A seismic reflection profile across the Cascadia Subduction Zone offshore central Oregon: New constraints on methane distribution and crustal structure

1995 ◽  
Vol 100 (B8) ◽  
pp. 15101-15116 ◽  
Author(s):  
Anne M. Tréhu ◽  
Guibiao Lin ◽  
Edward Maxwell ◽  
Chris Goldfinger
Keyword(s):  
Subduction Zone ◽  
Crustal Structure ◽  
Seismic Reflection ◽  
Cascadia Subduction Zone ◽  
Seismic Reflection Profile ◽  
Reflection Profile ◽  
Methane Distribution

Crustal structure of the transpressional Variscan orogen of SW Iberia: SW Iberia deep seismic reflection profile (IBERSEIS)

Tectonics ◽  
2003 ◽  
Vol 22 (6) ◽  
pp. n/a-n/a ◽  
Author(s):  
J. F. Simancas ◽  
R. Carbonell ◽  
F. González Lodeiro ◽  
A. Pérez Estaún ◽  
C. Juhlin ◽  
...  
Keyword(s):  
Crustal Structure ◽  
Seismic Reflection ◽  
Seismic Reflection Profile ◽  
Deep Seismic Reflection ◽  
Reflection Profile ◽  
Variscan Orogen ◽  
Deep Seismic Reflection Profile

Probing Fine Crustal Structure in the Beijing Region Using a Deep Seismic Reflection Profile

2009 ◽  
Vol 52 (5) ◽  
pp. 953-961
Author(s):  
Bao-Jin LIU ◽  
Ping HU ◽  
Yong-Qi MENG ◽  
Shao-Ying FENG ◽  
Jin-Hu SHI ◽  
...  
Keyword(s):  
Crustal Structure ◽  
Seismic Reflection ◽  
Seismic Reflection Profile ◽  
Deep Seismic Reflection ◽  
Reflection Profile ◽  
Deep Seismic Reflection Profile

Crustal structure across the Caledonides from the ‘WINCH’ seismic reflection profile: influences on the evolution of the Midland Valley of Scotland

1984 ◽  
Vol 75 (2) ◽  
pp. 97-109 ◽  
Author(s):  
J. Hall ◽  
J. A. Brewer ◽  
D. H. Matthews ◽  
M. R. Warner
Keyword(s):  
Crustal Structure ◽  
Crustal Deformation ◽  
Seismic Reflection ◽  
Deep Structure ◽  
Sedimentary Basins ◽  
Seismic Reflection Profile ◽  
Crustal Shortening ◽  
The North ◽  
Reflection Profile ◽  
Deep Seismic Reflection Profile

ABSTRACTThe Western Isles–North Channel (‘WINCH’) deep seismic reflection profile runs through the North Channel across the extension of the Midland Valley into the Firth of Clyde.A variety of shallow Carboniferous and younger sedimentary basins dominates the upper crustal structure. The deep structure includes a reflective lower crust, bounded downwards by the Moho, and dipping ‘thrusts’. No margins to the Midland Valley are observed equivalent to the bounding faults on land. Thrusts below both the Highlands and the Southern Uplands have a variety of dip directions indicative of zig-zag crustal shortening of 100 km in the Highlands and 60 km in the Southern Uplands.The Moho varies only a little in depth, despite the gross crustal deformation in the Caledonides. Isostatic recovery of the Moho on unlocking of collided crustal blocks may explain the formation of some sedimentary basins.

scholarly journals Brasiliano crustal structure and the tectonic setting of the Parnaíba basin of NE Brazil: Results of a deep seismic reflection profile

Tectonics ◽  
2014 ◽  
Vol 33 (11) ◽  
pp. 2102-2120 ◽  
Author(s):  
Michael C. Daly ◽  
Vander Andrade ◽  
Chuck A. Barousse ◽  
Rafaela Costa ◽  
Kenneth McDowell ◽  
...  
Keyword(s):  
Crustal Structure ◽  
Seismic Reflection ◽  
Tectonic Setting ◽  
Seismic Reflection Profile ◽  
Deep Seismic Reflection ◽  
Reflection Profile ◽  
Parnaíba Basin ◽  
Deep Seismic Reflection Profile
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