{"response":{"docs":[{"system_create_dtsi":"2018-03-26T15:26:05Z","system_modified_dtsi":"2018-03-27T16:05:41Z","has_model_ssim":["Etd"],"id":"n583xv070","accessControl_ssim":["fd436d6d-4810-4cc5-9f9b-57cecbe8a52c"],"hasRelatedMediaFragment_ssim":["9z902z875"],"hasRelatedImage_ssim":["9z902z875"],"depositor_ssim":["ucdp@uc.edu"],"depositor_tesim":["ucdp@uc.edu"],"title_tesim":["Quaternary Stratigraphy Near Cincinnati, Ohio, And Its Significance For Paleoclimate Reconstruction."],"date_uploaded_dtsi":"2018-03-26T15:26:05Z","date_modified_dtsi":"2018-03-26T15:26:05Z","isPartOf_ssim":["admin_set/default"],"degree_tesim":["Ph.D."],"advisor_tesim":["Chair: Thomas Lowell."],"college_tesim":["Other"],"department_tesim":["Other"],"etd_publisher_tesim":["University of Cincinnati"],"creator_tesim":["Savage, Kevin Michael."],"publisher_tesim":["University of Cincinnati"],"subject_tesim":["Geology","Paleoecology"],"language_tesim":["English"],"description_tesim":["Rare occurences of coeval late Wisconsin glacigenic diamictons and ice-proximal sediments with a diverse faunal assemblage provided an opportunity to test the viability of the glacigenic sediments as proxy paleoclimate indicators."],"license_tesim":["http://rightsstatements.org/vocab/InC/1.0/"],"date_created_tesim":["1992"],"thumbnail_path_ss":"/downloads/9z902z875?file=thumbnail","suppressed_bsi":false,"actionable_workflow_roles_ssim":["admin_set/default-default-depositing"],"workflow_state_name_ssim":["deposited"],"member_ids_ssim":["9z902z875"],"file_set_ids_ssim":["9z902z875"],"visibility_ssi":"open","admin_set_tesim":["Default Admin Set"],"sort_title_ssi":"QUATERNARY STRATIGRAPHY NEAR CINCINNATI OHIO AND ITS SIGNIFICANCE FOR PALEOCLIMATE RECONSTRUCTION","human_readable_type_tesim":["Etd"],"read_access_group_ssim":["public"],"edit_access_person_ssim":["ucdp@uc.edu"],"nesting_collection__pathnames_ssim":["n583xv070"],"nesting_collection__deepest_nested_depth_isi":1,"_version_":1697082428263235584,"timestamp":"2021-04-15T05:18:44.659Z","score":0.00049999997},{"system_create_dtsi":"2018-03-26T15:25:50Z","system_modified_dtsi":"2018-03-27T16:05:41Z","has_model_ssim":["Etd"],"id":"w37636789","accessControl_ssim":["85c6280b-8836-4ac6-afe3-a8b732810528"],"hasRelatedMediaFragment_ssim":["n870zq887"],"hasRelatedImage_ssim":["n870zq887"],"depositor_ssim":["ucdp@uc.edu"],"depositor_tesim":["ucdp@uc.edu"],"title_tesim":["Evolution Of The Witwatersrand Basin: Evidence From The Quartzites."],"date_uploaded_dtsi":"2018-03-26T15:25:50Z","date_modified_dtsi":"2018-03-26T15:25:50Z","isPartOf_ssim":["admin_set/default"],"degree_tesim":["Ph.D."],"advisor_tesim":["Chair: J. Barry Maynard."],"college_tesim":["Other"],"department_tesim":["Other"],"etd_publisher_tesim":["University of Cincinnati"],"creator_tesim":["Ritger, Scott D."],"publisher_tesim":["University of Cincinnati"],"subject_tesim":["Geochemistry","Geology"],"language_tesim":["English"],"description_tesim":["In this dissertation I present a tectonic, geochemical, and thermal history for the Witwatersrand basin, located on the Archean Kaapvaal craton, South Africa. The foreland basin tectonic setting of the Central Rand Group controls both the chemical and the thermal evolution of the basin, and unifies the basin evolution model presented