poster
... Genomic tool development for ecologically-relevant non-model species has lagged relative to model species, advancements in sequencing technology, bioinformatics processing, and gene expression platforms have led to an increasing number of non-model species having deepcoverage and well-annotated tran ...
... Genomic tool development for ecologically-relevant non-model species has lagged relative to model species, advancements in sequencing technology, bioinformatics processing, and gene expression platforms have led to an increasing number of non-model species having deepcoverage and well-annotated tran ...
B. The Mantle
... materials (i.e. silica) that have formed at the earth’s surface. Those banded iron formations that date before 3.0 BYA are composed of elemental, un-oxidized iron, indicating that they formed in an atmosphere devoid of free oxygen. Those banded iron formations that date younger than 3.0 BYA consist ...
... materials (i.e. silica) that have formed at the earth’s surface. Those banded iron formations that date before 3.0 BYA are composed of elemental, un-oxidized iron, indicating that they formed in an atmosphere devoid of free oxygen. Those banded iron formations that date younger than 3.0 BYA consist ...
1. Base your answer to the following question on the
... 20. Base your answer to the following question on the map below, which shows seismic stations X, Y, and Z that have recorded seismic waves from the same earthquake. The distances from seismic stations X and Y to the earthquake epicenter have been drawn on the map. Locations A, B, C, and D represent ...
... 20. Base your answer to the following question on the map below, which shows seismic stations X, Y, and Z that have recorded seismic waves from the same earthquake. The distances from seismic stations X and Y to the earthquake epicenter have been drawn on the map. Locations A, B, C, and D represent ...
Abstract
... Figure S5. 71 point sources are used to simulate a synthetic bilateral rupture. The total length of the synthetic rupture is about 974 km (487 km north and 487 south of the epicenter). The spacing between each point source is about 14 km. The timing between each point source is 5 seconds. This setup ...
... Figure S5. 71 point sources are used to simulate a synthetic bilateral rupture. The total length of the synthetic rupture is about 974 km (487 km north and 487 south of the epicenter). The spacing between each point source is about 14 km. The timing between each point source is 5 seconds. This setup ...
A bioinformatika új világa
... A science which deals with the production, analysis, modelling, depiction and storage of biological data Biological data: sequence, gene expression value, 3D protein structure Analysis can be done with an algorithm, program/script or pipeline of different tools Storage in databases for restricted/pu ...
... A science which deals with the production, analysis, modelling, depiction and storage of biological data Biological data: sequence, gene expression value, 3D protein structure Analysis can be done with an algorithm, program/script or pipeline of different tools Storage in databases for restricted/pu ...
III. MINERALS AND ROCKS 3.1 INTERPRETING SEISMIC
... The challenge before us is to interpret these curves in terms of the geology. What materials are these? To do this involves several different ideas: 1) Use the chemistry of the earth’s crust, which we can observe, to make useful extrapolations with depth. 2) Use the chemistry of the solar system (su ...
... The challenge before us is to interpret these curves in terms of the geology. What materials are these? To do this involves several different ideas: 1) Use the chemistry of the earth’s crust, which we can observe, to make useful extrapolations with depth. 2) Use the chemistry of the solar system (su ...
The electrical resistivity structure of the crust beneath the northern
... GPS timing (accurate to +2 ms) were obtained at most sites, allowing remote reference processing (Gamble et al. 1979). Direct current (DC) resistivity sounding data with electrode spacings of up to several hundred metres were collected at all sites to determine shallow structure; these models can be ...
... GPS timing (accurate to +2 ms) were obtained at most sites, allowing remote reference processing (Gamble et al. 1979). Direct current (DC) resistivity sounding data with electrode spacings of up to several hundred metres were collected at all sites to determine shallow structure; these models can be ...
psha using different attenuation relationships for different
... relations for different sets of sources. Use of multiple attenuation relations as is done to consider the epistemic uncertainties will not be able to solve this type of problem. This paper presents an example of the PSHA with simultaneous use of different attenuation relations for different seismic ...
