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   <subfield code="a">Initial seismic observations from a deep borehole drilled into the Canadian Shield in northeast Alberta</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[Judith Chan, Douglas Schmitt]</subfield>
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   <subfield code="a">The availability of a deep borehole in northeastern Alberta provides an unprecedented opportunity to study the in situ metamorphic craton rocks. This borehole reaches a depth of 2.4km, with 1.8km in the crystalline rocks, and is the only known borehole allowing access into the deeper rocks of the metamorphic Canadian Shield. In 2011, a zero-offset vertical seismic profile (VSP) was acquired to assist in the interpretation of seismic reflection data and geophysical logs. Three sets of upgoing tube waves interpreted from the raw profile correspond to the small-scale fluctuations in the borehole diameters and fracture zone in the crystalline rocks. A comparison between sonic log velocities and VSP velocities reveals a zone with increased velocity that could be due to the change in rock composition and texture in the basement rocks. The final processed profile is used to generate corridor stacks for differentiating between primary reflections and multiples in the seismic reflection profile. Analysis of the zero-offset VSP verifies existing log interpretation on the presence of fractures and the possible lithological changes in the metamorphic rocks of the Canadian Shield.</subfield>
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   <subfield code="a">The Author(s), 2014</subfield>
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   <subfield code="a">Zero-offset VSP</subfield>
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   <subfield code="a">Canadian Shield</subfield>
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   <subfield code="D">Judith</subfield>
   <subfield code="u">Department of Physics, Institute for Geophysical Research, University of Alberta, 4-181 CCIS, T6G 2E1, Edmonton, AB, Canada</subfield>
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   <subfield code="t">International Journal of Earth Sciences</subfield>
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   <subfield code="g">104/6(2015-09-01), 1549-1562</subfield>
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   <subfield code="a">Metadata rights reserved</subfield>
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