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Asymmetry of high-velocity lower crust on the South
Asymmetry of high-velocity lower crust on the South

... et al., 2008), but they have not yet been studied for areal extent and rifting process determination. That is the purpose of the study reported here. We provide seismic velocity and gravity models for two new margin profiles in South America and integrate them with five others into a regional interp ...
standard - TTAC Online
standard - TTAC Online

... a) volume, area, mass elapsed time, direction, temperature, pressure, distance, density, and changes in elevation/depth are calculated utilizing the most appropriate tools; b) technologies, including computers, probeware, and geospatial technologies, are used to collect, analyze, and report data and ...
Spreading Continents Kick-Started Plate Tectonics Plate tectonics
Spreading Continents Kick-Started Plate Tectonics Plate tectonics

... consistent with recent estimates of rheological parameters of the lithospheric mantle21,22, increasing ...
Assessment of Seismic Response Analysis of Base Isolated RC
Assessment of Seismic Response Analysis of Base Isolated RC

... significant loss of life and damage to property every year. Various seismic construction designs and techniques have been over the years in attempts to mitigate the effects of earthquakes on Buildings. Buildings are lifeline structures. They play very important role in our life, and their failure du ...
oceanic crust
oceanic crust

... decaying radioactive elements deep within the newly-assembled planet, and from gravitational compression and nearly constant asteroid impacts ...
Field Trip to the Fall Zone, Cape Fear River, Raven Rock State Park
Field Trip to the Fall Zone, Cape Fear River, Raven Rock State Park

... Malinconico, 2010). Much of this erosion occurred soon after breakup, producing a pronounced unconformity between the syn- and post-rift rocks. Additionally, significant deformation occurred after rifting, folding and tilting the synrift strata (e.g., Withjack et al., 1998). Like their post-Rodinian ...
The Sea Floor – Chapter 2
The Sea Floor – Chapter 2

... from decaying radioactive elements deep within the newly-assembled planet, and from gravitational compression and nearly constant ...
Lecture17
Lecture17

... down the fault plane, reducing the stress. 20 Seconds Rupture has progressed along the entire length of the fault. The earthquake stops. ...
- Wiley Online Library
- Wiley Online Library

... accommodated by the rotation of continental fault blocks, which are underlain by the S reflector, an interpreted detachment fault, along which exhumed and serpentinized mantle peridotite is observed. West of these features, the enigmatic Peridotite Ridge has been inferred to delimit the western exten ...
Continental hyperextension, mantle exhumation and thin oceanic
Continental hyperextension, mantle exhumation and thin oceanic

... accommodated by the rotation of continental fault blocks, which are underlain by the S reflector, an interpreted detachment fault, along which exhumed and serpentinized mantle peridotite is observed. West of these features, the enigmatic Peridotite Ridge has been inferred to delimit the western exten ...
Chapter 20 The Precambrian Record
Chapter 20 The Precambrian Record

... When you have finished reading the chapter, work through the material that follows to review it. Complete the sentences. As you proceed, evaluate your performance for each section by consulting the answers on pages 177-178. Do not continue with the next section until you understand each answer. If y ...
Earthquake Mechanisms and Plate Tectonics
Earthquake Mechanisms and Plate Tectonics

... neutral surface separating the upper extensional zone from the lower ¯exural zone, and thus provide information on the mechanical state of the lithosphere. Occasionally, trenches are the sites of large normal fault earthquakes (e.g., Sanriku 1933 and Indonesia 1977). There has been some controversy ...
Oceanic lithosphereasthenosphere boundary from surface wave
Oceanic lithosphereasthenosphere boundary from surface wave

... The data set is composed of compiled Rayleigh and Love wave group and phase velocities. A very large amount of these data was collected from different groups. These include phase velocity dispersion data of the fundamental mode of the Love and Rayleigh waves from Harvard [Ekström et al., 1997] using ...
Mantle Convection and Plate Tectonics: A Primary Cause
Mantle Convection and Plate Tectonics: A Primary Cause

... When the earth got cooled, the lithosphere cracked and split into seven large and twelve small floating islands with ragged edges: the „Tectonic Plate‟ which is a large relatively rigid segment of earth‟s lithosphere that moves in relation to other plates over the deep interior Plates meet in conver ...
3-Component Seismograph
3-Component Seismograph

