'Fault plane' diaporamas de présentation

Geology 12 -

Geology 12 -. Structural Geology. BIG IDEA The form, arrangement, and structure of rocks are affected by 3 dimensional forces over time. Rocks - Igneous, sedimentary, metamorphic. Forces - Pressure (think plate tectonics). Time - seconds to millions of years.

1.37k views • 85 slides

???????

???????. ? ??. 1. ?? 2. ?? 3. ?? 4. ????? 5. ???? 6. ?? 7. ???? 8. ??????? 9. ????? 10. ??. Structural geology. Structure. Ductile deformation Fold Foliation Lineation etc. Brittle deformation Joint Tension gash Styloite Fault etc. Fault.

453 views • 32 slides

491 views • 25 slides

Antonella Cirella, Alessio Piatanesi, Elisa Tinti, Massimo Cocco

403 views • 24 slides

??????? 2013 ? 6 ? 2 ??????????

??????? 2013 ? 6 ? 2 ??????????. ??? 1 , ?? 2 , ??? 1. 1 ????????????? 2 ????????????. Outline. Real-time Focal Mechanism Determination Generalized Cut and Paste method ( gCAP ) in 1D structure Revised Focal Mechanism in 3D Structure Improve focal mechanism solution in 3D structure

407 views • 21 slides

Yoshihiro Kaneko

376 views • 20 slides

590 views • 16 slides

Earthquakes and Hazards Blue Planet Lab 5 Components: Liquefaction demo/experiment

Earthquakes and Hazards Blue Planet Lab 5 Components: Liquefaction demo/experiment Liquefaction hazard in ABQ Measuring earthquake effects- Mercalli scale Contour mapping . Divergent Convergent Transform.

265 views • 14 slides

Wordlist 34 An Ocean Waiting to Happen

385 views • 14 slides

Slip on an earthquake fault

START. ?. Slip on an earthquake fault. Surface of the earth. Depth Into the earth. 100 km (60 miles). Distance along the fault plane. Slip on an earthquake fault Second 2.0. Slip on an earthquake fault Second 4.0. Slip on an earthquake fault Second 6.0.

301 views • 13 slides

Mountain Building

Mountain Building. Folding and Faulting. Stress in the Crust. Stress from plate motions causes crustal rocks to deform Rocks near the surface are cool and rigid . They will tend to fault ( break )

333 views • 11 slides

Structural G eology

Structural G eology . By: Maverick Irwin. faults. Fault plane. Hanging wall. The hanging wall of a fault is above the fault plane , and moves vertically horizontally or in both directions relative to the footwall.

204 views • 11 slides

FOLDS and FAULTS

1.04k views • 9 slides

Gravity results and interpretation Schurz, NV

Gravity results and interpretation Schurz, NV . by: Drew Jones and Marlon Ramos Gph 492/692, spring 2013 . Correction methods. Elevation Lattitude Instrument Drift Free Air Bouguer Slab Inner and Outer Terrain Used to Calculate Simple and Complete Bouguer Anomalies.

176 views • 9 slides

Earthquakes!!

Earthquakes!!. earthquakes. By Adriana Velasco And Allison Bogisich . By: Adriana velasco and Allison Bogisich. What is an earthquake?. The definition.

179 views • 8 slides

1.28k views • 5 slides

Types of Faults

Types of Faults. Strike Slip Fault: Two layers of rock are shifted horizontally or parallel to the fault plane. . 1) "Hanging Wall "- The surface of block that is ontop of the plane of the fault. 2) "Footwall" - The surface or block that lies below the plane of the fault.

396 views • 4 slides

Summary

New Earthquake Catalogs For Southern California And Their Use In Earthquake Forecasting Yan Y. Kagan, David D. Jackson and Yufang Rong, University of California, Los Angeles. Southern California Earthquake Catalog With Extended Sources. Summary

119 views • 1 slides

Aftershock statistics

142 views • 1 slides

DInSAR DATA AND PREVIOUS RESULTS

The Mw 7.9 Wenchuan (China) Earthquake: exploring the role of crustal heterogeneities from finite element analysis of DInSAR coseismic deformation. NE. SW. EGU2010-9315. C.Kyriakopoulos, E.Trasatti, S. Atzori, C.Bignami, M.Chini, S.Stramondo, and C.Tolomei

156 views • 1 slides