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• W2011076039 abstract "Research Article| May 01, 2006 Transgressive oversized radial ooid facies in the Late Jurassic Adriatic Platform interior: Low-energy precipitates from highly supersaturated hypersaline waters Antun Husinec; Antun Husinec 1Croatian Geological Survey, Sachsova 2, HR-10000 Zagreb, Croatia Search for other works by this author on: GSW Google Scholar J. Fred Read J. Fred Read 2Department of Geosciences, Virginia Tech, 4044 Derring Hall, Blacksburg, Virginia 24061, USA Search for other works by this author on: GSW Google Scholar Author and Article Information Antun Husinec 1Croatian Geological Survey, Sachsova 2, HR-10000 Zagreb, Croatia J. Fred Read 2Department of Geosciences, Virginia Tech, 4044 Derring Hall, Blacksburg, Virginia 24061, USA Publisher: Geological Society of America Received: 28 Jun 2005 Revision Received: 23 Jan 2006 Accepted: 01 Feb 2006 First Online: 08 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Geological Society of America GSA Bulletin (2006) 118 (5-6): 550–556. https://doi.org/10.1130/B25864.1 Article history Received: 28 Jun 2005 Revision Received: 23 Jan 2006 Accepted: 01 Feb 2006 First Online: 08 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Antun Husinec, J. Fred Read; Transgressive oversized radial ooid facies in the Late Jurassic Adriatic Platform interior: Low-energy precipitates from highly supersaturated hypersaline waters. GSA Bulletin 2006;; 118 (5-6): 550–556. doi: https://doi.org/10.1130/B25864.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract Dark-gray oolitic units characterized by oversized ooids with primary radial calcite fabrics occur in the interior of the Late Jurassic Late Tithonian, Adriatic Platform, a large Mesozoic, Tethyan isolated platform in Croatia. They differ from open-marine, platform-margin ooid grainstones in their dark color, cerebroid outlines, broken and recoated grains, abundant inclusions, highly restricted biota, and lack of cross-stratification. They have been interpreted as being of vadose origin (“vadoids”) at tops of upward-shallowing parasequences. However, detailed sections show that most oolitic units occur at bases of precessional parasequences, overlying erosional surfaces on fenestral carbonates. The oolitic units are similar to quiet-water ooids that form today in low-energy settings. They developed in an arid climate during initial transgression of supratidal flats, along low-energy shores seaward of tidal flats, and along the margins of restricted lagoons and intertidal ponds. Superimposed fenestral fabrics, meniscus micrite cements, and grain breakage occurred as they aggraded to high-tide level and were subjected to wetting and drying, thermal expansion and contraction, and wind transport. They migrated landward with transgression, forming extensive sheets, and were overlain by subtidal lagoonal facies that shallow up into fenestral carbonates. These distinctive facies may have been overlooked in the geological record, or their geological distribution requires juxtaposition of calcite seas, high-calcite supersaturation states, arid climate, and presence of flat-topped carbonate platforms in a greenhouse world. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2011076039 title "Transgressive oversized radial ooid facies in the Late Jurassic Adriatic Platform interior: Low-energy precipitates from highly supersaturated hypersaline waters" @default.
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