{"response":{"docs":[{"system_create_dtsi":"2018-03-26T15:26:56Z","system_modified_dtsi":"2018-03-27T16:05:43Z","has_model_ssim":["Etd"],"id":"zc77sq12h","accessControl_ssim":["573e1ca8-0660-4718-a6e4-e8d9027494a6"],"hasRelatedMediaFragment_ssim":["m326m179b"],"hasRelatedImage_ssim":["m326m179b"],"depositor_ssim":["ucdp@uc.edu"],"depositor_tesim":["ucdp@uc.edu"],"title_tesim":["The Cretaceous In The Caborca Santa Ana Region, Northern Sonora, Mexico."],"date_uploaded_dtsi":"2018-03-26T15:26:56Z","date_modified_dtsi":"2018-03-26T15:26:56Z","isPartOf_ssim":["admin_set/default"],"degree_tesim":["Ph.D."],"advisor_tesim":["Chair: Kees A. 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This study also finds that the Proterozoic-Paleozoic formations in northwest Sonora (Caborca terrane) were not part of the Cretaceous landscape, thus raising doubts about the existence of the Mojave-Sonora megashear."],"license_tesim":["http://rightsstatements.org/vocab/InC/1.0/"],"date_created_tesim":["1993"],"thumbnail_path_ss":"/downloads/m326m179b?file=thumbnail","suppressed_bsi":false,"actionable_workflow_roles_ssim":["admin_set/default-default-depositing"],"workflow_state_name_ssim":["deposited"],"member_ids_ssim":["m326m179b"],"file_set_ids_ssim":["m326m179b"],"visibility_ssi":"open","admin_set_tesim":["Default Admin Set"],"sort_title_ssi":"CRETACEOUS IN THE CABORCA SANTA ANA REGION NORTHERN SONORA MEXICO","human_readable_type_tesim":["Etd"],"read_access_group_ssim":["public"],"edit_access_person_ssim":["ucdp@uc.edu"],"nesting_collection__pathnames_ssim":["zc77sq12h"],"nesting_collection__deepest_nested_depth_isi":1,"_version_":1697117918417911808,"timestamp":"2021-04-15T14:42:50.708Z","score":0.00049999997},{"system_create_dtsi":"2018-03-26T15:26:44Z","system_modified_dtsi":"2018-03-27T16:05:43Z","has_model_ssim":["Etd"],"id":"76537140z","accessControl_ssim":["1b79860e-11bf-41e0-810f-1d35b66eec3e"],"hasRelatedMediaFragment_ssim":["q237hr963"],"hasRelatedImage_ssim":["q237hr963"],"depositor_ssim":["ucdp@uc.edu"],"depositor_tesim":["ucdp@uc.edu"],"title_tesim":["Burial Depth And Lithofacies Control Of Stylolite Development In The Mississippian Salem Limestone, Illinois Basin."],"date_uploaded_dtsi":"2018-03-26T15:26:44Z","date_modified_dtsi":"2018-03-26T15:26:44Z","isPartOf_ssim":["admin_set/default"],"degree_tesim":["Ph.D."],"advisor_tesim":["Chair: Wayne A. 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Many stylolites grade laterally into organic-rich layers, or hummocky seams. Thicknesses of stylolite caps and hummocky seams are approximately equal in the same host rock, but hummocky seams tend to be more laterally continuous. Stylolite density in packstone increases with burial depth, whereas hummocky seam density decreases. Hummocky seam thickness does not change with depth. Stylolite column height in grainstone, which is sparse in hummocky seams, increases with depth, whereas stylolite density does not increase. This list of observations supports the hypothesis that stylolites develop along pre-existing, organic-rich layers, or hummocky seams, rather than nucleating in pure host rock and creating organic-rich seams as accumulations of insoluble residue. 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Pryor."],"college_tesim":["Other"],"department_tesim":["Other"],"etd_publisher_tesim":["University of Cincinnati"],"creator_tesim":["Norrish, Winston Alfred."],"publisher_tesim":["University of Cincinnati"],"subject_tesim":["Geology"],"language_tesim":["English"],"description_tesim":["The Brassfield Formation is a very thin, highly condensed carbonate unit that encompasses most of the Llandovery (8.5 MMYR) and covers much of the eastern midcontinent. Fifty-six Brassfield outcrops exposed around the flanks of the Cincinnati arch comprise three members, four facies tracts, and seven lithofacies. 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