here."],"license_tesim":["http://rightsstatements.org/vocab/InC/1.0/"],"date_created_tesim":["1991"],"thumbnail_path_ss":"/downloads/n870zq887?file=thumbnail","suppressed_bsi":false,"actionable_workflow_roles_ssim":["admin_set/default-default-depositing"],"workflow_state_name_ssim":["deposited"],"member_ids_ssim":["n870zq887"],"file_set_ids_ssim":["n870zq887"],"visibility_ssi":"open","admin_set_tesim":["Default Admin Set"],"sort_title_ssi":"EVOLUTION OF THE WITWATERSRAND BASIN EVIDENCE FROM THE QUARTZITES","human_readable_type_tesim":["Etd"],"read_access_group_ssim":["public"],"edit_access_person_ssim":["ucdp@uc.edu"],"nesting_collection__pathnames_ssim":["w37636789"],"nesting_collection__deepest_nested_depth_isi":1,"_version_":1697081824512049152,"timestamp":"2021-04-15T05:09:08.877Z","score":0.00049999997},{"system_create_dtsi":"2018-03-26T15:25:34Z","system_modified_dtsi":"2018-03-27T16:05:41Z","has_model_ssim":["Etd"],"id":"1g05fb64j","accessControl_ssim":["ce644ae5-2791-443e-aa72-8a2dfb5da41f"],"hasRelatedMediaFragment_ssim":["4j03cz67q"],"hasRelatedImage_ssim":["4j03cz67q"],"depositor_ssim":["ucdp@uc.edu"],"depositor_tesim":["ucdp@uc.edu"],"title_tesim":["Geochemical Characterization Of Black Shale Types In The Midcontinent Pennsylvanian."],"date_uploaded_dtsi":"2018-03-26T15:25:34Z","date_modified_dtsi":"2018-03-26T15:25:34Z","isPartOf_ssim":["admin_set/default"],"degree_tesim":["Ph.D."],"advisor_tesim":["Adviser: J. Barry Maynard."],"college_tesim":["Other"],"department_tesim":["Other"],"etd_publisher_tesim":["University of Cincinnati"],"creator_tesim":["Schultz, Richard Brian."],"publisher_tesim":["University of Cincinnati"],"subject_tesim":["Geochemistry","Geology"],"language_tesim":["English"],"description_tesim":["Various geochemical parameters including type and abundance of organic matter (TOC), sulfide-sulfur quantities, fluctuations in bottom-water anoxicity (DOP), metal content differences, and sulfur isotope variations have been assessed in order to characterize Midcontinent Pennsylvanian black shales. Based on these geochemical parameters, the deposits can be grouped into three types: Mecca-type, Heebner-type, and Shanghai-type."],"license_tesim":["http://rightsstatements.org/vocab/InC/1.0/"],"date_created_tesim":["1991"],"thumbnail_path_ss":"/downloads/4j03cz67q?file=thumbnail","suppressed_bsi":false,"actionable_workflow_roles_ssim":["admin_set/default-default-depositing"],"workflow_state_name_ssim":["deposited"],"member_ids_ssim":["4j03cz67q"],"file_set_ids_ssim":["4j03cz67q"],"visibility_ssi":"open","admin_set_tesim":["Default Admin Set"],"sort_title_ssi":"GEOCHEMICAL CHARACTERIZATION OF BLACK SHALE TYPES IN THE MIDCONTINENT PENNSYLVANIAN","human_readable_type_tesim":["Etd"],"read_access_group_ssim":["public"],"edit_access_person_ssim":["ucdp@uc.edu"],"nesting_collection__pathnames_ssim":["1g05fb64j"],"nesting_collection__deepest_nested_depth_isi":1,"_version_":1697093283158687744,"timestamp":"2021-04-15T08:11:16.694Z","score":0.00049999997},{"system_create_dtsi":"2018-03-26T15:25:21Z","system_modified_dtsi":"2018-03-27T16:05:40Z","has_model_ssim":["Etd"],"id":"cj82k743r","accessControl_ssim":["aef74859-acc1-41c5-9264-bd6a6081f83f"],"hasRelatedMediaFragment_ssim":["cr56n1010"],"hasRelatedImage_ssim":["cr56n1010"],"depositor_ssim":["ucdp@uc.edu"],"depositor_tesim":["ucdp@uc.edu"],"title_tesim":["The Lower Silurian Brassfield Formation: A Condensed Sequence Of Punctuated Deposition?"],"date_uploaded_dtsi":"2018-03-26T15:25:21Z","date_modified_dtsi":"2018-03-26T15:25:21Z","isPartOf_ssim":["admin_set/default"],"degree_tesim":["Ph.D."],"advisor_tesim":["Adviser: Wayne A. 