... relations for different sets of sources. Use of multiple attenuation relations as is done to consider the epistemic uncertainties will not be able to solve this type of problem. This paper presents an example of the PSHA with simultaneous use of different attenuation relations for different seismic ...
A high conductivity anomaly on the West African craton
... Fig. 2. Observed Bouguer anomaly and schematic interpretational model along a NW-SE profile ...
... Fig. 2. Observed Bouguer anomaly and schematic interpretational model along a NW-SE profile ...
Seismic character of volcanic activity at the ultraslow
... relationship may exist between the average size and duration of an eruption and the spreading rate of the ridge at which it occurs, although continued monitoring will be needed to confirm this relationship. Similarly, the number of teleseismic events associated with the swarm is one to two orders of ...
... relationship may exist between the average size and duration of an eruption and the spreading rate of the ridge at which it occurs, although continued monitoring will be needed to confirm this relationship. Similarly, the number of teleseismic events associated with the swarm is one to two orders of ...
Author`s personal copy
... its intensity increases at offsets of 800–1300 km (Figs. 2 and 4). Sometimes, the records of PL continue the multi-phase record of PN2; therefore, these waves are difficult to separate (Figs. 2 and 3). The PL waves are refractions/reflections from depths of about 200 km. They can be related to the L b ...
... its intensity increases at offsets of 800–1300 km (Figs. 2 and 4). Sometimes, the records of PL continue the multi-phase record of PN2; therefore, these waves are difficult to separate (Figs. 2 and 3). The PL waves are refractions/reflections from depths of about 200 km. They can be related to the L b ...
Faults
... INQUA Scale (International Union for Quaternary Research) Japan Meteorological Agency seismic intensity scale ...
... INQUA Scale (International Union for Quaternary Research) Japan Meteorological Agency seismic intensity scale ...
Lesson 1: Introduction Objectives: Students will: • Familiarize
... the cracked shell on their worksheet and have them write down what the cracked shell pieces represent (Earth’s plates). Explain to students that the layers of the earth that form the plates are the crust and the uppermost part of the mantle, collectively known as the lithosphere. Have students write ...
... the cracked shell on their worksheet and have them write down what the cracked shell pieces represent (Earth’s plates). Explain to students that the layers of the earth that form the plates are the crust and the uppermost part of the mantle, collectively known as the lithosphere. Have students write ...
Imaging the mantle transition zone beneath eastern and central
... We applied the CCP stacking technique to the receiver-function data to image the P to S conversion events and their lateral variations beneath the array (e.g., Dueker and Sheehan, 1997; Niu et al., 2005). For an assumed conversion depth, d, we first computed the relative arrival time of the converted ...
... We applied the CCP stacking technique to the receiver-function data to image the P to S conversion events and their lateral variations beneath the array (e.g., Dueker and Sheehan, 1997; Niu et al., 2005). For an assumed conversion depth, d, we first computed the relative arrival time of the converted ...
and the Korea Strait
... ABSTRACT: Group velocity maps were derived for the southern East Sea (Japan Sea) and the Korea Strait (Tsushima Strait) for the 5–36 s period range, which is sensitive to shear wave velocities of the crust and the uppermost mantle. Images produced in our study enhance our understanding of the tecton ...
... ABSTRACT: Group velocity maps were derived for the southern East Sea (Japan Sea) and the Korea Strait (Tsushima Strait) for the 5–36 s period range, which is sensitive to shear wave velocities of the crust and the uppermost mantle. Images produced in our study enhance our understanding of the tecton ...
Geology Powerpoint - Jeremy`s e
... do than your in the right place! In order for an earthquake to happen, two tectonic plates have to rub against each other. If an earthquake forms in the water than a tsunami happens. The focus is directly under the earthquake where it forms. The epicenter is directly above the focus on the earths su ...
