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Abstract

3D seismic measurements have been performed in 2012 to explore a petrothermal reservoir in a crystalline environment (granite intrusion, metamorphic cover) within the Erzgebirge in Saxony. The intention and challenge is to image and characterize a steeply dipping fault zone with potentially permeable fracture zones at target depths of 5-6 km and temperatures well above 150 °C. The vibroseis technique was used in the experiment. A suite of imaging methods has been applied, from conventional CMP-stacking, CRS processing to pre-stack migrations.

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/content/papers/10.3997/2214-4609.20140512
2014-06-16
2024-04-23
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20140512
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