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. The three types of condensation recognized in the Brassfield (dynamic bypass, punctuated deposition, and sediment starvation) are related to sea level fluctuations, manifested as a hierarchy of sequence orders, that ultimately controlled the spatial and temporal distribution of facies."],"license_tesim":["http://rightsstatements.org/vocab/InC/1.0/"],"date_created_tesim":["1991"],"thumbnail_path_ss":"/downloads/cr56n1010?file=thumbnail","suppressed_bsi":false,"actionable_workflow_roles_ssim":["admin_set/default-default-depositing"],"workflow_state_name_ssim":["deposited"],"member_ids_ssim":["cr56n1010"],"file_set_ids_ssim":["cr56n1010"],"visibility_ssi":"open","admin_set_tesim":["Default Admin Set"],"sort_title_ssi":"LOWER SILURIAN BRASSFIELD FORMATION A CONDENSED SEQUENCE OF PUNCTUATED DEPOSITION","human_readable_type_tesim":["Etd"],"read_access_group_ssim":["public"],"edit_access_person_ssim":["ucdp@uc.edu"],"nesting_collection__pathnames_ssim":["cj82k743r"],"nesting_collection__deepest_nested_depth_isi":1,"_version_":1697097955846127616,"timestamp":"2021-04-15T09:25:32.916Z","score":0.00049999997},{"system_create_dtsi":"2018-03-26T15:25:08Z","system_modified_dtsi":"2018-03-27T16:05:40Z","has_model_ssim":["Etd"],"id":"tt44pm93m","accessControl_ssim":["cfb46d08-843a-4b83-b2bf-a1ce919167e7"],"hasRelatedMediaFragment_ssim":["f4752g76q"],"hasRelatedImage_ssim":["f4752g76q"],"depositor_ssim":["ucdp@uc.edu"],"depositor_tesim":["ucdp@uc.edu"],"title_tesim":["The Hydraulic Fracturing Of Soil."],"date_uploaded_dtsi":"2018-03-26T15:25:08Z","date_modified_dtsi":"2018-03-26T15:25:08Z","isPartOf_ssim":["admin_set/default"],"degree_tesim":["Ph.D."],"advisor_tesim":["Chair: Arvid M. Johnson."],"college_tesim":["Other"],"department_tesim":["Other"],"etd_publisher_tesim":["University of Cincinnati"],"creator_tesim":["Murdoch, Lawrence Corlies, Iii."],"publisher_tesim":["University of Cincinnati"],"subject_tesim":["Engineering, Civil","Geology","Geotechnology"],"language_tesim":["English"],"description_tesim":["Little is known about the hydraulic fracturing of soil, although the technique holds potential for several environmental engineering applications. The dissertation research consists of laboratory experiments, where hydraulic fractures were created by injecting dyed glycerin into colluvium contained in a triaxial pressure cell, and a field test, where hydraulic fractures were created by injecting guar gum gel at shallow depths in glacial drift. The laboratory tests showed that hydraulic fractures are readily created in clayey-silt colluvium. Furthermore, hydraulic fractures created in soil with positive pore pressure were filled with two fluids: one injected to create the fracture, and pore fluid that infiltrates into the fracture tip. The length of the infiltrated tip increases with increasing fracture length."],"license_tesim":["http://rightsstatements.org/vocab/InC/1.0/"],"date_created_tesim":["1991"],"thumbnail_path_ss":"/downloads/f4752g76q?file=thumbnail","suppressed_bsi":false,"actionable_workflow_roles_ssim":["admin_set/default-default-depositing"],"workflow_state_name_ssim":["deposited"],"member_ids_ssim":["f4752g76q"],"file_set_ids_ssim":["f4752g76q"],"visibility_ssi":"open","admin_set_tesim":["Default