{"response":{"docs":[{"system_create_dtsi":"2018-03-26T15:22:54Z","system_modified_dtsi":"2018-03-27T16:05:35Z","has_model_ssim":["Etd"],"id":"bk128998h","accessControl_ssim":["c5681108-e490-439f-a4b9-3eb384985418"],"hasRelatedMediaFragment_ssim":["44558d39p"],"hasRelatedImage_ssim":["44558d39p"],"depositor_ssim":["ucdp@uc.edu"],"depositor_tesim":["ucdp@uc.edu"],"title_tesim":["Origin Of Sedimentary Facies In The Upper San Rafael Group (Middle Jurassic), East Central Utah."],"date_uploaded_dtsi":"2018-03-26T15:22:54Z","date_modified_dtsi":"2018-03-26T15:22:54Z","isPartOf_ssim":["admin_set/default"],"degree_tesim":["Ph.D."],"college_tesim":["Other"],"department_tesim":["Other"],"etd_publisher_tesim":["University of Cincinnati"],"creator_tesim":["Caputo, Mario Vincent."],"publisher_tesim":["University of Cincinnati"],"subject_tesim":["Geology"],"language_tesim":["English"],"description_tesim":["In east-central Utah, tide-, wind-, and wave-currents deposited the Middle Jurassic (Callovian) Curtis and Summerville Formations and the Moab Member of the Entrada Sandstone along the southern and eastern coastal plain of an interior seaway. 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Contemporary crosslaminated and locally crossbedded sublitharenites in the rippled silty facies and the redbed facies were deposited by spring-tide and wind- or storm-enhanced tidal currents in higher intertidal and supratidal zones respectively."],"license_tesim":["http://rightsstatements.org/vocab/InC/1.0/"],"date_created_tesim":["1988"],"thumbnail_path_ss":"/downloads/44558d39p?file=thumbnail","suppressed_bsi":false,"actionable_workflow_roles_ssim":["admin_set/default-default-depositing"],"workflow_state_name_ssim":["deposited"],"member_ids_ssim":["44558d39p"],"file_set_ids_ssim":["44558d39p"],"visibility_ssi":"open","admin_set_tesim":["Default Admin Set"],"sort_title_ssi":"ORIGIN OF SEDIMENTARY FACIES IN THE UPPER SAN RAFAEL GROUP MIDDLE JURASSIC EAST CENTRAL UTAH","human_readable_type_tesim":["Etd"],"read_access_group_ssim":["public"],"edit_access_person_ssim":["ucdp@uc.edu"],"nesting_collection__pathnames_ssim":["bk128998h"],"nesting_collection__deepest_nested_depth_isi":1,"_version_":1697124747306860544,"timestamp":"2021-04-15T16:31:23.244Z","score":0.00049999997},{"system_create_dtsi":"2018-03-26T15:22:39Z","system_modified_dtsi":"2018-03-27T16:05:35Z","has_model_ssim":["Etd"],"id":"2514nk53w","accessControl_ssim":["6d5e3fe3-8e54-4c29-837a-20d9e2b13448"],"hasRelatedMediaFragment_ssim":["d504rk38j"],"hasRelatedImage_ssim":["d504rk38j"],"depositor_ssim":["ucdp@uc.edu"],"depositor_tesim":["ucdp@uc.edu"],"title_tesim":["The Aspen Grove Landslide, Ephraim Canyon, Central Utah."],"date_uploaded_dtsi":"2018-03-26T15:22:39Z","date_modified_dtsi":"2018-03-26T15:22:39Z","isPartOf_ssim":["admin_set/default"],"degree_tesim":["Ph.D."],"college_tesim":["Other"],"department_tesim":["Other"],"etd_publisher_tesim":["University of Cincinnati"],"creator_tesim":["Baum, Rex Lee."],"publisher_tesim":["University of Cincinnati"],"subject_tesim":["Geology"],"language_tesim":["English"],"description_tesim":["The Aspen Grove landslide, central Utah, occurred in older landslide debris. 