The 1994-2004 Al Hoceima (Morocco) earthquake sequence ... - ESA

The 1994-2004 Al Hoceima (Morocco) earthquake sequence ... - ESA The 1994-2004 Al Hoceima (Morocco) earthquake sequence ... - ESA

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The 1994-2004 1994 2004 Al Hoceima (Morocco) earthquake sequence: Conjugate fault ruptures deduced from InSAR A. Akoglu (1), Z. Cakir* Cakir (2), M. Meghraoui (2), N. Jabour (3), S. Belabbes (2), L. Ait-Brahim Ait Brahim (4), S. Ergintav (5) (1) ITU, Istanbul, Turkey; (2) IPG Strasbourg, France; (3) CNRST, CNRST, Rabat, Morocco; (4) U. Mohammed V, Rabat, Morocco Morocco (5) TUBITAK MRC, Izmit, Turkey; * presenter ESA CAT-1 CAT 1 2532 project 1/18

<strong>The</strong> <strong>1994</strong>-<strong>2004</strong> <strong>1994</strong> <strong>2004</strong> <strong>Al</strong> <strong>Hoceima</strong> (<strong>Morocco</strong>) <strong>earthquake</strong> <strong>sequence</strong>:<br />

Conjugate fault ruptures deduced from InSAR<br />

A. Akoglu (1), Z. Cakir* Cakir (2), M. Meghraoui (2), N. Jabour (3),<br />

S. Belabbes (2), L. Ait-Brahim Ait Brahim (4), S. Ergintav (5)<br />

(1) ITU, Istanbul, Turkey; (2) IPG Strasbourg, France; (3) CNRST, CNRST,<br />

Rabat, <strong>Morocco</strong>; (4) U. Mohammed V, Rabat, <strong>Morocco</strong> <strong>Morocco</strong><br />

(5) TUBITAK MRC, Izmit, Turkey;<br />

* presenter<br />

<strong>ESA</strong> CAT-1 CAT 1 2532 project<br />

1/18


<strong>The</strong> <strong>1994</strong> and <strong>2004</strong> <strong>Al</strong> <strong>Hoceima</strong> <strong>earthquake</strong>s<br />

2/18


Proposed ruptures for the <strong>1994</strong> and <strong>2004</strong><br />

<strong>earthquake</strong>s<br />

<strong>1994</strong><br />

<strong>2004</strong><br />

3/18


InSAR data<br />

4/18


InSAR data<br />

5/18


230<br />

Solutions from InSAR<br />

280<br />

6/18


<strong>1994</strong><br />

<strong>2004</strong><br />

Coseismic interferograms<br />

ascending descending<br />

7/18


<strong>1994</strong><br />

<strong>2004</strong><br />

Location of the <strong>1994</strong> <strong>earthquake</strong> rupture<br />

ascending descending<br />

8/18


<strong>1994</strong><br />

<strong>2004</strong><br />

Locations of the <strong>1994</strong>-<strong>2004</strong> <strong>1994</strong> <strong>2004</strong> <strong>earthquake</strong>s ruptures<br />

ascending descending<br />

9/18


<strong>1994</strong><br />

<strong>2004</strong><br />

Modeling coseismic interferograms<br />

with Poly3D<br />

ascending descending<br />

10/18


Modeling the <strong>2004</strong> <strong>earthquake</strong><br />

Cakir et al., BSSA in press<br />

11/18


<strong>1994</strong><br />

<strong>2004</strong><br />

Best models for the <strong>1994</strong> & <strong>2004</strong><br />

interferograms<br />

ascending descending<br />

12/18


<strong>1994</strong><br />

<strong>2004</strong><br />

Residuals (observed – modeled)<br />

ascending descending<br />

13/18


Modeled slip distributions<br />

14/18


Proposed fault ruptures for<br />

the <strong>1994</strong> and <strong>2004</strong> <strong>earthquake</strong>s<br />

15/18


Proposed fault ruptures for<br />

the <strong>1994</strong> and <strong>2004</strong> <strong>earthquake</strong>s<br />

16/18


Stress field in the <strong>Al</strong> <strong>Hoceima</strong> region<br />

(See poster of Belabbes et al. for details)<br />

17/18


Summary of conclusions<br />

• <strong>The</strong> <strong>1994</strong> & <strong>2004</strong> <strong>earthquake</strong>s in the Rif mountains took<br />

place on N31°E and N43°W trending conjugate faults.<br />

• Modeled faults are consistent with focal mechanism<br />

solutions.<br />

• <strong>The</strong> Rif is now deforming under a strike-slip regime.<br />

• InSAR appears to be the best method for characterizing<br />

the seismic source parameters, especially in the<br />

absence of surface faulting.<br />

18/18


Acknowledgments ☺<br />

European Space Agency provided Envisat ASAR<br />

and ERS1-2 ERS1 2 SAR data under the projects:<br />

AOTR.2436 (Interseismic Strain Accumulation and Earthquake Mechanisms Mechanisms<br />

in<br />

Turkey and Surrounding Regions Using Envisat and ERS SAR<br />

Interferometry [PI:Z.Cakir [ PI:Z.Cakir]) ])<br />

CAT1-2532 CAT1 2532 (Studying crustal deformation in Middle East and North Africa Africa<br />

using<br />

SAR Interferometry [PI:M.Meghraoui<br />

[ PI:M.Meghraoui]) ])<br />

Financial support is from EC project RELIEF and<br />

APAME<br />

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