Admin Set"],"sort_title_ssi":"HYDRAULIC FRACTURING OF SOIL","human_readable_type_tesim":["Etd"],"read_access_group_ssim":["public"],"edit_access_person_ssim":["ucdp@uc.edu"],"nesting_collection__pathnames_ssim":["tt44pm93m"],"nesting_collection__deepest_nested_depth_isi":1,"_version_":1697112980937768960,"timestamp":"2021-04-15T13:24:21.960Z","score":0.00049999997},{"system_create_dtsi":"2018-03-26T15:24:53Z","system_modified_dtsi":"2018-03-27T16:05:39Z","has_model_ssim":["Etd"],"id":"th83kz37g","accessControl_ssim":["26afe70d-1bf8-428b-bd1b-bd7a192e6ae6"],"hasRelatedMediaFragment_ssim":["hh63sv958"],"hasRelatedImage_ssim":["hh63sv958"],"depositor_ssim":["ucdp@uc.edu"],"depositor_tesim":["ucdp@uc.edu"],"title_tesim":["Skeletal Growth And Chemistry Of The Sea Urchin Strongylocentrotus (Echinodermata:Echinoidea)."],"date_uploaded_dtsi":"2018-03-26T15:24:53Z","date_modified_dtsi":"2018-03-26T15:24:53Z","isPartOf_ssim":["admin_set/default"],"degree_tesim":["Ph.D."],"college_tesim":["Other"],"department_tesim":["Other"],"etd_publisher_tesim":["University of Cincinnati"],"creator_tesim":["Scancar, Sonja Marguerite."],"publisher_tesim":["University of Cincinnati"],"subject_tesim":["Paleontology","Paleozoology","Biology, Zoology"],"language_tesim":["English"],"description_tesim":["Investigation of the coronal plates of the regular echinoid Strongy-locentrotus (Echinodermata: Echinoidea) shows that skeletal growth and chemistry may be interrelated."],"license_tesim":["http://rightsstatements.org/vocab/InC/1.0/"],"date_created_tesim":["1990"],"thumbnail_path_ss":"/downloads/hh63sv958?file=thumbnail","suppressed_bsi":false,"actionable_workflow_roles_ssim":["admin_set/default-default-depositing"],"workflow_state_name_ssim":["deposited"],"member_ids_ssim":["hh63sv958"],"file_set_ids_ssim":["hh63sv958"],"visibility_ssi":"open","admin_set_tesim":["Default Admin Set"],"sort_title_ssi":"SKELETAL GROWTH AND CHEMISTRY OF THE SEA URCHIN STRONGYLOCENTROTUS ECHINODERMATAECHINOIDEA","human_readable_type_tesim":["Etd"],"read_access_group_ssim":["public"],"edit_access_person_ssim":["ucdp@uc.edu"],"nesting_collection__pathnames_ssim":["th83kz37g"],"nesting_collection__deepest_nested_depth_isi":1,"_version_":1697100944937844736,"timestamp":"2021-04-15T10:13:03.536Z","score":0.00049999997},{"system_create_dtsi":"2018-03-26T15:24:41Z","system_modified_dtsi":"2018-03-27T16:05:39Z","has_model_ssim":["Etd"],"id":"m039k492n","accessControl_ssim":["dbe2db2a-f490-4f32-aead-ce8352e7e5b0"],"hasRelatedMediaFragment_ssim":["cj82k742g"],"hasRelatedImage_ssim":["cj82k742g"],"depositor_ssim":["ucdp@uc.edu"],"depositor_tesim":["ucdp@uc.edu"],"title_tesim":["An Integrated Study Of Echinoid Taphonomy: Predictions For The Fossil Record Of Four Echinoid Families."],"date_uploaded_dtsi":"2018-03-26T15:24:42Z","date_modified_dtsi":"2018-03-26T15:24:42Z","isPartOf_ssim":["admin_set/default"],"degree_tesim":["Ph.D."],"advisor_tesim":["Chair: David L. Meyer."],"college_tesim":["Other"],"department_tesim":["Other"],"etd_publisher_tesim":["University of Cincinnati"],"creator_tesim":["Greenstein, Benjamin Joel."],"publisher_tesim":["University