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Huff."],"college_tesim":["Other"],"department_tesim":["Other"],"etd_publisher_tesim":["University of Cincinnati"],"creator_tesim":["Sutton, Sally Jo."],"publisher_tesim":["University of Cincinnati"],"subject_tesim":["Geology"],"language_tesim":["English"],"description_tesim":["Slaty cleavage exposed in the fine-grained metasediments of western Ocoee Gorge, Tennessee is characterized by zones enriched in cleavage-parrallel white mica (P domains), alternating with zones enriched in quartz and feldspar and in which phyllosilicates are bedding-parallel (Q domains). This domainal fabric appears to develop by growth of new mica from mica components carried in a moving fluid. Solid state recrystallization of clays and mica may also have contributed to the development of the fabric, but little, if any, mechanical rotation or passive concentration of mica grains occurred. Both P domain morphology and mineralogical differences between P and Q domain phyllosilicate populations suggest that nucleation and growth of P domains may involve the expulsion of fluids, during diagenesis and low-grade metamorphism."],"license_tesim":["http://rightsstatements.org/vocab/InC/1.0/"],"date_created_tesim":["1987"],"thumbnail_path_ss":"/downloads/bg257f135?file=thumbnail","suppressed_bsi":false,"actionable_workflow_roles_ssim":["admin_set/default-default-depositing"],"workflow_state_name_ssim":["deposited"],"member_ids_ssim":["bg257f135"],"file_set_ids_ssim":["bg257f135"],"visibility_ssi":"open","admin_set_tesim":["Default Admin Set"],"sort_title_ssi":"DEVELOPMENT OF SLATY CLEAVAGE AT OCOEE GORGE TENNESSEE","human_readable_type_tesim":["Etd"],"read_access_group_ssim":["public"],"edit_access_person_ssim":["ucdp@uc.edu"],"nesting_collection__pathnames_ssim":["47429921g"],"nesting_collection__deepest_nested_depth_isi":1,"_version_":1697108608063373312,"timestamp":"2021-04-15T12:14:51.662Z","score":0.00049999997},{"system_create_dtsi":"2018-03-26T15:22:09Z","system_modified_dtsi":"2018-03-27T16:05:34Z","has_model_ssim":["Etd"],"id":"bk1289977","accessControl_ssim":["ddb212e2-0009-4be9-8fe9-9dc5a2a9ef1c"],"hasRelatedMediaFragment_ssim":["gt54kn109"],"hasRelatedImage_ssim":["gt54kn109"],"depositor_ssim":["ucdp@uc.edu"],"depositor_tesim":["ucdp@uc.edu"],"title_tesim":["Anchoring Of Thin Colluvium On Hillslopes In Cincinnati By Roots Of Sugar Maple And White Ash."],"date_uploaded_dtsi":"2018-03-26T15:22:09Z","date_modified_dtsi":"2018-03-26T15:22:09Z","isPartOf_ssim":["admin_set/default"],"degree_tesim":["Ph.D."],"college_tesim":["Other"],"department_tesim":["Other"],"etd_publisher_tesim":["University of Cincinnati"],"creator_tesim":["Riestenberg, Mary Margaret."],"publisher_tesim":["University of Cincinnati"],"subject_tesim":["Geology","Agriculture, Forestry and Wildlife","Biology, General"],"language_tesim":["English"],"description_tesim":["Roots of white ash have a better configuration than roots of sugar maple for anchoring shallow colluvium against landsliding on hillslopes along the Ohio River and its tributaries in southwestern Ohio. 