New bathymetric data (Marion Dufresne July 2008).

Slides:



Advertisements
Similar presentations
Cascadia Ken Creager, Steve Malone, Geoff Abers, Stephane Rondenay, Brad Hacker and Tim Melbourne Earth and Space Sciences University of Washington.
Advertisements

Conjugate Passive Rifted Margins Separated by Rapid Strain Rate 1 – The Southern Margin Preliminary Insights to the Crust and Upper Mantle Structure of.
ISOSTASY Removal of material from the top will induce uplift at the surface. Removal of material from the bottom will produce subsidence. Thus, in the.
Crustal Structure and Deformation in the Northern California Coast Ranges Gavin P. Hayes 1, Kevin P. Furlong 1, S. Schwartz 2, C. Hall 2, C. Ammon 1 1.
Chapter 17 Earth’s interior. Earth’s interior structure Earth is composed of three shells; –Crust –Mantle –Core.
EarthScope targets in the central Appalachians Eastern US continental margin preserves the signature of several cycles of supercontinent assembly and breakup.
Article 76, paragraph 4 a) “For the purposes of this Convention, the coastal State shall establish the outer edge of the continental margin wherever the.
The Planet Oceanus. 2-1 The Earth’s Structure Earth consists of a series of concentric layers or spheres which differ in chemistry and physical properties.
Near-Bottom Sedimentation Offshore Southwestern Taiwan from Echo Character Study Jui-kun Chiu, Cher-Shine Liu Institute of Oceanography National Taiwan.
12 Month Report on WP2: Tsunami source characterisation Nearest 12 Month Meeting Marrakech, October 25-26, 2007 WP Leader:
Walter D. Mooney, Ph.D. US Geological Survey Menlo Park, California USA Lecture #15: Continental Margins IPRCC and SinoProbe Short Course:
Exploring the inner and outer shells of earth. Earth consists of a series of concentric layers or spheres which differ in chemistry and physical properties.
Relative plate velocities based on seafloor spreading rates and directions plus directions from earthquake slip vectors.
Topic: The End is Just the Beginning... Leg 194 Wrap-up Broadcast 7: February 28, 2001 Mrs. Joan Linsley.
(Chapter 10 in D & R) Geometry and Kinematics: Plates.
SEEING FROM HEARING VISUALIZING CRUSTAL THICKNESS FROM ACTIVE- SOURCE SEISMOLOGY..
Seismicity, Major Structural Elements and Required Tsunami Early Warning System for Makran (Sea of Oman) Region Dr. Mohammad Mokhtari Director of National.
THE EVOLUTION OF OCEAN BASINS
Integrated 2-D and 3-D Structural, Thermal, Rheological and Isostatic Modelling of Lithosphere Deformation: Application to Deep Intra- Continental Basins.
Magnetic anomaly number age (Ma) from geomagnetic reversal chronology extrapolated in South Atlantic assuming constant rate of spreading paleontological.
Total Heat Loss of the Earth and Heat Production in the Continental Crust Makoto Yamano Earthquake Research Institute, University of Tokyo, Japan.
Walter D. Mooney, Ph.D. US Geological Survey Menlo Park, California USA Lecture #10: Lithosphere of Young Mountain Belts IPRCC and SINOPROBE.
Sea Floor Spreading & the Plate Tectonics Revolution ( ) The research ship Horizon Scripps Institution of Oceanography
USGS – GeoPRISMS Synergistic Opportunities: Offshore Atlantic Margin Debbie Hutchinson Jason Chaytor Matt Arsenault Greg Mountain Ginger Barth Jon Childs.
Integrated and Comparative Geophysical Studies of Crustal Structure of Pull-apart Basins: The Salton Trough and Death Valley, California Regions.
17.1 Notes: Earth’s Mantle & Crust Continental crust Thickness: Continental crust is thicker (30-40Km) Age: older (up to 4.4 billion yrs old) Composition:
Chronology of geomagnetic field reversals magnetic anomaly “number” Ocean floor age, millions of years (Ma), determined largely from deep sea drilling.
Earthquakes and the Interior  Earthquakes are definitely a geologic hazard for people living in earthquake regions, but the seismic waves generated by.
Tom Wilson, Department of Geology and Geography tom.h.wilson tom. Department of Geology and Geography West Virginia University Morgantown,
Nearest - WP2 30 months Progress Report Nearest 30 Months Meeting Brest, April 2-3, 2009 Task 2.2 Wide-Angle Seismic cruise.
EXTENSION AND MAGMATISM AT THE GOBAN SPUR RIFTED CONTINENTAL MARGIN: GEOPHYSICAL AND GEOCHEMICAL APPROACHES T. A. Minshull 1, A. D. Bullock 1, S. M. Dean.
Other Tectonic Rifts: the Woodlark-D'Entrecasteaux Rift, Papua New Guinea Geoffrey Abers, Boston University Thanks to: A. Ferris (BU), S. Baldwin (Syracuse),
Gravity IV: Dipole moment of density anomaly: the ambiguity
The effect of Plate Tectonics (Once again not a form of dubstep)
The Structure of the Earth and Plate Tectonics. Structure of the Earth The Earth is made up of 3 main layers: –Core –Mantle –Crust Inner core Outer core.
The Global Ocean The Vast World Ocean.
Glenn Spinelli Effects of fluid circulation in ocean crust on subduction zone temperatures and metamorphism.
The India - Eurasia collision, Himalaya and the Tibetan plateau.
Gravity anomalies and flexure at the West Taiwan basin:
NEAREST Kick Off Meeting Bologna, 09/10/2006 WP2 Tsunami source characterisation.
TRIN - Gail L. Christeson
Isostasy in Geology and Basin Analysis This exercise is drawn from Angevine, Heller and Paola (1990), with inspiration and essential planning by R. Dorsey.
Extent of new, non-oceanic crust in the northern Gulf of California: Constraints and Controversies Joann Stock Caltech.
Crustal Structure using the tomography method, in the central part of Itoigawa-Shizuoka Tectonic Line (ISTL), Japan. Presenter: Hirata Naoshi Panayotopoulos.
Costa Rica Seismogenesis Project OBJECTIVES: Explain causes of seismogenic behavior along convergent margins that erode rather than accrete. Record low.
Seismogenic Characteristics and Seismic Structure of the Mariana Arc: Comparison with Central America Douglas A. Wiens, James Conder, Sara Pozgay, Mitchell.
Tom.h.wilson tom. Department of Geology and Geography West Virginia University Morgantown, WV More about Isostacy.
What is the thermal structure of a subduction zone?
Gravity modeling as guidance for salt interpretation: a case study from the Western Gulf of Mexico Irina Filina* (formerly at Hess Corporation, currently.
Measuring bathymetry Ocean depths and topography of ocean floor
Nils Holzrichter, Jörg Ebbing
Carla Braitenberg Department of Mathematics and Geosciences
THE EVOLUTION OF OCEAN BASINS. 1. THE EVOLUTION OF OCEAN BASINS An individual ocean basin grows from: - An initial rift, reaches a maximum size, then.
Lecture 7 Mapping the Ocean Floor Earth’s Internal Structure
Internal Structure of the Earth
William W. Sager, Department of Oceanography, Texas A&M University
CHAPTER 2 Plate Tectonics and the Ocean Floor
The Missing Piece of Wegener’s Continental Drift Puzzle
Application to the Iberian Margin
William W. Sager, Department of Oceanography, Texas A&M University
Geophysics/Tectonics
by Satish C. Singh, and Raphaële Moeremans
South China Sea crustal thickness and oceanic lithosphere distribution from satellite gravity inversion by Simon Gozzard, Nick Kusznir, Dieter Franke,
Midcontinent Rift (MCR)
Finding The SLO Moho GOAL: Estimate Crustal Thickness Beneath San Luis Obispo & Coastal California.
Sensitivity of crustal thickness and continental lithosphere thinning determined from gravity inversion to sediment thickness used in the gravity inversion.
by Alan M. Roberts, Andrew D. Alvey, and Nick J. Kusznir
Introduction to Earth Structure
Interpreted seismic reflection image across reactivated fracture zones
Crustal cross-sections with Moho from gravity-anomaly inversion along line 1. Crustal cross-sections with Moho from gravity-anomaly inversion along line.
Presentation transcript:

New bathymetric data (Marion Dufresne July 2008)

New bathymetric data (Marion Dufresne July 2008)

New bathymetric data (Marion Dufresne July 2008)

Depth to basement map [MCS and OBS data] (Thiebot and Gutscher, 2006)

Sediment thickness map - W of Gibraltar (Gutscher et al., accepted Tectonophys.)

Depth to Moho map (Gutscher et al., accepted Tectonophys.)

Crustal thickness map [S. Iberia - N. Morocco] (Gutscher et al., accepted Tectonophys.)

Extent of oceanic crust ?

Proposed OBS lines

Proposed OBS lines, SWIM bathymetry and MCS lines

Regional seismicity (PDE Catalog )

Seismicity (29 Aug July 2008) (recorded by land stations) SWIM 2008 Cruise Report (L. Matias)

Seismicity (29 Aug July 2008) within 75 km of OBS-BB network SWIM 2008 Cruise Report (L. Matias)

Proposed OBS lines

Proposed OBS lines P1: - too long / too many deployments, total 36 (thus compromising other lines) [10 OBS in Tagus, 6 on and S of thrust belt, 3 overlap SISMAR OBS] - very deep water (very long recovery time) Tagus 5000m, HAP 4800m, SAP 4200m - little new info on crustal types (except perhaps Tagus) - 50% of line has no seismicity, and is distant from OBS-BB network

Proposed OBS lines P2: - shortest distance between the SW Iberian (continental) margin and the NW Moroccan (continental margin) crossing thin crust of uncertain type - passes along existing high quality MCS profile (pre-stack depth migrated) - crosses Marq. Pombal and the toe of the accretionary wedge (potentially seismogenic structures)

Free-air gravity anomaly (and SISMAR seismic profiles)

Kinematic reconstruction 195Ma (Sahabi et al., 2004)

Kinematic reconstruction 195Ma (Sahabi et al., 2004) w. magnetic anomalies (from Verhoef et al., 1991)

Magnetic anomaly maps (Verhoef et al., 1991)

Magnetic anomaly maps Iberian aero-mag map (left) (Verhoef et al., below)

Extent of oceanic crust ?