of Cincinnati"],"subject_tesim":["Paleontology","Geology"],"language_tesim":["English"],"description_tesim":["The nature of taphonomic overprint affecting the fossil records of the regular echinoid Families Cidaridae, Diadematidae, Toxopneustidae and Echinometridae is investigated using a synthesis of actualistic and literature-derived data. The actualistic portion of this study focuses on the following extant members of the four families: Eucidaris tribuloides, Diadema antillarum, Tripneustes ventricosus and Echinometra lucunter. Population censuses of these animals in tropical reef and near-reef environments demonstrate that the distribution of macro- and microscopic skeletal material does not reflect the distribution of the living fauna. Field experiments with freshly-killed carcasses of Eucidaris, Diadema and Echinometra indicate that loss of all organic tissue occurs within six days after death, reducing these echinoids to essentially bleached carcasses."],"license_tesim":["http://rightsstatements.org/vocab/InC/1.0/"],"date_created_tesim":["1990"],"thumbnail_path_ss":"/downloads/cj82k742g?file=thumbnail","suppressed_bsi":false,"actionable_workflow_roles_ssim":["admin_set/default-default-depositing"],"workflow_state_name_ssim":["deposited"],"member_ids_ssim":["cj82k742g"],"file_set_ids_ssim":["cj82k742g"],"visibility_ssi":"open","admin_set_tesim":["Default Admin Set"],"sort_title_ssi":"INTEGRATED STUDY OF ECHINOID TAPHONOMY PREDICTIONS FOR THE FOSSIL RECORD OF FOUR ECHINOID FAMILIES","human_readable_type_tesim":["Etd"],"read_access_group_ssim":["public"],"edit_access_person_ssim":["ucdp@uc.edu"],"nesting_collection__pathnames_ssim":["m039k492n"],"nesting_collection__deepest_nested_depth_isi":1,"_version_":1697082870329245696,"timestamp":"2021-04-15T05:25:46.246Z","score":0.00049999997},{"system_create_dtsi":"2018-03-26T15:24:28Z","system_modified_dtsi":"2018-03-27T16:05:38Z","has_model_ssim":["Etd"],"id":"8336h194p","accessControl_ssim":["e4669bf2-b8cd-4c07-be27-30da0fcef8f9"],"hasRelatedMediaFragment_ssim":["1c18df81z"],"hasRelatedImage_ssim":["1c18df81z"],"depositor_ssim":["ucdp@uc.edu"],"depositor_tesim":["ucdp@uc.edu"],"title_tesim":["Experimental And Numerical Study Of Low Pressure Mineral Melt Equilibria In Alkaline Lavas."],"date_uploaded_dtsi":"2018-03-26T15:24:28Z","date_modified_dtsi":"2018-03-26T15:24:28Z","isPartOf_ssim":["admin_set/default"],"degree_tesim":["Ph.D."],"advisor_tesim":["Adviser: Attila I. Kilinc."],"college_tesim":["Other"],"department_tesim":["Other"],"etd_publisher_tesim":["University of Cincinnati"],"creator_tesim":["Camur, Mehmet Zeki."],"publisher_tesim":["University of Cincinnati"],"subject_tesim":["Mineralogy","Geochemistry","Geology"],"language_tesim":["English"],"description_tesim":["This dissertation is a contribution toward low pressure geochemistry and petrology of alkaline rocks. In order to analyze the phase equilibria in multiply saturated potassic alkaline systems, experiments were performed at one atmosphere pressure and under the $\\rm f\\sb{O2}\\sim QFM$ buffer. Range of temperature covered in this study is 1060-1250$\\sp\\circ$C. In addition, temperature and composition dependency of low pressure mineral-melt equilibria involving olivine, pyroxenes, plagioclase, nepheline, and leucite were modeled using empirical