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Sugar maple is the most common species on the landslides; its roots do not penetrate the soil as deeply as the roots of the white ash."],"license_tesim":["http://rightsstatements.org/vocab/InC/1.0/"],"date_created_tesim":["1987"],"thumbnail_path_ss":"/downloads/gt54kn109?file=thumbnail","suppressed_bsi":false,"actionable_workflow_roles_ssim":["admin_set/default-default-depositing"],"workflow_state_name_ssim":["deposited"],"member_ids_ssim":["gt54kn109"],"file_set_ids_ssim":["gt54kn109"],"visibility_ssi":"open","admin_set_tesim":["Default Admin Set"],"sort_title_ssi":"ANCHORING OF THIN COLLUVIUM ON HILLSLOPES IN CINCINNATI BY ROOTS OF SUGAR MAPLE AND WHITE ASH","human_readable_type_tesim":["Etd"],"read_access_group_ssim":["public"],"edit_access_person_ssim":["ucdp@uc.edu"],"nesting_collection__pathnames_ssim":["bk1289977"],"nesting_collection__deepest_nested_depth_isi":1,"_version_":1697074116578770944,"timestamp":"2021-04-15T03:06:38.019Z","score":0.00049999997},{"system_create_dtsi":"2018-03-26T15:21:55Z","system_modified_dtsi":"2018-03-27T16:05:34Z","has_model_ssim":["Etd"],"id":"cf95jb48w","accessControl_ssim":["da3aef9f-d3de-41e4-b777-e202e24e9277"],"hasRelatedMediaFragment_ssim":["xk81jk46z"],"hasRelatedImage_ssim":["xk81jk46z"],"depositor_ssim":["ucdp@uc.edu"],"depositor_tesim":["ucdp@uc.edu"],"title_tesim":["Paleocene Benthic Foraminiferal Biostratigraphy, Paleoecology, And Paleoceanography Of The Eastern Gulf Coastal Plain."],"date_uploaded_dtsi":"2018-03-26T15:21:56Z","date_modified_dtsi":"2018-03-26T15:21:56Z","isPartOf_ssim":["admin_set/default"],"degree_tesim":["Ph.D."],"college_tesim":["Other"],"department_tesim":["Other"],"etd_publisher_tesim":["University of Cincinnati"],"creator_tesim":["Fluegeman, Richard Herbert."],"publisher_tesim":["University of Cincinnati"],"subject_tesim":["Paleontology","Geology","Paleoecology"],"language_tesim":["English"],"description_tesim":["A stratigraphic and paleontological analysis of 303 samples of Paleocene sediments of the eastern Gulf Coastal Plain of Mississippi, Alabama, and Georgia provided the basis for a geochronologic, quantitative paleoecologic, and paleoceanographic model."],"license_tesim":["http://rightsstatements.org/vocab/InC/1.0/"],"date_created_tesim":["1987"],"thumbnail_path_ss":"/downloads/xk81jk46z?file=thumbnail","suppressed_bsi":false,"actionable_workflow_roles_ssim":["admin_set/default-default-depositing"],"workflow_state_name_ssim":["deposited"],"member_ids_ssim":["xk81jk46z"],"file_set_ids_ssim":["xk81jk46z"],"visibility_ssi":"open","admin_set_tesim":["Default Admin Set"],"sort_title_ssi":"PALEOCENE BENTHIC FORAMINIFERAL BIOSTRATIGRAPHY PALEOECOLOGY AND PALEOCEANOGRAPHY OF THE EASTERN GULF COASTAL PLAIN","human_readable_type_tesim":["Etd"],"read_access_group_ssim":["public"],"edit_access_person_ssim":["ucdp@uc.edu"],"nesting_collection__pathnames_ssim":["cf95jb48w"],"nesting_collection__deepest_nested_depth_isi":1,"_version_":1697124908253839360,"timestamp":"2021-04-15T16:33:56.735Z","score":0.00049999997},{"system_create_dtsi":"2018-03-26T15:21:41Z","system_modified_dtsi":"2018-03-27T16:05:33Z","has_model_ssim":["Etd"],"id":"xs55mc11m","accessControl_ssim":["cd1749a8-1db9-4e05-b555-11260d6eeb4d"],"hasRelatedMediaFragment_ssim":["k0698754k"],"hasRelatedImage_ssim":["k0698754k"],"depositor_ssim":["ucdp@uc.edu"],"depositor_tesim":["ucdp@uc.edu"],"title_tesim":["Stratigraphy, Depositional