... do than your in the right place! In order for an earthquake to happen, two tectonic plates have to rub against each other. If an earthquake forms in the water than a tsunami happens. The focus is directly under the earthquake where it forms. The epicenter is directly above the focus on the earths su ...
Body wave phase nomenclature
... - sP is an S-wave travelling up from the source and being reflected and converted to a P-wave at the surface. - PP is a P-wave which is reflected once at the earth’s surface on its way from source to receiver. - SSS is an S-wave which is reflected twice at the earth’s surface. - PcP is a P-wave whic ...
... - sP is an S-wave travelling up from the source and being reflected and converted to a P-wave at the surface. - PP is a P-wave which is reflected once at the earth’s surface on its way from source to receiver. - SSS is an S-wave which is reflected twice at the earth’s surface. - PcP is a P-wave whic ...
An Alternative Analysis of the Probabilistic Seismic Hazard for Las Vegas Valley, Nevada 2014
... - 3 ground shaking parameters - Peak Ground Acceleration (PGA) - 0.2-s spectral acceleration - 1.0-s spectral acceleration ...
... - 3 ground shaking parameters - Peak Ground Acceleration (PGA) - 0.2-s spectral acceleration - 1.0-s spectral acceleration ...
Discussion of MS magnitude computation
... surface wave amplitudes change smoothly with distance. They generally decay up to about 140° and increase again beyond about 150°-160°. The latter is due to the increased geometric focusing towards the antipode of the spherical Earth's surface which then overwhelms the amplitude decay due to attenua ...
... surface wave amplitudes change smoothly with distance. They generally decay up to about 140° and increase again beyond about 150°-160°. The latter is due to the increased geometric focusing towards the antipode of the spherical Earth's surface which then overwhelms the amplitude decay due to attenua ...
Free Surface Multiple Removal Theory - M-OSRP
... the wavelet shape. The result is shown in Figure 5. In the last figure, we see there is no source notch to fill; the first source notch is at 44Hz which lies above the source frequency range (1–30Hz). Figure 5: SEAM data, shot 131373: recorded data at 17m (top panel), receiver deghosted at 10m (seco ...
... the wavelet shape. The result is shown in Figure 5. In the last figure, we see there is no source notch to fill; the first source notch is at 44Hz which lies above the source frequency range (1–30Hz). Figure 5: SEAM data, shot 131373: recorded data at 17m (top panel), receiver deghosted at 10m (seco ...
Introduction to Plate Tectonics By Elizabeth Cochran
... student must interpret several sets of data to determine the location and type of plate boundary. To develop a set of basic analytical skills, the students draw several diagrams and graphs to reinforce the data presented in figures. Students are also asked to think critically about plate rates and w ...
... student must interpret several sets of data to determine the location and type of plate boundary. To develop a set of basic analytical skills, the students draw several diagrams and graphs to reinforce the data presented in figures. Students are also asked to think critically about plate rates and w ...
Regional phases in continental and oceanic environments
... the frames at 30 and 44 s) and transmission into the mantle occurs in each of the pre-critical reflections, helping to enhance the Sn field. The S waves in the oceanic crust are linked to reverberations of P waves in the ocean. These P multiples build a strong wave train following Sn that extends ne ...
... the frames at 30 and 44 s) and transmission into the mantle occurs in each of the pre-critical reflections, helping to enhance the Sn field. The S waves in the oceanic crust are linked to reverberations of P waves in the ocean. These P multiples build a strong wave train following Sn that extends ne ...
Student`s Copy
... 15. The study of how seismic waves change as they travel through Earth has revealed that A) P-waves travel more slowly than S-waves through Earth’s crust B) seismic waves travel more slowly through the mantle because it is very dense C) Earth’s outer core is solid because P-waves are not transmitted ...
... 15. The study of how seismic waves change as they travel through Earth has revealed that A) P-waves travel more slowly than S-waves through Earth’s crust B) seismic waves travel more slowly through the mantle because it is very dense C) Earth’s outer core is solid because P-waves are not transmitted ...
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.