Nearest - WP2 30 months Progress Report Nearest 30 Months Meeting Brest, April 2-3, 2009 Task 2.2 Wide-Angle Seismic cruise.

Slides:



Advertisements
Similar presentations
Class 9. Mid-Ocean Ridges Dax Soule OCEAN/ESS 410.
Advertisements

© 2011 Pearson Education, Inc. CHAPTER 3 Marine Provinces.
8. Ocean Crustal Structure and Seismic Reflection William Wilcock (via Michelle W.) OCEAN/ESS 410.
Locating Plate Boundaries of the Pacific Rim
Place these notes in your Notebook.
OCEANIC TOPOGRAPHY By Greg Schwab May 7, Competency 39 The teacher understands structure and function of the hydrosphere The teacher understands.
12 Month Report on WP2: Tsunami source characterisation Nearest 12 Month Meeting Marrakech, October 25-26, 2007 WP Leader:
La Jolla, San Diego Small faults in San Diego & La Jolla yellow -> gen. fault trend red -> small faults Mt. Soledad formed by tectonic uplift N.
GG 450 April 15, 2008 Refraction Applications. While refraction is used for engineering studies such as depth to basement and depth to the water table,
Lecture 20 Turbidites and other deep- ocean sediments.
Bathymetry Study of the ocean floor and its contours Originally done by lowering a line over ship with a heavy weight Echo Sounder used a powerful sound.
Further topics in tectonics: 1.Focal mechanisms 2.Pac NW tectonic setting 3.Shape of mid-ocean ridges (depth of the ocean) 4.Driving forces of plate tectonics.
Seismic refraction surveys
HEAVY-OIL SEISMIC MONITORING at PIKES PEAK, SK I.A. Watson*, L.R. Lines and K.F. Brittle November 20, 2001.
Earthquake Focal Mechanisms
Bathymetry of the Ocean Floor The ocean floor is mapped by SONAR. (Sound navigation and ranging) Depth = (time x 1500 m/sec)/2 (round trip) At 25 degrees.
GG450 March 20, 2008 Introduction to SEISMIC EXPLORATION.
Work on GEOSTAR included ESONET LIDO - Demo Mission: the Cadiz node INGV activities D. Embriaco, G. Marinaro, G. Giovanetti, S. Monna, G. Cianchini, M.
NEAREST kick-off Meeting 9-11 October, Bologna NEARESTWP4 INGV: Leader PI: Paolo Favali.
SEG 3-D Elastic Salt Model
PROMESS 1 PARTNERS 1- Institut Français de Recherche pour l’Exploitation de la Mer (Ifremer)France 2- Istituto di Geologia Marina – CNR-IGMItaly 3- British.
The Oceans of the World 13.1.
FFCUL, PORTUGALBologna Oct 2006 NEAREST Coordinator: Maria Ana V Baptista NEAREST PARTNER - FFCUL PORTUGAL.
USGS – GeoPRISMS Synergistic Opportunities: Offshore Atlantic Margin Debbie Hutchinson Jason Chaytor Matt Arsenault Greg Mountain Ginger Barth Jon Childs.
Searching for blind faults: the Haiti subsurface imaging project ERAY KOCEL ERAY KOCEL with with Robert R. Stewart, Paul Mann, Robert R. Stewart, Paul.
G.S.I. Seabed Survey Seminar Possible Carbonate Mound Distribution November 2001 Thomas Furey.
FFCUL, PORTUGALBologna Oct 2006 NEAREST Coordinator: Maria Ana V Baptista NEAREST PARTNER FFCUL PORTUGAL.
WP1 WP1 - Tsunami sources Identification WP1 - Tsunami sources Identification FFCUL group Marrakesh, Oct
November 2001 iSIMM NERC/DTI LINK OCEAN MARGINS THEMATIC PROGRAMME Mapping & Modelling Heterogeneous Stretching & Volcanism on the NW European Atlantic.
Continental Margins and Ocean Basins. Continental Margins Three Main Divisions  Continental shelf  Continental slope  Continental rise.
Deep Ocean Technology & The Ocean Floor
Plan of Action Juan José Dañobeitia (UTM- CSIC) Evaluation Committe The Marine Technology Unit A Challenge for Oceanography Development in.
The effect of Plate Tectonics (Once again not a form of dubstep)
The Earth’s Oceans A Dynamic System where many physical and chemical changes are taking place!
U.S. Department of the Interior U.S. Geological Survey Preliminary Analysis of High- Resolution P-Wave Seismic Imaging Profiles Acquired Through Reno,
NEAREST Kick Off Meeting Bologna, 09/10/2006 WP2 Tsunami source characterisation.
New bathymetric data (Marion Dufresne July 2008).
Barcelona 8th-9th May 2008 NEAREST 2nd mid-year meeting Introduction.
Seismic phases and earthquake location
Bellringer Explain in complete sentences what are pros and cons of coal energy use.
© 2014 Pearson Education, Inc. Marine Provinces Chapter 1 Clickers Essentials of Oceanography Eleventh Edition Alan P. Trujillo Harold V. Thurman © 2014.
Instructor: Dr. C. Charles Dong,
Measuring bathymetry Ocean depths and topography of ocean floor
NEAREST FFCUL WP7 Modelling of tsunami impact in SW Portugal
Chapter Overview The study of bathymetry determines ocean depths and ocean floor topography. Echo sounding and satellites are efficient bathymetric tools.
Chapter 19 Study Notes: The Ocean Basins
NEAREST FFCUL WP7 Modelling of tsunami impact in SW Portugal
Laura Beranzoli Istituto Nazionale di Geofisica e Vulcanologia
Tectonics and The Provinces of the Oceans
Ifremer naval facilities
Ocean Bounty What does the ocean provide for us?
Lecture 7 Mapping the Ocean Floor Earth’s Internal Structure
Chapter 20.
Understanding Earth Fourth Edition Chapter 17:
The Ocean floor.
The Theory of Plate Tectonics
The Ocean Floor.
Ocean Features.
Bathymetry of the Ocean Floor
Acoustic Reflection 2 (distance) = (velocity) (time) *
Place these notes in your Notebook.
Oceanography.
Ocean Features.
The Ocean Basins.
Ocean Features.
Ocean Features.
CHAPTER 3 Marine Provinces
Ocean Features.
Ocean Features.
HAZARDS Seismic hazards
Presentation transcript:

Nearest - WP2 30 months Progress Report Nearest 30 Months Meeting Brest, April 2-3, 2009 Task 2.2 Wide-Angle Seismic cruise

Characterisation of the potential tsunami source areas Definition of the geometry and velocity structure of the continental margin offshore SW Iberia Definition of the main plate limits and geological domains Relate earthquake and tectonic structures, specially the deep décollement surfaces. Overall objective of WP2  Integration of existing MCS data (SWIM, Rifano, IAM, Sismar, etc) with newly acquired Wide-Angle Seismic data (Nearest-Seis survey). Nearest 30 Months Meeting Brest, April 2-3, 2009 Objectives

State of knowledge concerning the main active, potentially tsunamigenic structures > tectonic map as D1 Legacy data of MCS profiles re-processed up to PSDM > compilation as D4 (Task 2.1 -finished-)‏ Preparation of the Nearest-Seis survey, including assembly of instrumentation (OBS and guns), definition of scientific and technical teams, lines, vessel schedule, acquisition geometry, etc. Starting point (activities done in 2008)‏  Nearest-Seis survey took place between Oct 27 th and Nov 11 th on board R/V Hespérides Nearest 30 Months Meeting Brest, April 2-3, 2009 Starting point

Provide information on the physical properties of the crust as well as the crust-mantle boundary geometry Identify the nature of the crust (eg. oceanic vs. continental) and the limits of the different crustal domains Obtain information to construct a 3-D P-wave velocity model to be used to improve earthquake locations (WP3)‏ Specific objectives of Nearest-Seis Nearest 30 Months Meeting Brest, April 2-3, 2009 Specific objectives

Meeting presentations Bartolomé, R., Gràcia, E., Martínez-Loriente, S. and EVENT and NEAREST Teams (2009). Estructuras activas en el Golfo de Cádiz, 1ª Reunión del Proyecto de Excelencia de la Junta de Andalucía RNM 3713, 12 March 2009, Granada, Spain. Martínez-Loriente, S. (2009). Stratigraphy and structure of external Gulf of Cadiz from pre-stack depth migrated seismic profiles (SWIM-2006) implications for earthquake and tsunami hazard in SW Iberia, IPGP Doctoral Student Congress; March 2009; Paris, France. Publications Martínez-Loriente, S. (2009) "Estratigrafia i estructura de la part externa del Golf de Cadis basades en dades de sísmica de reflexió multicanal migrades en profunditat pre-stack". DEA report presented at the University of Barcelona. Martínez-Loriente, S., Gràcia, E., Bartolomé, R., Sallarès, V., Dañobeitia, J.J., and Swim-06 Cruise Party (2008). Pre-stack depth migration seismic imaging of the Coral Patch Ridge and adjacent Horseshoe and Seine Abyssal Plains (Gulf of Cadiz): Tectonic implications. Trabajos de Geología, ISSN: Falivene, O., Arbués, J., Ledo, J., Benjumea, B., Muñoz, J.A., Fernandez, O., Martínez-Loriente, S. (2008). Synthetic seismic from outcrop-derived reservoir-scale facies models, the Ainsa turbidite system (NE Spain). Submitted to AAPG Bulletin. Nearest 30 Months Meeting Brest, April 2-3, 2009