Environment, And Reservoir Analysis Of The Itarare Group (Permo Carboniferous), Parana Basin   Brazil."],"date_uploaded_dtsi":"2018-03-26T15:21:41Z","date_modified_dtsi":"2018-03-26T15:21:41Z","isPartOf_ssim":["admin_set/default"],"degree_tesim":["Ph.D."],"college_tesim":["Other"],"department_tesim":["Other"],"etd_publisher_tesim":["University of Cincinnati"],"creator_tesim":["Franca, Almerio Barros."],"publisher_tesim":["University of Cincinnati"],"subject_tesim":["Geology"],"language_tesim":["English"],"description_tesim":["The present work is a stratigraphic, reservoir, and environmental analysis of the Itarare Group (Permo-Carboniferous) using the well data of the Parana Basin which covers about 1,000,000 Km$\\sp{2}$ in Brazil alone. More than three thousand kilometers of cross sections were analysed, over 100 wells were studied, nearly 400 meters of cores were described, and 95 thin sections were analysed."],"license_tesim":["http://rightsstatements.org/vocab/InC/1.0/"],"date_created_tesim":["1987"],"thumbnail_path_ss":"/downloads/k0698754k?file=thumbnail","suppressed_bsi":false,"actionable_workflow_roles_ssim":["admin_set/default-default-depositing"],"workflow_state_name_ssim":["deposited"],"member_ids_ssim":["k0698754k"],"file_set_ids_ssim":["k0698754k"],"visibility_ssi":"open","admin_set_tesim":["Default Admin Set"],"sort_title_ssi":"STRATIGRAPHY DEPOSITIONAL ENVIRONMENT AND RESERVOIR ANALYSIS OF THE ITARARE GROUP PERMO CARBONIFEROUS PARANA BASIN BRAZIL","human_readable_type_tesim":["Etd"],"read_access_group_ssim":["public"],"edit_access_person_ssim":["ucdp@uc.edu"],"nesting_collection__pathnames_ssim":["xs55mc11m"],"nesting_collection__deepest_nested_depth_isi":1,"_version_":1697075986304073728,"timestamp":"2021-04-15T03:36:21.128Z","score":0.00049999997},{"system_create_dtsi":"2018-03-26T15:21:25Z","system_modified_dtsi":"2018-03-27T16:05:33Z","has_model_ssim":["Etd"],"id":"9593tv18r","accessControl_ssim":["f2d7b47a-d4c8-4ffd-b5ea-da165af06aec"],"hasRelatedMediaFragment_ssim":["5712m6567"],"hasRelatedImage_ssim":["5712m6567"],"depositor_ssim":["ucdp@uc.edu"],"depositor_tesim":["ucdp@uc.edu"],"title_tesim":["Geochemistry And Mineralogy Of The Molango Manganese Orebody, Hidalgo State, Mexico."],"date_uploaded_dtsi":"2018-03-26T15:21:26Z","date_modified_dtsi":"2018-03-26T15:21:26Z","isPartOf_ssim":["admin_set/default"],"degree_tesim":["Ph.D."],"college_tesim":["Other"],"department_tesim":["Other"],"etd_publisher_tesim":["University of Cincinnati"],"creator_tesim":["Okita, Patrick Masao."],"publisher_tesim":["University of Cincinnati"],"subject_tesim":["Geology"],"language_tesim":["English"],"description_tesim":["\"The Molango manganese deposit is the only known large Mn deposit in North America. Mineralization involves Mn-carbonate exclusively in a finely laminated bed about 10 meters thick with a strike length $\u003e$50 kilometers. The ore bed is the basal unit of the Chipoco facies (Taman Fm., Kimmeridgian) and underlain by laminated black shales of the Santiago formation (Oxfordian).