{"id":{"repo_id":"uiuc","oai_identifier":"oai:www.ideals.illinois.edu:2142/78424"},"canonical_url":"https://search.dev.ndltd.org/etd/uiuc/oai:www.ideals.illinois.edu:2142/78424","repository":{"repo_id":"uiuc","name":"University of Illinois - Urbana-Champaign","base_url":"https://www.ideals.illinois.edu/oai-pmh"},"display":{"title":"Depositional characterization of the Eau Claire Formation at the Illinois Basin - Decatur Project: facies, mineralogy and geochemistry","abstract":"The Cambrian-age Eau Claire Formation serves as the primary seal at the Illinois Basin – Decatur Project (IBDP), a one million tonne carbon capture and storage demonstration project located in Decatur, Illinois. The Eau Claire Formation conformably overlies the Mt. Simon Sandstone, the reservoir for the IBDP. At the IBDP site, analysis of drill core and geophysical logs reveals the Eau Claire consists of two major lithostratigraphic units: a siliciclastic dominant lower unit and a carbonate dominant upper unit. Within the Eau Claire, four major depositional facies exist within a tidally influenced, shallow marine depositional environment. These include (Unit A) intertidal mixed sand/mud flats and tidal channels of the foreshore environment; (Unit B) subtidal deposits of the offshore transition zone; (Unit C) subtidal deposits of the upper shoreface environment; and (Unit D) subtidal mixed carbonate/siliciclastic deposits. An approximately +8‰ δ13C excursion (R2 = 0.97) defines the Eau Claire at the IBDP site, possibly correlative with the Steptoean positive carbon isotope excursion (SPICE) found worldwide 500– 495 Ma ago. This study aims to elucidate the depositional environment, seal quality, age and provenance of the Eau Claire Formation in central Illinois. The mineralogy of the four depositional facies varies widely throughout the Eau Claire, with a persistently high K-feldspar content. The K-feldspar mode averages 8.7% for the formation and reaches an average of 20.3% in Unit C. Unit A is approximately 30 ft. (9.1 m) thick and exhibits intense bioturbation, ripple beds, and flaser/lenticular bedding, with an average porosity and permeability (n = 20) of 6.7% and 8.6 mD. Unit B is an approximately 40 ft. (12.2 m) thick tight shale sequence, with thin siltstones interbedded throughout. Unit B represents the most desirable seal facies in the formation with an average porosity (n=9) and permeability (n=4) of 5.6% and 2.0x10-5 mD. Unit C is the largest siliciclastic unit in the formation, spanning an average of 95 ft. (29 m) in all three wells at the IBDP. Unit C exhibits the classic tidalite signature of rhythmically interbedded siltstones and shales, with an average porosity and permeability (n = 50) of 9.4% and 0.9 mD. Unit D spans approximately 345 ft. (105.2 m) and begins as a mixed siliciclastic/carbonate environment, slowly becoming a dolomitized carbonate shelf dominated by oolitic packstone and grainstone.","abstract_html":"The Cambrian-age Eau Claire Formation serves as the primary seal at the Illinois Basin – Decatur Project (IBDP), a one million tonne carbon capture and storage demonstration project located in Decatur, Illinois. The Eau Claire Formation conformably overlies the Mt. Simon Sandstone, the reservoir for the IBDP. At the IBDP site, analysis of drill core and geophysical logs reveals the Eau Claire consists of two major lithostratigraphic units: a siliciclastic dominant lower unit and a carbonate dominant upper unit. Within the Eau Claire, four major depositional facies exist within a tidally influenced, shallow marine depositional environment. These include (Unit A) intertidal mixed sand/mud flats and tidal channels of the foreshore environment; (Unit B) subtidal deposits of the offshore transition zone; (Unit C) subtidal deposits of the upper shoreface environment; and (Unit D) subtidal mixed carbonate/siliciclastic deposits. An approximately +8‰ δ13C excursion (R2 = 0.97) defines the Eau Claire at the IBDP site, possibly correlative with the Steptoean positive carbon isotope excursion (SPICE) found worldwide 500– 495 Ma ago. This study aims to elucidate the depositional environment, seal quality, age and provenance of the Eau Claire Formation in central Illinois. The mineralogy of the four depositional facies varies widely throughout the Eau Claire, with a persistently high K-feldspar content. The K-feldspar mode averages 8.7% for the formation and reaches an average of 20.3% in Unit C. Unit A is approximately 30 ft. (9.1 m) thick and exhibits intense bioturbation, ripple beds, and flaser/lenticular bedding, with an average porosity and permeability (n = 20) of 6.7% and 8.6 mD. Unit B is an approximately 40 ft. (12.2 