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A wide-angle seismic traverse through the Variscan of southwest Ireland

Urheber*innen

Masson,  F.
External Organizations;
Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

Jacob,  A. W. B.
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Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

Prodehl,  C.
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Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

Readman,  P. W.
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Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

Shannon,  P. M.
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Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

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Schulze,  Albrecht
Deutsches GeoForschungsZentrum;
Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

Enderle,  U.
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Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

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227898.pdf
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Zitation

Masson, F., Jacob, A. W. B., Prodehl, C., Readman, P. W., Schulze, A., Enderle, U. (1998): A wide-angle seismic traverse through the Variscan of southwest Ireland. - Geophysical Journal International, 134, 3, 689-705.
https://doi.org/10.1046/j.1365-246x.1998.00572.x


Zitierlink: https://gfzpublic.gfz-potsdam.de/pubman/item/item_227898
Zusammenfassung
A wide-angle seismic profile across the western peninsulas of SW Ireland was performed. This region corresponds to the northernmost Variscan thrust and fold deformation. The dense set of 13 shots and 109 stations along the 120 km profile provides a detailed velocity model of the crust. The seismic velocity model, obtained by forward and inverse modelling, defines a five-layer crust. A sedimentary layer, 5-8 km thick, is underlain by an upper-crustal layer of variable thickness, with a base generally at a depth of 10-12 km. Two mid-crustal layers are defined, and a lower-crustal layer below 22 km. The Moho lies at a depth of 30-32 km. A low-velocity zone, which coincides with a well-defined gravity low, is observed in the central part of the region and is modelled as a Caledonian granite which intruded upper-crustal basement. The granite may have acted as a buffer to northward-directed Variscan thrusting. The Dingle-Dungarvan Line (DDL) marks a major change in sedimentary and crustal velocity and structure. It lies immediately to the north of the velocity and gravity low, and shows thickness and velocity differences in many of the underlying crustal layers and even in the Moho. This suggests a deep, pre-Variscan control of the structural development of this area. The model is compatible with thin-skinned tectonics, which terminated at the DDL and which incorporated thrusts involving the sedimentary and upper-crustal layers.