equations."],"license_tesim":["http://rightsstatements.org/vocab/InC/1.0/"],"date_created_tesim":["1989"],"thumbnail_path_ss":"/downloads/1c18df81z?file=thumbnail","suppressed_bsi":false,"actionable_workflow_roles_ssim":["admin_set/default-default-depositing"],"workflow_state_name_ssim":["deposited"],"member_ids_ssim":["1c18df81z"],"file_set_ids_ssim":["1c18df81z"],"visibility_ssi":"open","admin_set_tesim":["Default Admin Set"],"sort_title_ssi":"EXPERIMENTAL AND NUMERICAL STUDY OF LOW PRESSURE MINERAL MELT EQUILIBRIA IN ALKALINE LAVAS","human_readable_type_tesim":["Etd"],"read_access_group_ssim":["public"],"edit_access_person_ssim":["ucdp@uc.edu"],"nesting_collection__pathnames_ssim":["8336h194p"],"nesting_collection__deepest_nested_depth_isi":1,"_version_":1697114047961366528,"timestamp":"2021-04-15T13:41:19.553Z","score":0.00049999997},{"system_create_dtsi":"2018-03-26T15:24:14Z","system_modified_dtsi":"2018-03-27T16:05:38Z","has_model_ssim":["Etd"],"id":"qb98mf474","accessControl_ssim":["8647b1d0-f204-46ce-8322-871dea3f16fe"],"hasRelatedMediaFragment_ssim":["r781wg04p"],"hasRelatedImage_ssim":["r781wg04p"],"depositor_ssim":["ucdp@uc.edu"],"depositor_tesim":["ucdp@uc.edu"],"title_tesim":["On The Role Of Atmospheric Gravity Waves In Mesospheric Dynamics."],"date_uploaded_dtsi":"2018-03-26T15:24:14Z","date_modified_dtsi":"2018-03-26T15:24:14Z","isPartOf_ssim":["admin_set/default"],"degree_tesim":["Ph.D."],"advisor_tesim":["Adviser: T. F. Tuan."],"college_tesim":["Other"],"department_tesim":["Other"],"etd_publisher_tesim":["University of Cincinnati"],"creator_tesim":["Makhlouf, Usama Butros."],"publisher_tesim":["University of Cincinnati"],"subject_tesim":["Geophysics","Physics, General"],"language_tesim":["English"],"description_tesim":["The effects of downward gravity wave reflection from atmospheric structure and horizontal winds; the geometry of the wave source and observation region; and the relative importance of the horizontal and vertical transport are being investigated for several different but often used gravity wave models. A quantitative study is also made on the relative importance of the purely gravitationally induced compression (G.I.C.) due to fluid particle altitude change and the actual wave compression which can occur at a fixed altitude in a gravity wave."],"license_tesim":["http://rightsstatements.org/vocab/InC/1.0/"],"date_created_tesim":["1989"],"thumbnail_path_ss":"/downloads/r781wg04p?file=thumbnail","suppressed_bsi":false,"actionable_workflow_roles_ssim":["admin_set/default-default-depositing"],"workflow_state_name_ssim":["deposited"],"member_ids_ssim":["r781wg04p"],"file_set_ids_ssim":["r781wg04p"],"visibility_ssi":"open","admin_set_tesim":["Default Admin Set"],"sort_title_ssi":"ON THE ROLE OF ATMOSPHERIC GRAVITY WAVES IN MESOSPHERIC DYNAMICS","human_readable_type_tesim":["Etd"],"read_access_group_ssim":["public"],"edit_access_person_ssim":["ucdp@uc.edu"],"nesting_collection__pathnames_ssim":["qb98mf474"],"nesting_collection__deepest_nested_depth_isi":1,"_version_":1697100693724200960,"timestamp":"2021-04-15T10:09:03.960Z","score":0.00049999997},{"system_create_dtsi":"2018-03-26T15:24:01Z","system_modified_dtsi":"2018-03-27T16:05:38Z","has_model_ssim":["Etd"],"id":"cn69m4153","accessControl_ssim":["b326f0fd-cb97-475c-b413-801f89795308"],"hasRelatedMediaFragment_ssim":["m900nt44j"],"hasRelatedImage_ssim":["m900nt44j"],"depositor_ssim":["ucdp@uc.edu"],"depositor_tesim":["ucdp@uc.edu"],"title_tesim":["The