m) thick tight shale sequence, with thin siltstones interbedded throughout. Unit B represents the most desirable seal facies in the formation with an average porosity (n=9) and permeability (n=4) of 5.6% and 2.0x10-5 mD. Unit C is the largest siliciclastic unit in the formation, spanning an average of 95 ft. (29 m) in all three wells at the IBDP. Unit C exhibits the classic tidalite signature of rhythmically interbedded siltstones and shales, with an average porosity and permeability (n = 50) of 9.4% and 0.9 mD. Unit D spans approximately 345 ft. (105.2 m) and begins as a mixed siliciclastic/carbonate environment, slowly becoming a dolomitized carbonate shelf dominated by oolitic packstone and grainstone.","abstract_has_math":false,"creators":["Palkovic, Martin J"],"institution":"University of Illinois at Urbana-Champaign","degree_name":"M.S.","degree_level":"Thesis","degree_discipline":"Geology","degree_department":null,"school":null,"contributors":["Freiburg, Jared T"],"advisors":[],"committee_chairs":[],"committee_members":[],"year":2015,"date_issued":"2015-07-22T22:17:09Z","date_published":"2015-07-22T22:17:09Z","updated_at":"2026-07-22T22:26:11Z","subjects":["Geology","Sedimentology"],"languages":["en"],"rights":["Copyright 2015 Martin Palkovic"],"rights_urls":[],"identifier_entries":[]},"links":{"outbound_url":"http://hdl.handle.net/2142/78424","outbound_label":"Handle","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:contributor","label":"Contributor","values":["Freiburg, Jared T"]},{"key":"dc:creator","label":"Author","values":["Palkovic, Martin J"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date","label":"Dc Date","values":["2015-07-22T22:17:09Z","2015-05","2015-04-20","2015-5"]},{"key":"dc:type","label":"Dc Type","values":["text"]},{"key":"thesis:degree_discipline","label":"Discipline","values":["Geology"]},{"key":"thesis:degree_level","label":"Degree Level","values":["Thesis"]},{"key":"thesis:degree_name","label":"Degree Name","values":["M.S."]},{"key":"thesis:institution_name","label":"Thesis Institution Name","values":["University of Illinois at Urbana-Champaign"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["Geology","Sedimentology"]}]},{"id":"language_rights","label":"Language and Rights","entries":[{"key":"dc:language","label":"Dc Language","values":["en"]},{"key":"dc:rights","label":"Dc Rights","values":["Copyright 2015 Martin Palkovic"]}]},{"id":"identifiers","label":"Identifiers","entries":[{"key":"dc:identifier","label":"Identifier","values":["http://hdl.handle.net/2142/78424"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description","label":"Description","values":["The Cambrian-age Eau Claire Formation serves as the primary seal at the Illinois Basin – Decatur Project (IBDP), a one million tonne carbon capture and storage demonstration project located in Decatur, Illinois. The Eau Claire Formation conformably overlies the Mt. Simon Sandstone, the reservoir for the IBDP. At the IBDP site, analysis of drill core and geophysical logs reveals the Eau Claire consists of two major lithostratigraphic units: a siliciclastic dominant lower unit and a carbonate dominant upper unit. Within the Eau Claire, four major depositional facies exist within a tidally influenced, shallow marine depositional environment. These include (Unit A) intertidal mixed sand/mud flats and tidal channels of the foreshore environment; (Unit B) subtidal deposits of the offshore transition zone; (Unit C) subtidal deposits of the upper shoreface environment; and (Unit D) subtidal mixed carbonate/siliciclastic deposits. An approximately +8‰ δ13C excursion (R2 = 0.97) defines the Eau Claire at the IBDP site, possibly correlative with the Steptoean positive carbon isotope excursion (SPICE) found worldwide 500– 495 Ma ago. This study aims to elucidate the depositional environment, seal quality, age and provenance of the Eau Claire Formation in central Illinois. The mineralogy of the four depositional facies varies widely throughout the Eau Claire, with a persistently high K-feldspar content. The K-feldspar mode averages 8.7% for the formation and reaches an average of 20.3% in Unit C. Unit A is approximately 30 ft. (9.1 m) thick and exhibits intense bioturbation, ripple beds, and flaser/lenticular bedding, with an average porosity and permeability (n = 20) of 6.7% and 8.6 mD. Unit B is an approximately 40 ft. (12.2 m) thick tight shale sequence, with thin siltstones interbedded throughout. Unit B represents the most desirable seal facies in the formation with an average porosity (n=9) and permeability (n=4) of 5.6% and 2.0x10-5 mD. Unit C is the largest siliciclastic unit in the formation, spanning an