作者: Strength 時(shí)間: 2025-3-21 22:40
Rifted Continental Margin off Mid-Norway, km wide rift lone. Uplift of the cen tral rift led to massive subaerial volcanism during breakup. Modeling of the margin history of vertical Illotion Illust consider large melt volumes eillplaced during hreakup, presently constituting lower crust;tI high-velocity bodies.作者: 使迷醉 時(shí)間: 2025-3-22 03:25 作者: ELATE 時(shí)間: 2025-3-22 08:18
Book 1995sional stresses thatmay cause break-up. One part of the book is dedicated to currentknowledge of the structure and evolution of various Atlantic margins.After a brief incursion into the Mediterranean, succeeding articlesreport on the transform and active margins of the Ivory Coast-Ghanatransform margin and the Sea of Japan. .作者: 生來 時(shí)間: 2025-3-22 11:42
Book 1995ecific margins around the world.Special emphasis is placed on the structure and evolution of variousAtlantic margins. .After an introduction to volcanic margin concepts, the first articlesreport the results of numerical models of the mechanics of riftpropagation, melt generation and sources of exten作者: 富饒 時(shí)間: 2025-3-22 15:57 作者: FIS 時(shí)間: 2025-3-22 21:04 作者: propose 時(shí)間: 2025-3-22 21:55
Volcanic Margin Concepts,ing and after continental breakup. Whether a volcanic margin develops or not, i.e. the relative magnitude of magmatism during breakup, depends on the temperature and fluid content of the asthenosphere along the incipient plate boundary and the dynamic history of the lithosphere during the syn-rift p作者: jovial 時(shí)間: 2025-3-23 02:33
Lithosphere-Asthenosphere Interactions Below Rifts,nsequences of extension within the solid upper lithosphere. The flow is calculated using a two-dimensional, time-dependent formulation of the Navier -Stokes equations for an incompressible viscous fluid. The viscosity depends on temperature, pressure and strain-rate. Velocity boundary conditions on 作者: 收藏品 時(shí)間: 2025-3-23 08:07
Finite Duration Rifting, Melting and Subsidence at Continental Margins,the a nhydrous manl le solidus. The qu antity of melt generated depends on four principal factors: the degree of lilhospheric thinning; the potential temperature of the asthenospheric mantle; the thickness of the lithosphere prior to rifting; and t he duration of rifting. Subsidence at rifted contin作者: RENIN 時(shí)間: 2025-3-23 09:43
Stresses Associated with Continental Break-Up,lop as the lithosphere thins are not large enough to have much influence on the tectonic development. A source of sufficiently large renewable extensional stress to cause lithospheric failure is the hot, low-density upper mantle of the type associated with a plume. Widespread extensional stress may 作者: 民間傳說 時(shí)間: 2025-3-23 15:43
Gravity Anomalies and the Thermal and Mechanical Structure of Rifted Continental Margins,sediment loading by flexure. Two main types of edge effect have been recognised: a long-wavelength, high-amplitude “single” associated WIth high rigidity. strong, margins and a short-wavelength, low-amplitude “double” associated with low rigidity , weak. margins. Within the weak margin category two 作者: Graves’-disease 時(shí)間: 2025-3-23 21:02
Nature of Thin Crust Across the Southwest Greenland Margin and its Bearing on the Location of the Oe of thin upper crust overlying a serpentinized mantle. The nature of the crust in this zone, however, remains in dispute. Interpretation that this is thinned continental crust is in conflict with the interpretation based on magnetic data which suggest it to be oceanic. The magnetic data from this r作者: 積習(xí)難改 時(shí)間: 2025-3-24 00:15