Mineralogy And Stratigraphic Setting Of The Rocklandian (Upper Ordovician) Deicke And Millbrig K Bentonite Beds Along The Cincinnati Arch And In The Southern Valley And Ridge."],"date_uploaded_dtsi":"2018-03-26T15:24:01Z","date_modified_dtsi":"2018-03-26T15:24:01Z","isPartOf_ssim":["admin_set/default"],"degree_tesim":["Ph.D."],"college_tesim":["Other"],"department_tesim":["Other"],"etd_publisher_tesim":["University of Cincinnati"],"creator_tesim":["Haynes, John Tweedt."],"publisher_tesim":["University of Cincinnati"],"subject_tesim":["Geology"],"language_tesim":["English"],"description_tesim":["Petrographic study of the Deicke and Millbrig K-benonite beds (altered volcanic ash) of Rocklandian age has revealed that they can be distinguished by their non-clay mineralogy. The Deicke phenocryst assemblage is primarily labradorite, Fe-Ti oxides, apatite, and zircon, while the Millbrig assemblage is primarily andesine, quartz, biotite, apatite, and zircon. The Deicke is altered dacitic ash, while the Millbrig is altered rhyodacitic ash."],"license_tesim":["http://rightsstatements.org/vocab/InC/1.0/"],"date_created_tesim":["1989"],"thumbnail_path_ss":"/downloads/m900nt44j?file=thumbnail","suppressed_bsi":false,"actionable_workflow_roles_ssim":["admin_set/default-default-depositing"],"workflow_state_name_ssim":["deposited"],"member_ids_ssim":["m900nt44j"],"file_set_ids_ssim":["m900nt44j"],"visibility_ssi":"open","admin_set_tesim":["Default Admin Set"],"sort_title_ssi":"MINERALOGY AND STRATIGRAPHIC SETTING OF THE ROCKLANDIAN UPPER ORDOVICIAN DEICKE AND MILLBRIG K BENTONITE BEDS ALONG THE CINCINNATI ARCH AND IN THE SOUTHERN VALLEY AND RIDGE","human_readable_type_tesim":["Etd"],"read_access_group_ssim":["public"],"edit_access_person_ssim":["ucdp@uc.edu"],"nesting_collection__pathnames_ssim":["cn69m4153"],"nesting_collection__deepest_nested_depth_isi":1,"_version_":1697086545098440704,"timestamp":"2021-04-15T06:24:10.779Z","score":0.00049999997}],"facets":[{"name":"human_readable_type_sim","items":[{"value":"Image","hits":4797,"label":"Image"},{"value":"Dataset","hits":3723,"label":"Dataset"},{"value":"Etd","hits":994,"label":"Etd"},{"value":"Document","hits":980,"label":"Document"},{"value":"Article","hits":967,"label":"Article"},{"value":"Student Work","hits":756,"label":"Student Work"}],"label":"Human Readable Type Sim"},{"name":"creator_sim","items":[{"value":"Snider, Jerry A. (senior collector)","hits":3484,"label":"Snider, Jerry A. (senior collector)"},{"value":"Tepe, Eric (record/image)","hits":3484,"label":"Tepe, Eric (record/image)"},{"value":"Huston, Ron","hits":2344,"label":"Huston, Ron"},{"value":"He, Si (co-collector)","hits":1093,"label":"He, Si (co-collector)"},{"value":"Meyer, David L.","hits":631,"label":"Meyer, David L."