Mechanism of slab thickening near 670 km under Indonesia

Geophysical Research Letters

Volumn 27, Issue 6, 2000, Pages 831-834

  Das, Shamita ^a   Schöffel, Hans Joachim ^a   Gilbert, Freeman ^b  

^a UNIVERSITY OF OXFORD   (United Kingdom)

^b UNIVERSITY OF CALIFORNIA   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

CRUSTAL THICKENING; SLAB; SUBDUCTION ZONE;

INDONESIA;

GEOPHYSICS; DEVELOPING COUNTRIES; EARTHQUAKES; SEISMIC WAVES; SEISMOGRAPHS; SEISMOLOGY;

CONJUGATE FAULTS; DATA SET; INDONESIA; SEISMIC ZONES; WADATI-BENIOFF ZONES;

EARTHQUAKES; TECTONICS;

CONJUGATE FAULT PLANES; INDONESIA; WADATI-BENIOFF ZONE;

EID: 0034353333     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/1999GL010865     Document Type: Article

References (11)

1. Slab weakening by the exothermic olivine-spinel phase change
2. Effect of recent revisions to geomagnetic reversal time scale on estimates of current plate motions
3. Centroid-moment tensor solutions 1977-1997
4. Deep seismicity and modes of deformation in Tonga subduction zone
5. Centroid-moment tensor inversions of analog seismograms from deep earthquakes (1907-1976)
6. Centroid-moment tensor solutions for deep earthquakes predating the digital era; the world-wide standardized seismograph network dataset (1962-1976)
7. Metastable mantle phase transformations and deep earthquakes in subducting oceanic lithosphere
8. Depression of the 660 km discontinuity beneath the Tonga slab determined from near-vertical ScS reverberations
9. Fine details of the Wadati-Benioff zone under Indonesia and its geodynamic implications
10. The 1996 June 17 Flores Sea and 1994 March 9 Fiji-Tonga earthquakes: Source processes and deep earthquake mechanisms
11. Mainshock and aftershock analysis of the June 17, 1996, deep Flores Sea earthquake sequence: Implications for the mechanism of deep earthquakes and the tectonics of the Banda Sea