Anisotropy Measurements and the Deep Structure of a Passive Margin: Southwestern Greenland,opy. Seismic anisotropy estimation can constitute an additional constraint in the determination of the mineralogical composition of the deep crust from indirect seismic measurements. Resolution analysis studies reveal that p-and S-wave velocity measurements derived from wide-angle seismic reflection作者: Talkative 時(shí)間: 2025-3-24 02:39
Rifted Continental Margin off Mid-Norway,agmatic dimensions of the Late CretaceousPaleocene rift episode which terminated with complete lithospheric separation and massive igneous activity during breakup and initial sea floor spreading. The breakup was preceded by a 15-20 m.y syn-rift phase developing a more than 2600 km long and about 300作者: 全等 時(shí)間: 2025-3-24 09:19
The Edge Experiment and the U.S. East Coast Magnetic Anomaly,d seismic refraction data. These results are combined with magnetic total intensity data in order to establish the origin for the East Coast Magnetic Anomaly (ECMA) and to hypothesize about geological events taking place at the time that opening was initiated in the North Atlantic..Prominent seaward作者: 逃避責(zé)任 時(shí)間: 2025-3-24 13:49
Structure of Atlantic Oceanic Crust Around Chron M16 from Deep Seismic Reflection Profiles,f the acquisition parameters and of the reflective patterns, allows us to perform an identical post-stack processing sequence in order to interpret jointly the three data-sets. Despite the scattered energy produced at the contact between the sedimentary cover and the top of the igneous basement, a r作者: 殘酷的地方 時(shí)間: 2025-3-24 16:52 作者: 討好女人 時(shí)間: 2025-3-24 21:00
Nature, Structure and Evolution of the Ocean-Continent Boundary: The Lesson of the West Galicia Mar from the oceanic domain to the passive margin: basaltic seafloor, sheared and serpentinized mantle rocks cropping out on the “peridotite ridge”, mylonitized underplated gabbro, and upper continental crust resting on a strong seismic reflector considered to be a detachment..The geological and geophy作者: 賠償 時(shí)間: 2025-3-25 02:38
Detachment Faulting and Continental Breakup: The S Reflector Offshore Galicia,fault blocks are underlain on time sections by an undulating group of bright reflections, the so-called Galicia S reflector. We use a variety of advanced processing techniques to constrain the nature of S, including pre stack depth migration to construct detailed velocity models of the section overl作者: Deadpan 時(shí)間: 2025-3-25 04:28
Lithospheric Transition from Continental to Oceanic in the West Iberia Atlantic Margin,dicular to the margin from the deep ocean to the continental platform. The profiles cut across the Iberian and Tagus Abyssal Plains, respectively. The lithospheric modelling, which is based on finite element technique, combines elevation, heat flow, and gravity data. This together with the computati作者: CRATE 時(shí)間: 2025-3-25 08:25 作者: Tidious 時(shí)間: 2025-3-25 13:32
Mapping the Moho in the Iberian Mediterranean Margin by Multicoverage Processing and Merging of Widiments include in-line recordings onshore of marine profiles, and provide coincident small and large-offset multicoverage of complex areas such as the onshore/offshore transition, where classic stacked images of the vertical reflectivity lack resolution and hamper a thorough comprehension of the str作者: 釘牢 時(shí)間: 2025-3-25 17:06 作者: 傲慢人 時(shí)間: 2025-3-25 21:40
,The Cote D’Ivoire — Ghana Transform Margin: An Example of an Ocean-Continent Transform Boundary,late boundaries and are less understood than the two other major plate boundaries, (divergent and convergent). Secondly, the precise study of transfonn margins can help in better constraining the structure and evolution of the ocean-continent transfonn boundary, particularly the history of the defon作者: stress-test 時(shí)間: 2025-3-26 01:04