Nearest 30 Months Meeting Brest, April 2-3, 2009 Task 2.2 Wide-Angle Seismic cruise Took place between Oct 27 th (Cartagena) and Nov 11 th (Cadiz) on board BIO Hespérides: Length: 82,5 m Arm: 14,30 m Military crew : 52 Sci/tech crew: 29 Widely used for Antarctic operations Main Spanish seismic ship to date Task 2.2 Wide-Angle Seismic cruise Devoted to the acquisition of WAS data, together with complementary swath bathymetry, sediment profiler, gravity data

Nearest 30 Months Meeting Brest, April 2-3, 2009 Scientific/technical teams A total of 27 persons: 12 Scientific (9 institututions)‏ 12 Technical (5 OBS, 4 gunners, 2 shooting, 1 acoustics) 3 journalists (ZDF)‏ Task 2.2 Wide-Angle Seismic cruise

Nearest 30 Months Meeting Brest, April 2-3, 2009 Instrumentation 19 MicrOBS OBS from Ifremer/UBO 17 LC2000 OBS from UTM-CSIC 7 Hathor LEAS landstations (1 Hz)‏ 7 Bolt 1500LL guns ( c.i.)‏ Simrad EM120 multibeam (12 kHz)‏ Topas sediment profiler (3.5 kHz)‏ BGM-3 gravimeter Task 2.2 Wide-Angle Seismic cruise OBS Short period (4.5 Hz), 3 components seismometer Hydrophone Differ in size, weight, functioning and authonomy

Nearest 30 Months Meeting Brest, April 2-3, 2009 Gun array 4520 c.i. maximum (2 new guns were constructed), but only 3520 c.i. in most P1 12 m depth (notch at 80 Hz), 90 s shooting interval Useful bandwith between Hz (peak at 25 Hz)‏ Task 2.2 Wide-Angle Seismic cruise

Nearest 30 Months Meeting Brest, April 2-3, 2009 Task 2.2 Wide-Angle Seismic cruise WAS profiles P1 is 350 km long, with 29 OBS separated 5 nm in average P2 is 260 km long, with 15 OBS (7 nm) and 7 landstations

Nearest 30 Months Meeting Brest, April 2-3, 2009 Task 2.2 Wide-Angle Seismic cruise WAS profiles P1 is ~coincident with PSDM MCS lines SW13 and IAM4 P2 is coincident with PSDM MCS line SW01

Nearest 30 Months Meeting Brest, April 2-3, 2009 Task 2.2 Wide-Angle Seismic cruise WAS data along P1

Nearest 30 Months Meeting Brest, April 2-3, 2009 Task 2.2 Wide-Angle Seismic cruise WAS data along P1

Nearest 30 Months Meeting Brest, April 2-3, 2009 Task 2.2 Wide-Angle Seismic cruise WAS data along P1

Nearest 30 Months Meeting Brest, April 2-3, 2009 Task 2.2 Wide-Angle Seismic cruise WAS data along P2

Nearest 30 Months Meeting Brest, April 2-3, 2009 Task 2.2 Wide-Angle Seismic cruise WAS data along P2

Nearest 30 Months Meeting Brest, April 2-3, 2009 Task 2.2 Wide-Angle Seismic cruise WAS data along P2

Nearest 30 Months Meeting Brest, April 2-3, 2009 Task 2.2 Wide-Angle Seismic cruise WAS data along P2

Nearest 30 Months Meeting Brest, April 2-3, 2009 Task 2.2 Wide-Angle Seismic cruise Earthquakes recorded by OBS Waveforms from OBSs 8 ( top), 13 (mid), 14 (bottom), P1 profile (right).

Nearest 30 Months Meeting Brest, April 2-3, 2009 Task 2.3 Processing and modelling of WAS data Task 2.3 Processing and modelling All data have been pre-processed (record sections constructed, clock correction done, OBS relocated, bandpass filtering done)‏ P2 has been modeled (preliminary model by A. Gailler)‏ P1 will be modeled by S. Martínez (starting next week)‏

Nearest 30 Months Meeting Brest, April 2-3, 2009 Gantt Table Task 2.3 Processing and modelling