward increase of trapped air vesicle content and size. This unit is interpreted as a cohesive debris flow deposit
spawned from a debris avalanche upstream. In contrast, U4 has large mega-blocks (up to 40 m wide), sharp contacts between
mixed facies zones with different colours and numerous jigsaw fit blocks (open jigsaw cracks filled by monogenic intra-clast
matrix). Mega-blocks are concentrated near the deposit base and are spatially associated with major substratum erosion. This
deposit has a debris avalanche distal facies with local debris flow affinities due to partial water saturation. We also identify
two landslide deposits (L1 and L2) resulting from recent reworking that has produced a similar facies to U1 and U4. These
are distinguishable from the original deposits, as they contain blocks of mixed U1/U4 facies, a distinctly less consolidated
and more porous matrix and a fresh hummocky topography. This work shows how to differentiate epiclastic deposits with similar
characteristics, but different origins. In doing so, we improve understanding of present and past instability of the Monts
Dore and identify present landslide hazards at Perrier. 相似文献
73.
This study assesses surface urban heat island (UHI) and its associated surface physical characteristics using remote sensing approaches. TERRA/MODIS images acquired in 2005 in three different seasons were selected to generate land surface tem-perature and surface characteristics for the Changsha-Zhuzhou-Xiangtan metropolitan area in China. The intensity of urban heat is-land effects and its seasonal variations were examined. The result showed that UHI effects were significant both in the summer and the spri... 相似文献
74.
Victor L. Vinograd Benjamin P. Burton Neil L. Allan 《Geochimica et cosmochimica acta》2007,71(4):974-983
Thermodynamic mixing properties and subsolidus phase relations of the rhombohedral carbonate system, (1 − x) · CaCO3 − x · MgCO3, were modelled in the temperature range of 623-2023 K with static structure energy calculations based on well-parameterised empirical interatomic potentials. Relaxed static structure energies of a large set of randomly varied structures in a 4 × 4 × 1 supercell of calcite (a = 19.952 Å, c = 17.061 Å) were calculated with the General Utility Lattice Program (GULP). These energies were cluster expanded in a basis set of 12 pair-wise effective interactions. Temperature-dependent enthalpies of mixing were calculated by the Monte Carlo method. Free energies of mixing were obtained by thermodynamic integration of the Monte Carlo results. The calculated phase diagram is in good agreement with experimental phase boundaries. 相似文献
75.
76.
Wylie A. Carr Christopher J. Preston Laurie Yung Bronislaw Szerszynski David W. Keith Ashley M. Mercer 《Climatic change》2013,121(3):567-577
There have been a number of calls for public engagement in geoengineering in recent years. However, there has been limited discussion of why the public should have a say or what the public can be expected to contribute to geoengineering discussions. We explore how public engagement can contribute to the research, development, and governance of one branch of geoengineering, solar radiation management (SRM), in three key ways: 1. by fulfilling ethical requirements for the inclusion of affected parties in democratic decision making processes; 2. by contributing to improved dialogue and trust between scientists and the public; and 3. by ensuring that decisions about SRM research and possible deployment are informed by a broad set of societal interests, values, and framings. Finally, we argue that, despite the nascent state of many SRM technologies, the time is right for the public to participate in engagement processes. 相似文献
77.