Backarc Evolution and Ophiolite Formation, to discuss a possible relationship between the opening of the Japan Sea and the formation of the Ophiolite belt. It is speculated that the Ophiolite belt was formed by slicing of the lithosphere and uplift of serpentinized mantle peridotite in Miocene times. Slicing of the lithosphere was induced b作者: 嚴(yán)峻考驗(yàn) 時(shí)間: 2025-3-26 05:01 作者: 武器 時(shí)間: 2025-3-26 10:53
Backarc Evolution and Ophiolite Formation,belt was formed by slicing of the lithosphere and uplift of serpentinized mantle peridotite in Miocene times. Slicing of the lithosphere was induced by the opening of the Shikoku Basin (a part of the Philippine Sea Plate) shortly after the opening of the Japan Sea.作者: 安定 時(shí)間: 2025-3-26 16:39 作者: Addictive 時(shí)間: 2025-3-26 19:28 作者: Adrenal-Glands 時(shí)間: 2025-3-26 23:34 作者: PALL 時(shí)間: 2025-3-27 01:50
J. J. Da?obeitia,R. W. Hobbs,J. H. McBride,T. A. Minshull,J. Gallart作者: CHOIR 時(shí)間: 2025-3-27 05:31
Jean-Claude Sibuet,Véronique Louvel,Robert B. Whitmarsh,Robert S. White,Susan J. Horsefield,Bertrand作者: MERIT 時(shí)間: 2025-3-27 10:13 作者: 檔案 時(shí)間: 2025-3-27 13:47
Lithosphere-Asthenosphere Interactions Below Rifts,he convective flow. The most vigorous flows occur when the rift is narrow and the transition from extended to unextended regions is sharp. The rate of extension is relatively unimportant for the parameter ranges explored here. The strain-rate dependence of viscosity is an important factor in determi作者: OFF 時(shí)間: 2025-3-27 20:09
Finite Duration Rifting, Melting and Subsidence at Continental Margins, We present results from a uniform pure-shear lithospheric stretching model for melt generation and for subsidence at continental margins rifted at realistic finite rates. Predict ions from the model are compared with observations of melt generation and Subsidence from the ‘nonvolcanic’ Galicia Bank作者: 使高興 時(shí)間: 2025-3-28 01:03
Gravity Anomalies and the Thermal and Mechanical Structure of Rifted Continental Margins,than adjacent oceanic lithosphere. Why stretched lithosphere is weak is enigmatic but. the lack of evidence of any hot-spot activity suggests that it is caused by rheological effects related to crustal composillon. rather than by reheating of the lithosphere following rifting . Despite a region of w作者: Androgen 時(shí)間: 2025-3-28 05:47
Nature of Thin Crust Across the Southwest Greenland Margin and its Bearing on the Location of the Othe southern Labrador Sea, their symmetry across the extinct ridge, and their correlation with seafloor spreading models, strongly argue for their formation by seafloor spreading. Such an interpretation is also consistent with the plate kinematic motions derived for the North American and Eurasian P作者: 相反放置 時(shí)間: 2025-3-28 08:31
Anisotropy Measurements and the Deep Structure of a Passive Margin: Southwestern Greenland,ampling) have prevented the use of a nisotropy as a constraint for the determination of lower crustal composition in favor of estimates on Poisson’s ratio. Therefore, we suggest that anisotropy estimates can place new and more relevant constraints on the different rock types present in the deep crus作者: tendinitis 時(shí)間: 2025-3-28 13:21
The Edge Experiment and the U.S. East Coast Magnetic Anomaly,ing reflectors alone are responsible for the ECMA. The crustal section here represents the Initial Oceanic Crust which is thicker and possesses higher seismic velocities than normal oceanic crust. It should not be called “transitional crust,” “modified continental crust,” or “rift stage crus!.” The 作者: Parameter 時(shí)間: 2025-3-28 15:08 作者: 驚惶 時(shí)間: 2025-3-28 20:53 作者: CRUMB 時(shí)間: 2025-3-28 23:47 作者: certain 時(shí)間: 2025-3-29 03:08