\""],"license_tesim":["http://rightsstatements.org/vocab/InC/1.0/"],"date_created_tesim":["1987"],"thumbnail_path_ss":"/downloads/5712m6567?file=thumbnail","suppressed_bsi":false,"actionable_workflow_roles_ssim":["admin_set/default-default-depositing"],"workflow_state_name_ssim":["deposited"],"member_ids_ssim":["5712m6567"],"file_set_ids_ssim":["5712m6567"],"visibility_ssi":"open","admin_set_tesim":["Default Admin Set"],"sort_title_ssi":"GEOCHEMISTRY AND MINERALOGY OF THE MOLANGO MANGANESE OREBODY HIDALGO STATE MEXICO","human_readable_type_tesim":["Etd"],"read_access_group_ssim":["public"],"edit_access_person_ssim":["ucdp@uc.edu"],"nesting_collection__pathnames_ssim":["9593tv18r"],"nesting_collection__deepest_nested_depth_isi":1,"_version_":1697103980829605888,"timestamp":"2021-04-15T11:01:18.788Z","score":0.00049999997},{"system_create_dtsi":"2018-03-26T15:21:11Z","system_modified_dtsi":"2018-03-27T16:05:32Z","has_model_ssim":["Etd"],"id":"gq67jr21k","accessControl_ssim":["d365eaae-4535-4364-833f-84ec42a669b7"],"hasRelatedMediaFragment_ssim":["zk51vg82g"],"hasRelatedImage_ssim":["zk51vg82g"],"depositor_ssim":["ucdp@uc.edu"],"depositor_tesim":["ucdp@uc.edu"],"title_tesim":["On Forms Of Folds (Asymmetry)."],"date_uploaded_dtsi":"2018-03-26T15:21:12Z","date_modified_dtsi":"2018-03-26T15:21:12Z","isPartOf_ssim":["admin_set/default"],"degree_tesim":["Ph.D."],"college_tesim":["Other"],"department_tesim":["Other"],"etd_publisher_tesim":["University of Cincinnati"],"creator_tesim":["Pfaff, Virginia J."],"publisher_tesim":["University of Cincinnati"],"subject_tesim":["Geology"],"language_tesim":["English"],"description_tesim":["A 3rd order theory of folding of viscous multilayers indicates that forms of folds are controlled by the behavior of layer contacts or interbeds, the relative stiffnesses of the multilayer and confining media, and the scale of the folding. A 2nd order analysis shows that asymmetry of folds is determined largely by the behavior of layer contacts and the sense of layer-parallel shear during folding."],"license_tesim":["http://rightsstatements.org/vocab/InC/1.0/"],"date_created_tesim":["1986"],"thumbnail_path_ss":"/downloads/zk51vg82g?file=thumbnail","suppressed_bsi":false,"actionable_workflow_roles_ssim":["admin_set/default-default-depositing"],"workflow_state_name_ssim":["deposited"],"member_ids_ssim":["zk51vg82g"],"file_set_ids_ssim":["zk51vg82g"],"visibility_ssi":"open","admin_set_tesim":["Default Admin Set"],"sort_title_ssi":"ON FORMS OF FOLDS ASYMMETRY","human_readable_type_tesim":["Etd"],"read_access_group_ssim":["public"],"edit_access_person_ssim":["ucdp@uc.edu"],"nesting_collection__pathnames_ssim":["gq67jr21k"],"nesting_collection__deepest_nested_depth_isi":1,"_version_":1697083142992560128,"timestamp":"2021-04-15T05:30:06.278Z","score":0.00049999997},{"system_create_dtsi":"2018-03-26T15:20:57Z","system_modified_dtsi":"2018-03-27T16:05:31Z","has_model_ssim":["Etd"],"id":"sq87bt68c","accessControl_ssim":["57e265c7-6302-4667-9f31-921c6de22f18"],"hasRelatedMediaFragment_ssim":["dz010q102"],"hasRelatedImage_ssim":["dz010q102"],"depositor_ssim":["ucdp@uc.edu"],"depositor_tesim":["ucdp@uc.edu"],"title_tesim":["Analysis Of Bed Duplication Folding (Tennessee, West Virginia)."],"date_uploaded_dtsi":"2018-03-26T15:20:58Z","date_modified_dtsi":"2018-03-26T15:20:58Z","isPartOf_ssim":["admin_set/default"],"degree_tesim":["Ph.D."],"college_tesim":["Other"],"department_tesim":["Other"],"etd_publisher_tesim":["University