... Background page to accompany the animations on the website: IRIS Animations ...
Statistical petrology reveals a link between supercontinents cycle
Statistical petrology reveals a link between supercontinents cycle

... great an excess Tp might be derived from a plume originating from the deep mantle (Bunge 2005). Assuming that the supercontinent cycle modulates the temperature in the convective mantle, then, on a global scale, magmatic minerals like olivine, pyroxene, amphibole, and plagioclase should have recorde ...
Statistical petrology reveals a link between supercontinents cycle
Statistical petrology reveals a link between supercontinents cycle

... great an excess Tp might be derived from a plume originating from the deep mantle (Bunge 2005). Assuming that the supercontinent cycle modulates the temperature in the convective mantle, then, on a global scale, magmatic minerals like olivine, pyroxene, amphibole, and plagioclase should have recorde ...
Plate Tectonics and the El Nino Cycle
Plate Tectonics and the El Nino Cycle

... Daniel Walker, University of Hawaii, studied earthquake activity on the East Pacific Rise (EPR), specifically at 20-40oS and 100-120oW. He gathered data on the number, size, and distribution in time and space of earthquakes provided by the International Seismological Centre of Berkshire, England. He ...
PDF - World Housing Encyclopedia
PDF - World Housing Encyclopedia

... center of Athens. The earthquake was magnitude .s =5.9 and the coordinates of the epicentre were located at 38.12.-23.64., in the area of Parnitha mountain. This earthquake came as a surprise, since no seismic activity was recorded in this region for the last 200 years. According to strong-motion re ...
Geodetic and tectonic analyses along an active plate boundary : the
Geodetic and tectonic analyses along an active plate boundary : the

... distance measurements (EDM), and provided a description and interpretation of the distribution and the evolution of active deformation across different kinds of plate boundaries. New geodetic technologies, such as very long baseline interferometry (VLBI) and the satellite laser ranging (SLR), are pl ...
Depleted lithosphere, cold, trapped asthenosphere, and frozen melt
Depleted lithosphere, cold, trapped asthenosphere, and frozen melt

... area are very different from those found in subduction zones with “normal,” steeper slab geometries. The mantle above the horizontal section of the flat slab is characterized by low P-wave velocities, high S-wave velocities, and low Vp / Vs ratios. As the slab begins to transition to a more normal d ...
Lecture 6 - Mantle and Basalts
Lecture 6 - Mantle and Basalts

... contain melt; they ascend by “creep”. Adiabatic melting occurs when rising mantle does not cool along the geotherm, but instead it remains hot. This allows it to reach the mantle solidus that has a shallower slope on the P-T diagram (see diagram below). The melting is eutectic involving olivine, opx ...
Mantle detachment faults and the breakup of cold continental
Mantle detachment faults and the breakup of cold continental

... The results indicate that decoupling between the doming subcontinental mantle and the stretched continental crust is facilitated by strain localization into diffuse zones of high strain rates, forming mantle detachments with opposite dips. Lithospheric breakup in the absence of magmas starts with hi ...
The geologic evolution of Point Lobos
The geologic evolution of Point Lobos

... Figure 5. “Transform faults” are giant fractures in the earth’s crust, across which an oceanic ridge is displaced. Offset of the ridge is not necessarily ongoing, but the crust on opposite sides of the fracture may be moving in opposite directions or in the same direction, but at different rates an ...
Investigation of the Low Velocity Layer using Shallow Seismic
Investigation of the Low Velocity Layer using Shallow Seismic

... seismic time delays of magnitude dependent on the positions (elevations) of the shot and detector. These time delays, if not accounted for, degrade the reflection seismic section by improper alignment of traces. These near surface zone has various properties. Its top sediments are usually aerated, l ...
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Earthscope



Earthscope is an earth science program using geological and geophysical techniques to explore the structure and evolution of the North American continent and to understand the processes controlling earthquakes and volcanoes. The project has three components: USARRAY, the Plate Boundary Observatory, and the San Andreas Fault Observatory at Depth.The project is funded by the National Science Foundation (NSF), and the data produced is publicly accessible in real-time. Organizations associated with the project include UNAVCO, the Incorporated Research Institutions for Seismology (IRIS), Stanford University, the United States Geological Survey (USGS) and National Aeronautics and Space Administration (NASA). Several international organizations also contribute to the initiative.
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