Pelatihan : Techniques in Active Tectonic Study Juni 20-Juli 2, 2013 Instruktur: Prof. J Ramon Arrowsmith (JRA) Dari Arizona State University (ASU) - US.

Slides:



Advertisements
Similar presentations
Pelatihan : Techniques in Active Tectonic Study Juni 20-Juli 2, 2013 Instruktur: Prof. J Ramon Arrowsmith (JRA) Dari Arizona State University (ASU) - US.
Advertisements

Pelatihan : Techniques in Active Tectonic Study Juni 20-Juli 2, 2013 Instruktur: Prof. J Ramon Arrowsmith (JRA) Dari Arizona State University (ASU) - US.
Earthquakes Chapter 19.
Pelatihan : Techniques in Active Tectonic Study Juni 20-Juli 2, 2013 Instruktur: Prof. J Ramon Arrowsmith (JRA) Dari Arizona State University (ASU) - US.
Pelatihan : Techniques in Active Tectonic Study Juni 20-Juli 2, 2013 Instruktur: Prof. J Ramon Arrowsmith (JRA) Dari Arizona State University (ASU) - US.
Pelatihan : Techniques in Active Tectonic Study Juni 20-Juli 2, 2013 Instruktur: Prof. J Ramon Arrowsmith (JRA) Dari Arizona State University (ASU) - US.
Pelatihan : Techniques in Active Tectonic Study Juni 20-Juli 2, 2013 Instruktur: Prof. J Ramon Arrowsmith (JRA) Dari Arizona State University (ASU) - US.
Pelatihan : Techniques in Active Tectonic Study Juni 20-Juli 2, 2013 Instruktur: Prof. J Ramon Arrowsmith (JRA) Dari Arizona State University (ASU) - US.
Pelatihan : Techniques in Active Tectonic Study Juni 20-Juli 2, 2013 Instruktur: Prof. J Ramon Arrowsmith (JRA) Dari Arizona State University (ASU) - US.
Pelatihan : Techniques in Active Tectonic Study Juni 20-Juli 2, 2013 Instruktur: Prof. J Ramon Arrowsmith (JRA) Dari Arizona State University (ASU) - US.
Active Folding within the L.A. Basin with a focus on: Argus et al. (2005), Interseismic strain accumulation and anthropogenic motion in metropolitan Los.
Sally McGill California State University, San Bernardino
Pelatihan : Techniques in Active Tectonic Study Juni 20-Juli 2, 2013 Instruktur: Prof. J Ramon Arrowsmith (JRA) Dari Arizona State University (ASU) - US.
Long and short term deformation along the San Andreas Fault Examples of issues of spatial and temporal scale of interest. Also indicates rate of deformation.
Earthquakes Chapter 16. What is an earthquake? An earthquake is the vibration of Earth produced by the rapid release of energy Energy radiates in all.
Geology Introduction to Strike-Slip Faults.
Strike slip faults 1. Regional tectonic setting 2. Example: the San Andreas 3. Patterns, complexities 4. Societal importance.
Earthquakes recorded in the landscape: Using digital topography to investigate earthquake faulting Christopher Crosby GEON / Arizona State University SDSC.
Tsunami Great Sumatra Earthquake Tsunami Death Toll ~ 250,000 Tsunami Death Toll ~ 250,000.
UseIT Tutorial # 3 Earthquakes in the Southern California Fault System Tom Jordan June 16, 2011.
Earthquakes Faults Stress Quakes at plate boundaries Quakes within plates.
NA-Pa Plate Boundary Wilson [1960] USGS Prof. Paper 1515.
Lecture 16 Earthquakes What are earthquakes? Elastic rebound theory Waves generated by earthquakes: P waves, S waves, Surface waves Locating earthquakes.
EARTHQUAKES 2007 Japan quake.
Earthquakes.
Pelatihan : Techniques in Active Tectonic Study Juni 20-Juli 2, 2013 Instruktur: Prof. J Ramon Arrowsmith (JRA) Dari Arizona State University (ASU) - US.
Pelatihan : Techniques in Active Tectonic Study Juni 20-Juli 2, 2013 Instruktur: Prof. J Ramon Arrowsmith (JRA) Dari Arizona State University (ASU) - US.
GEO 6950 Reviews in Earth Science, Fall 2011 Topic 2 Tectonics of Western North America 11. San Andreas Fault System Carrie Welker and Alex Turner.
These boundaries are where plates “slide” past each other. In about 60 million years Los Angeles and San Francisco will be next to each other.
Unit 1.4 Earthquakes. Where do earthquakes Occur? Earthquakes can occur near the Earth’s surface or far below the surface. Most earthquakes occur at plate.
Part 8: Fold Types. Tensional Stress Compressive Stress Shear Stress Orientation of stress leads to different folds.
Earth Science Applications of Space Based Geodesy DES-7355 Tu-Th 9:40-11:05 Seminar Room in 3892 Central Ave. (Long building) Bob Smalley Office: 3892.
Pelatihan : Techniques in Active Tectonic Study Juni 20-Juli 2, 2013 Instruktur: Prof. J Ramon Arrowsmith (JRA) Dari Arizona State University (ASU) - US.
LiDAR and the San Andreas Fault exercise Sarah Robinson ASU.
Faulting landforms from side-by-side (transform) motion
The deformation in the Plate Boundary zones Shear Zone : San Andreas - Frédéric Flerit.
Fig Earthquakes and Earthquake Hazards. 3 Seismic waves allow us to look inside the Earth.
 A vibration of the Earth produced by a rapid release of energy  Often occur along faults – breaks in the Earths crust and mantle (plate boundaries)
Using GPS and InSAR to study tectonics, deformation, and earthquakes GPS displacements, velocities (and transients) InSAR displacements.
Earthquakes. What is an Earthquake? Earthquake—the vibration of Earth produced by the rapid release of energy – Most often caused by slippage along a.
Elizabeth H. Hearn, UBC, Vancouver, CANADA in collaboration with Semih Ergintav, Marmara Research Centre, Gebze, TURKEY Robert Reilinger, MIT, Cambridge.
Pelatihan : Techniques in Active Tectonic Study Juni 20-Juli 2, 2013 Instruktur: Prof. J Ramon Arrowsmith (JRA) Dari Arizona State University (ASU) - US.
Earthquakes Chapter 6.1. Earthquakes & Plate Tectonics 1. Earthquakes are vibrations of the earth’s crust. a. Earthquakes occur when rocks under stress.
Learning about: The Great Southern California ShakeOut November 13, 2008 A Teachable Moment.
Section 6.1 Objectives 1. Discuss the elastic rebound theory.
CHAPTER 8 EARTHQUAKES. EARTHQUAKES Earthquakes result from sudden motions along breaks in Earth’s crust and can affect landforms and societies. An entire.
The repetition of large earthquakes, with similar coseismic offsets along the Carrizo segment of San Andreas fault has been documented using geomorphic.
Earthquake Machine Mechanical Modeling to Increase Student Understanding of Complex Earth Systems Most of you are probably covering strike-slip faults.
Earthquakes and crustal Deformation - Objectives of class- Introduce a variety of techniques to describe ‘quantitatively’ deformation of the lithosphere.
EART 118 Seismotectonics MWF D250 9:30-10:40 am; Th D250 2:00-4:00 pm Prof.: Thorne Lay, C382 E&MS, Office Hours 11:00-12:00 MWF TA: Lingling Ye, Office.
GeoFEM Kinematic Earthquake Cycle Modeling in the Japanese Islands Hirahara, K. (1), H. Suito (1), M. Hyodo (1) M. Iizuka (2) and H. Okuda (3) (1) Nagoya.
EARTHQUAKES Information from the USGS Locations of Earthquakes Dots are earthquakes.
Earthquakes: Forces Inside of Earth
Motion of Bering Plate? Jeff Freymueller.
Velocities in ITRF – not appropriate for interpretation
By: Andrea Jimeno Martinez 4ºA
Earthquakes and crustal Deformation - Objectives of class-
Earthquakes.
Introduction to Earthquakes
EARTHQUAKES: WHY? AND HOW?
8.1 What Is an Earthquake?  Earthquake - vibration of Earth produced by rapid release of energy - Caused by motion of tectonic (lithospheric) plates.
Warm Up 09/26/2016 What are the three types of boundaries and explain the motion that occurs at each? What is produced at a Transform Boundary? What.
SICHUAN EARTHQUAKE May 12, 2008
Earthquakes Vocab.
Earth Science Turn in “Locating an Earthquake” activity from Friday!
Plate Tectonics Quiz What is a tectonic plate? (part of your answer should include the part of the earth that is tectonic plates.) What are the three kinds.
EARTHQUAKES Chapter 16 pg. 426.
San Andreas Fault Images
Earthquakes Forces Inside Earth
Chapter 6, Lesson 1, Earthquakes and Plate Boundaries
Presentation transcript:

