Partial breaking of a mature seismic gap: The 1987 earthquakes in New Britain

1991 ◽  
Vol 136 (4) ◽  
pp. 459-477 ◽  
Author(s):  
R. Dmowska ◽  
L. C. Lovison-Golob ◽  
J. J. Durek
Keyword(s):  
Seismic Gap ◽  
New Britain

Partial Breaking of a Mature Seismic Gap: The 1987 Earthquakes in New Britain

1991 ◽  
pp. 459-477
Author(s):  
R. Dmowska ◽  
L. C. Lovison-Golob ◽  
J. J. Durek
Keyword(s):  
Seismic Gap ◽  
New Britain

New Britain Thrush (Zoothera talaseae)

2020 ◽  
Author(s):  
Josep del Hoyo ◽  
Nigel Collar ◽  
David Christie
Keyword(s):  
New Britain

New Britain Bronzewing (Henicophaps foersteri)

2020 ◽  
Author(s):  
Luis F. Baptista ◽  
Pepper W. Trail ◽  
H.M. Horblit ◽  
Eduardo de Juana ◽  
Peter F. D. Boesman ◽  
...  
Keyword(s):  
New Britain

Petroglyphs and place: complex histories at four sites in New Britain

2021 ◽  
Author(s):  
JIM SPECHT ◽  
ROBIN TORRENCE ◽  
KEN MULVANEY
Keyword(s):  
New Britain

Estimation of site response functions for the central seismic gap of Himalaya, India

2021 ◽  
Author(s):  
Anjali Sharma ◽  
Renu Yadav ◽  
Dinesh Kumar ◽  
Ajay Paul ◽  
S. S. Teotia
Keyword(s):  
Site Response ◽  
Seismic Gap ◽  
Response Functions ◽  
Central Seismic Gap

scholarly journals Plate Coupling Mechanism of the Central Andes Subduction: Insight from Gravity Model

2019 ◽  
Vol 9 (1) ◽  
pp. 13-21
Author(s):  
Rezene Mahatsente
Keyword(s):  
Subduction Zone ◽  
Continental Crust ◽  
Gravity Model ◽  
Central Andes ◽  
High Density ◽  
Seismic Gap ◽  
Coupling Mechanism ◽  
Crust And Upper Mantle ◽  
Velocity Models ◽  
Plate Coupling

Abstract The Central Andes experienced major earthquake (Mw =8.2) in April 2014 in a region where the giant 1877 earthquake (Mw=8.8) occurred. The 2014 Iquique earthquake did not break the entire seismic gap zones as previously predicted. Geodetic and seismological observations indicate a highly coupled plate interface. To assess the locking mechanism of plate interfaces beneath Central Andes, a 2.5-D gravity model of the crust and upper mantle structure of the central segment of the subduction zone was developed based on terrestrial and satellite gravity data from the LAGEOS, GRACE and GOCE satellite missions. The densities and major structures of the gravity model are constrained by velocity models from receiver function and seismic tomography. The gravity model defined details of crustal and slab structure necessary to understand the cause of megathrust asperity generation. The densities of the upper and lower crust in the fore-arc (2970 – 3000 kg m−3) are much higher than the average density of continental crust. The high density bodies are interpreted as plutonic or ophiolitic structures emplaced onto continental crust. The plutonic or ophiolitic structures may be exerting pressure on the Nazca slab and lock the plate interfaces beneath the Central Andes subduction zone. Thus, normal pressure exerted by high density fore-arc structures and buoyancy force may control plate coupling in the Central Andes. However, this interpretation does not exclude other possible factors controlling plate coupling in the Central Andes. Seafloor roughness and variations in pore-fluid pressure in sediments along subduction channel can affect plate coupling and asperity generation.

Fitting copulas to bivariate earthquake data: the seismic gap hypothesis revisited

2008 ◽  
Vol 19 (3) ◽  
pp. 251-269 ◽  
Author(s):  
Aristidis K. Nikoloulopoulos ◽  
Dimitris Karlis
Keyword(s):  
Seismic Gap ◽  
Earthquake Data
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