of Cincinnati"],"creator_tesim":["Berger, Philip S."],"publisher_tesim":["University of Cincinnati"],"subject_tesim":["Geology"],"language_tesim":["English"],"description_tesim":["I solve boundary-value problems for an idealized thrust block moving over a detachment surface and ramp, and produce theoretical bed-duplication folds in the thrust block that closely resemble the Powell Valley anticline in the southern Appalachian Mountains. The anticline is narrow and rounded if the translation is small, and broad and flat-topped if the translation is large. The limbs of the anticline are symmetric if drag is zero. Drag along the ramp part of the detachment surface can explain the asymmetry of dips of the two limbs of the Powell Valley anticline, particularly if drag between relatively competent rocks in opposition at the ramp causes an initial anticline to form as the thrust block begins to move, and then drag reduces markedly as relatively soft shales at the base of the block were thrust over competent rocks in the ramp."],"license_tesim":["http://rightsstatements.org/vocab/InC/1.0/"],"date_created_tesim":["1986"],"thumbnail_path_ss":"/downloads/dz010q102?file=thumbnail","suppressed_bsi":false,"actionable_workflow_roles_ssim":["admin_set/default-default-depositing"],"workflow_state_name_ssim":["deposited"],"member_ids_ssim":["dz010q102"],"file_set_ids_ssim":["dz010q102"],"visibility_ssi":"open","admin_set_tesim":["Default Admin Set"],"sort_title_ssi":"ANALYSIS OF BED DUPLICATION FOLDING TENNESSEE WEST VIRGINIA","human_readable_type_tesim":["Etd"],"read_access_group_ssim":["public"],"edit_access_person_ssim":["ucdp@uc.edu"],"nesting_collection__pathnames_ssim":["sq87bt68c"],"nesting_collection__deepest_nested_depth_isi":1,"_version_":1697100435747241984,"timestamp":"2021-04-15T10:04:57.934Z","score":0.00049999997},{"system_create_dtsi":"2018-03-26T15:20:43Z","system_modified_dtsi":"2018-03-27T16:05:30Z","has_model_ssim":["Etd"],"id":"3484zg951","accessControl_ssim":["4050747b-fb90-4936-817f-90890c46cdac"],"hasRelatedMediaFragment_ssim":["bz60cw27k"],"hasRelatedImage_ssim":["bz60cw27k"],"depositor_ssim":["ucdp@uc.edu"],"depositor_tesim":["ucdp@uc.edu"],"title_tesim":["Middle And Upper Ordovician Monoplacophora And Bellerophontacean Gastropoda Of The Cincinnati Arch Region."],"date_uploaded_dtsi":"2018-03-26T15:20:43Z","date_modified_dtsi":"2018-03-26T15:20:43Z","isPartOf_ssim":["admin_set/default"],"degree_tesim":["Ph.D."],"college_tesim":["Other"],"department_tesim":["Other"],"etd_publisher_tesim":["University of Cincinnati"],"creator_tesim":["Wahlman, Gregory Paul."],"publisher_tesim":["University of Cincinnati"],"subject_tesim":["Paleontology"],"language_tesim":["English"],"description_tesim":["The taxonomy, phylogeny, biostratigraphy, functional morphology, and paleoecology of Middle and Upper Ordovician (Blackriveran-Richmondian) Monoplacophora and bellerophontacean Gastropoda of the Cincinnati Arch region are discussed. Six genera and 29 species of monoplacophorans, and 13 genera and 56 species of bellerophontaceans are evaluated. 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