Pelatihan : Techniques in Active Tectonic Study Juni 20-Juli 2, 2013 Instruktur: Prof. J Ramon Arrowsmith (JRA) Dari Arizona State University (ASU) - US Tempat Pelaksanaan: Ruang Pangea, Laboratorium Gempabumi (LabEarth) – Puslit Geoteknologi LIPI dan Kuliah lapangan akan dilakukan disekitar Sesar Lembang, Jawa Barat. * Lebih jelas baca TOR/KAK dan daftar acara

Earthquake cycle exploration using 2D dislocations: strike-slip Outline of this lecture Motivations from the San Andreas Fault Basic ideas of dislocations Strike-slip parallel displacements from simple screw dislocation model (Thatcher, 1990) A few examples Application to Izmit Earthquake

Areas of contrasting behavior along the San Andreas Fault (from Allen, 1968) Carrizo Plain

1906 M7.8 San Francisco Earthquake Beginning of modern earthquake science

1906 earthquake surface rupture. 8’ fence offset above enter/1906EQ/1906thumb.html And ages/fenceoffset_big.html ages/fenceoffset_big.html

“Reid’s elastic rebound hypothesis

Edge dislocation Screw dislocation Dislocation: simple idealization of displacement discontinuity in continuous body

Idealization of brittle crust with embedded strike slip fault (Thatcher, 1990)

Strike-slip parallel displacements from simple screw dislocation model (Thatcher, 1990)

1906 coseismic displacements

Best fit depth: 7000 m

Interseismic motion along the San Andreas Fault System (max arrow length=~50mm/yr relative to stable North America) Noriega, et al ; see also Schmalzle, et al., 2006 Thatcher, 1990 Plate Boundary Observatory velocity field

Young, et al., 2001

Feedback: Privacy Policy Feedback
Do Not Sell My Personal Information
About project: SlidePlayer Terms of Service

© 2025 SlidePlayer.com. Inc. All rights reserved.