Synthesis of the crustal structure of the transform continental margin off Ghana, northern Gulf of Guinea

1997 ◽  
Vol 17 (1) ◽  
pp. 12-20 ◽  
Author(s):  
R. A. Edwards ◽  
R. B. Whitmarsh ◽  
R. A. Scrutton
2013 ◽  
Vol 194 (1) ◽  
pp. 362-366 ◽  
Author(s):  
Yingjie Xia ◽  
Sidao Ni ◽  
Xiangfang Zeng

Abstract Based on studies of continuous waveform data recorded on broad-band seismograph stations in Africa, Europe and North America, we report evidences for two temporally persistent and spatially localized monochromatic vibrating sources (around 0.036 and 0.038 Hz, respectively) in the Gulf of Guinea, instead of just one source (0.038 Hz or 26 s) found 50 yr ago. The location of the 0.036 Hz source is close to the Sao Tome Volcano, therefore it may be related to volcano processes. However, the 0.038 Hz source cannot be explained with known mechanisms, such as tectonic or oceanic processes. The most likely mechanism is volcano processes, but there is no reported active volcano in source region. Such repetitive vibration sources may provide valuable tools for detecting temporal variation of crustal structure of the Earth.


Tectonics ◽  
2018 ◽  
Vol 37 (5) ◽  
pp. 1576-1604 ◽  
Author(s):  
M. Druet ◽  
A. Muñoz-Martín ◽  
J. L. Granja-Bruña ◽  
A. Carbó-Gorosabel ◽  
J. Acosta ◽  
...  

Author(s):  
G. Drivenes ◽  
M. A. Sellevoll ◽  
V. Renard ◽  
F. Avedik ◽  
J. Pajchel

2013 ◽  
Vol 599 ◽  
pp. 170-196 ◽  
Author(s):  
Volker Thor Leinweber ◽  
Frauke Klingelhoefer ◽  
Sönke Neben ◽  
Christian Reichert ◽  
Daniel Aslanian ◽  
...  

2017 ◽  
Vol 154 (4) ◽  
pp. 903-913 ◽  
Author(s):  
ALAN DICKIN ◽  
JACOB STRONG ◽  
GABRIEL ARCURI ◽  
ANNIKA VAN KESSEL ◽  
LUCIA KRIVANKOVA-SMAL

AbstractThe Grenville Province forms the exhumed remnants of a 1.1 Ga collisional orogeny that telescoped an older continental margin. Terranes with distinct crustal formation ages can be mapped using Nd isotopes, revealing a ramp–flat thrust structure. The ramp is identified by the presence of retrogressed eclogites, and its trajectory is refined using Nd model ages. The main allochthon is locally overlain by the Parry Sound klippe, but is also underlain by a tectonic duplex. Northwest-directed nappes represent remnants of a corrugated thrust sheet, but a ring-shaped remnant was also preserved where the thrust sheet was down-buckled under the dense rocks of Parry Sound domain.


2004 ◽  
Vol 25 (3-4) ◽  
pp. 283-304 ◽  
Author(s):  
Wilfried Jokat ◽  
Oliver Ritzmann ◽  
Christian Reichert ◽  
Karl Hinz

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