},{"value":"Davis, Jack","hits":611,"label":"Davis, Jack"}],"label":"Creator Sim"},{"name":"subject_sim","items":[{"value":"Kingdom: Plantae","hits":3453,"label":"Kingdom: Plantae"},{"value":"Phylum: Bryophyta","hits":3146,"label":"Phylum: Bryophyta"},{"value":"Class: Bryopsida","hits":2902,"label":"Class: Bryopsida"},{"value":"Biology","hits":2362,"label":"Biology"},{"value":"Order: Hypnales","hits":1190,"label":"Order: Hypnales"},{"value":"Order: Dicranales","hits":369,"label":"Order: Dicranales"}],"label":"Subject Sim"},{"name":"college_sim","items":[{"value":"Arts and Sciences","hits":6146,"label":"Arts and Sciences"},{"value":"Engineering and Applied Science","hits":2772,"label":"Engineering and Applied Science"},{"value":"Design, Architecture, Art and Planning","hits":1236,"label":"Design, Architecture, Art and Planning"},{"value":"Other","hits":1070,"label":"Other"},{"value":"Libraries","hits":671,"label":"Libraries"},{"value":"Education, Criminal Justice, and Human Services","hits":543,"label":"Education, Criminal Justice, and Human Services"}],"label":"College Sim"},{"name":"department_sim","items":[{"value":"Biological Sciences","hits":3503,"label":"Biological Sciences"},{"value":"Mechanical and Materials Engineering","hits":2264,"label":"Mechanical and Materials Engineering"},{"value":"Other","hits":992,"label":"Other"},{"value":"Simpson Center for Urban Futures ","hits":784,"label":"Simpson Center for Urban Futures "},{"value":"Classics","hits":769,"label":"Classics"},{"value":"Romance \u0026 Arabic Languages \u0026 Literat","hits":644,"label":"Romance \u0026 Arabic Languages \u0026 Literat"}],"label":"Department Sim"},{"name":"language_sim","items":[{"value":"English","hits":1957,"label":"English"},{"value":"en_US","hits":224,"label":"en_US"},{"value":"English ","hits":145,"label":"English "},{"value":"Russian","hits":34,"label":"Russian"},{"value":"Spanish","hits":24,"label":"Spanish"},{"value":"German","hits":19,"label":"German"}],"label":"Language Sim"},{"name":"publisher_sim","items":[{"value":"University of Cincinnati, Margaret H. Fulford Herbarium (CINC)","hits":3484,"label":"University of Cincinnati, Margaret H. Fulford Herbarium (CINC)"},{"value":"University of Cincinnati","hits":3011,"label":"University of Cincinnati"},{"value":"University of Cincinnati: Romance and Arabic Languages and Literatures","hits":603,"label":"University of Cincinnati: Romance and Arabic Languages and Literatures"},{"value":"University of Cincinnati ","hits":100,"label":"University of Cincinnati "},{"value":"viDEO sAVant","hits":92,"label":"viDEO sAVant"},{"value":"Benjamin Britton","hits":60,"label":"Benjamin Britton"}],"label":"Publisher Sim"},{"name":"date_created_sim","items":[{"value":"2017","hits":2305,"label":"2017"},{"value":"","hits":211,"label":""},{"value":"2001-03-31","hits":181,"label":"2001-03-31"},{"value":"2017-10-31","hits":163,"label":"2017-10-31"},{"value":"2001-03-30","hits":156,"label":"2001-03-30"},{"value":"2001-03-29","hits":127,"label":"2001-03-29"}],"label":"Date Created Sim"},{"name":"member_of_collection_ids_ssim","items":[{"value":"1r66j250c","hits":3484,"label":"1r66j250c"},{"value":"79407x47z","hits":2123,"label":"79407x47z"},{"value":"05741w32f","hits":341,"label":"05741w32f"},{"value":"bc3871882","hits":225,"label":"bc3871882"},{"value":"x346d4806","hits":219,"label":"x346d4806"},{"value":"bc387z838","hits":189,"label":"bc387z838"}],"label":"Member Of Collection Ids Ssim"},{"name":"generic_type_sim","items":[{"value":"Work","hits":12586,"label":"Work"},{"value":"Collection","hits":174,"label":"Collection"}],"label":"Generic Type Sim"}],"pages":{"current_page":1008,"next_page":1009,"prev_page":1007,"total_pages":1276,"limit_value":10,"offset_value":10070,"total_count":12760,"first_page?":false,"last_page?":false}}}