Precambrian Basement Tectonics Beneath a CCS Site, Illinois Basin
Abstract
Characterization of Precambrian basement tectonics using 3D seismic
data is critical for fully constraining the geology of a carbon capture and storage (CCS) site. Our study applies state-of-the-art visualization and
attribute
analysis to a 3D
seismic
volume of the basement complex that underlies the Illinois Basin-Decatur Project CCS site. The most successful interpretative techniques used include geo-body analysis, X (east-west, cross-line)-directed amplitude change, and co-rendering (e.g., amplitude with semblance), integrated with gradient analysis. The 3D volume reveals a strong reflector deep within the basement complex that is interpreted to be a mafic sill, disrupted by a coherent pattern of prominent structural discontinuities. The discontinuities, which have a mutually orthogonal northwest-northeast trend, could have formed as part of the intrusion process, as post-emplacement tectonic faults, or a combination of both processes. Our preferred interpretation is that discontinuities are small faults with varying senses of offset. The most prominent of these is a narrow, well-defined northwest-striking crest or flexure in the igneous sill reflector. Injection-induced microseismicity describes a conspicuous pattern of northeast-trending clusters of events, some of which nucleated in the uppermost part of basement, directly over this crest. This distribution of
seismic
events is proposed to be controlled, in part, by fracture zones related to the crest and associated discontinuities in the mafic sill. These fractures would be oriented in directions to be critically stressed, resulting in microseismicity following pore pressure increases.
AAPG Datapages/Search and Discovery Article #90323 ©2018 AAPG Annual Convention and Exhibition, Salt Lake City, Utah, May 20-23, 2018