Globalization,Pacific Islands,and the paradox of resilience 总被引:1,自引:0,他引:1
Matthew Lauer Simon Albert Shankar Aswani Benjamin S. Halpern Luke Campanella Douglas La Rose 《Global Environmental Change》2013,23(1):40-50
On April 2nd, 2007 a 12 m tsunami struck Simbo, a relatively remote island in Western Province, Solomon Islands. Although Simbo's population continues to depend on their own food production and small-scale governance regimes regulate access to resources, the island's way of life over the last century has increasingly been affected by processes associated with globalization. In this context of a rapidly globalizing world, this article examines the island's resilience and vulnerability to the tsunami and the adaptive capacities that enabled the response and recovery. The tsunami completely destroyed two villages and damaged fringing coral reefs, but casualties were low and social–ecological rebound relatively brisk. By combining social science methods (household surveys, focus group and ethnographic interviews) and underwater reef surveys we identify a number of countervailing challenges and opportunities presented by globalization that both nurture and suppress the island's resilience to high amplitude, low-frequency disturbances like tsunamis. Analysis suggests that certain adaptive capacities that sustain general system resilience come at the cost of more vulnerability to low-probability hazards. We discuss how communities undergoing increasingly complex processes of change must negotiate these kinds of trade-offs as they manage resilience at multiple spatial and temporal scales. Understanding the shifting dynamics of resilience may be critical for Pacific Island communities who seek to leverage globalization in their favor as they adapt to current social–ecological change and prepare for future large-scale ecological disturbances. 相似文献
78.
Dave A.Yuen Benjamin J. Kadlec Evan F. Bollig Witold Dzwinel Zachary A. Garbow Cesar R. S. da Silva 《Visual Geosciences》2005,10(1):1-12
We present a web client-server service WEB-IS, which we have developed for remote analysis and visualization of seismic data consisting of both small magnitude events and large earthquakes. We show that the problem-solving environment (PSE) intended for prediction of large magnitude earthquakes can be based on this WEB-IS idea. The clustering schemes, feature generation, feature extraction techniques and rendering algorithms form a computational framework of this environment. On the other hand, easy and fast access both to the seismic data distributed among distant computing resources and to computational and visualization resources can be realized in a GRID framework. We discuss the usefulness of NaradaBrokering (iNtegrated Asynchronous Real-time Adaptive Distributed Architecture) as a middleware, allowing for flexibility and high throughput for remote visualization of geophysical data. The WEB-IS functionality was tested both on synthetic and the actual earthquake catalogs. We consider the application of similar methodology for tsunami alerts. 相似文献
79.
Inflation along Kilauea's Southwest Rift Zone in 2006 总被引:1,自引:0,他引:1
David Myer David Sandwell Benjamin Brooks James Foster Masanobu Shimada 《Journal of Volcanology and Geothermal Research》2008
We report on InSAR and GPS results showing the first crustal inflation along the southwest rift zone at Kilauea volcano in over 20 years. Two independent interferograms (May 2–August 2, 2006 and June 22–Nov 7, 2006) from the ALOS PALSAR instrument reveal domal uplift located southwest of the main caldera. The uplift is bounded on the northeast by the caldera and follows the southwest rift zone for about 12 km. It is approximately 8 km wide. We use data derived from permanent GPS stations to calibrate the InSAR displacement data and estimate uplift of 7.7 cm during the first interferogram and 8.9 cm during the second with line-of-sight volumes of 2.8 × 106 m3 and 3.0 × 106 m3 respectively. The earthquake record for the periods before, during, and after inflation shows that a swarm of shallow earthquakes (z < 5 km) signaled the beginning of the uplift and that elevated levels of shallow seismicity along the rift zones occurred throughout the uplift period. GPS data indicate that the inflation occurred steadily over nine months between mid-January and mid-October, 2006 making injection of a sill unlikely. We attribute the inflation to recharge of a shallow ductile area under the SWRZ. 相似文献
80.
Interactive 3-D computation of fault surfaces using level sets 总被引:1,自引:0,他引:1
Benjamin J. Kadlec Geoffrey A. Dorn Henry M. Tufo David A. Yuen 《Visual Geosciences》2008,13(1):133-138
Deformable implicit surfaces, implemented with level set methods, have demonstrated a great potential in the computational
sciences for applications such as modeling, simulation, and segmentation. They allow implicit handling of complex topologies
deformed by operations where large changes can occur without destroying the level set representation. The use of level set
techniques for the computation and segmentation of plane-like and high positive curvature features is nontrivial. We present
a technique for representing and extracting fault surfaces from 3-D seismic attribute data such that 2-manifolds can be interactively
computed and segmented. We present our approach as an interactive workflow that generates highly accurate fault surfaces. 相似文献