Continental-Oceanic Crustal Transition in the Bransfield Trough and the South Scotia Ridge (Antarctic Peninsula..II. South Scotia Ridge, a chain of highs and depressions along the boundary between the Scotia and Antarctic plates. It consists of continental crustal fragments transported eastward from their original position along the South America-Antarctic isthmus during the opening of Drake Pass作者: 放肆的我 時(shí)間: 2025-3-29 08:36 作者: Exposure 時(shí)間: 2025-3-29 13:55
Structure of the Marmara Sea Basin in the North Anatolian Fault Zone,a broad tectonic zone with associated high swarmlike seismic activity. The Marmara Sea basin is the extension of the Thrace basin in the north and northwest. During the Middle Eocene, the subsidence of basement occurred, creating the Thrace basin. Therefore it could be assumed that the extensional b作者: 祖先 時(shí)間: 2025-3-29 19:32 作者: BIBLE 時(shí)間: 2025-3-29 22:53 作者: Semblance 時(shí)間: 2025-3-30 02:04
ansformed into a completely different shape. To do this, we need to specify the rotation axis and angle, translation vector, scaling vector, or other manipulations to the model. The ordinary . is a process of mathematical manipulations of all the vertices of the model through matrix multiplications,作者: Legion 時(shí)間: 2025-3-30 06:08 作者: gout109 時(shí)間: 2025-3-30 08:32
Rifted Ocean-Continent Boundaries978-94-011-0043-4Series ISSN 1389-2185 作者: 暗諷 時(shí)間: 2025-3-30 15:31 作者: 先行 時(shí)間: 2025-3-30 19:27
https://doi.org/10.1007/978-94-011-0043-4Atlantic Ocean; Coast; Moho; Ocean; fault; fault zone; transform boundary; structural geology作者: Cursory 時(shí)間: 2025-3-30 22:01 作者: 充足 時(shí)間: 2025-3-31 04:22 作者: 黃油沒有 時(shí)間: 2025-3-31 08:01
,CADIAG-1 und CADIAG-2: Ans?tze zur Integrierten Computerunterstützten Medizinischen Diagnostik,ihre Berechtigung somit dadurch, da? sie die praktische ?rztliche Erfahrung, Kreativit?t und Intuition durch im Idealfall vollst?ndig gespeicherte gro?e Datenmengen und durch die M?glichkeit komplexer logischer Schlu?folgerungen erg?nzen.作者: 改正 時(shí)間: 2025-3-31 10:45 作者: 希望 時(shí)間: 2025-3-31 14:37
al (8). A remarkable aspect is the limited degree of specialisation of the phagocytic reaction: once stimulated, a virtually identical chain of events takes place, whatever the stimulus. It consists of the uptake of the challenging microparticle, if any, the activation of a series of metabolic react作者: intimate 時(shí)間: 2025-3-31 20:31
Performance of MIMO Space-Time Coding with Discrete Modulations,merical results of the .% cutoff capacities, which are defined as the highest supportable rates for target cutoff probabilities at .%. Our discussion show how this new notion can provide a unified view of all the three main theoretic results of MIMO space-time coding: rate enhancements, achievable d作者: Density 時(shí)間: 2025-3-31 22:34
2366-5998 rspectives on decision making processes in socio-environmental transformations". In conclusion, the results are framed in a broad temporal framework, and patterns of socio-environmental change are presented acr978-3-031-53316-7978-3-031-53314-3Series ISSN 2366-5998 Series E-ISSN 2366-6005 作者: Thyroxine 時(shí)間: 2025-4-1 02:09
ome the initial difficulties before the achievement of the successful results which are confidently expected today. Certainly, in the 1950s attempts to relieve pain and restore movement to an arthritic hip frequently failed. Such operations which were practised often involved a prolonged period of i作者: detach 時(shí)間: 2025-4-1 08:04
Christopher Freyisted him in editing his works, notably .. Her main contributions to phenomenology concern empathy, the body, intersubjectivity, psychology, social ontology, the state, religion, education, the human being, the human person, woman, being, and God. Her working out of the conditions for an alignment o作者: 尊敬 時(shí)間: 2025-4-1 10:31