average of 95 ft. (29 m) in all three wells at the IBDP. Unit C exhibits the classic tidalite signature of rhythmically interbedded siltstones and shales, with an average porosity and permeability (n = 50) of 9.4% and 0.9 mD. Unit D spans approximately 345 ft. (105.2 m) and begins as a mixed siliciclastic/carbonate environment, slowly becoming a dolomitized carbonate shelf dominated by oolitic packstone and grainstone.","Submission original under an indefinite embargo labeled 'Open Access'. The submission was exported from vireo on 2015-07-22 without embargo terms","The student, Martin Palkovic, accepted the attached license on 2015-04-20 at 11:08.","The student, Martin Palkovic, submitted this Thesis for approval on 2015-04-20 at 11:34.","This Thesis was approved for publication on 2015-04-20 at 15:49.","DSpace SAF Submission Ingestion Package generated from Vireo submission #7947 on 2015-07-22 at 10:32:53","Made available in DSpace on 2015-07-22T22:17:09Z (GMT). No. of bitstreams: 2 PALKOVIC-THESIS-2015.pdf: 5216422 bytes, checksum: 553ba6b68782a6750a44f417168d112d (MD5) LICENSE.txt: 4212 bytes, checksum: e03bffffd81be3fd8315bc8d792ea0cc (MD5) Previous issue date: 2015-04-20"]},{"key":"dc:format","label":"Dc Format","values":["application/pdf"]},{"key":"dc:title","label":"Title","values":["Depositional characterization of the Eau Claire Formation at the Illinois Basin - Decatur Project: facies, mineralogy and geochemistry"]}]}],"canonical_facts":{"dc:contributor":["Freiburg, Jared T"],"dc:creator":["Palkovic, Martin J"],"dc:date":["2015-07-22T22:17:09Z","2015-05","2015-04-20","2015-5"],"dc:description":["The Cambrian-age Eau Claire Formation serves as the primary seal at the Illinois Basin – Decatur Project (IBDP), a one million tonne carbon capture and storage demonstration project located in Decatur, Illinois. The Eau Claire Formation conformably overlies the Mt. Simon Sandstone, the reservoir for the IBDP. At the IBDP site, analysis of drill core and geophysical logs reveals the Eau Claire consists of two major lithostratigraphic units: a siliciclastic dominant lower unit and a carbonate dominant upper unit. Within the Eau Claire, four major depositional facies exist within a tidally influenced, shallow marine depositional environment. These include (Unit A) intertidal mixed sand/mud flats and tidal channels of the foreshore environment; (Unit B) subtidal deposits of the offshore transition zone; (Unit C) subtidal deposits of the upper shoreface environment; and (Unit D) subtidal mixed carbonate/siliciclastic deposits. An approximately +8‰ δ13C excursion (R2 = 0.97) defines the Eau Claire at the IBDP site, possibly correlative with the Steptoean positive carbon isotope excursion (SPICE) found worldwide 500– 495 Ma ago. This study aims to elucidate the depositional environment, seal quality, age and provenance of the Eau Claire Formation in central Illinois. The mineralogy of the four depositional facies varies widely throughout the Eau Claire, with a persistently high K-feldspar content. The K-feldspar mode averages 8.7% for the formation and reaches an average of 20.3% in Unit C. Unit A is approximately 30 ft. (9.1 m) thick and exhibits intense bioturbation, ripple beds, and flaser/lenticular bedding, with an average porosity and permeability (n = 20) of 6.7% and 8.6 mD. Unit B is an approximately 40 ft. (12.2 m) thick tight shale sequence, with thin siltstones interbedded throughout. Unit B represents the most desirable seal facies in the formation with an average porosity (n=9) and permeability (n=4) of 5.6% and 2.0x10-5 mD. Unit C is the largest siliciclastic unit in the formation, spanning an average of 95 ft. (29 m) in all three wells at the IBDP. Unit C exhibits the classic tidalite signature of rhythmically interbedded siltstones and shales, with an average porosity and permeability (n = 50) of 9.4% and 0.9 mD. Unit D spans approximately 345 ft. (105.2 m) and begins as a mixed siliciclastic/carbonate environment, slowly becoming a dolomitized carbonate shelf dominated by oolitic packstone and grainstone.","Submission original under an indefinite embargo labeled 'Open Access'. The submission was exported from vireo on 2015-07-22 without embargo terms","The student, Martin Palkovic, accepted the attached license on 2015-04-20 at 11:08.","The student, Martin Palkovic, submitted this Thesis for approval on 2015-04-20 at 11:34.","This Thesis was approved for publication on 2015-04-20 at 15:49.","DSpace SAF Submission Ingestion Package generated from Vireo submission #7947 on 2015-07-22 at 10:32:53","Made available in DSpace on 2015-07-22T22:17:09Z (GMT). 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