Matches in SemOpenAlex for { <https://semopenalex.org/work/W2083372372> ?p ?o ?g. }
- W2083372372 endingPage "101" @default.
- W2083372372 startingPage "85" @default.
- W2083372372 abstract "Shifts in world barite production since the 1980s have resulted in China becoming the world's largest barite-producing country followed by the US and India. Most barite produced for use in drilling fluids is derived from black shale- and chert-hosted, stratiform marine deposits. In China, Late Proterozoic to Early Cambrian marine barite deposits occur on the oceanic margins of the Yangtze platform, in the Qinling region in the north and the Jiangnan region in the south. Most US ore-grade deposits are in the Nevada barite belt; most commercial deposits occur in Ordovician and Devonian marine rocks along the western margin of the early Paleozoic North American continent. Production in India is predominantly from a single Middle Proterozoic deposit in a sedimentary basin located on Archean basement in Andrah Pradesh. The geologic and geochemical characteristics of the deposits are consistent with origins from a variety of sedimentary-exhalative processes, with biogenic processes contributing to the concentration of some seafloor barite. Linear distributions of clusters of lenticular deposits suggest a geographic relationship to syndepositional seafloor fault zones. Sulfur isotope data of the barite deposits range from values that are similar to coeval seawater sulfate to significantly higher δ34S values. Strontium isotope values of continental-margin-type deposits in Nevada and China are less radiogenic than those of cratonic-rift deposits (e.g. Meggen and Rammelsberg). Comparison of Lan/Cen ratios of barite in the Qinling region of China with marine chert ratios suggests a relationship to hydrothermal fluids, whereas ratios from the Jiangnan region and Nevada can be interpreted as reflecting a biogenic influence. The California Borderland provides a potential modern analog where hydrothermal barium is being deposited on the seafloor in fault-block-bounded basins. Anoxic to dysaerobic conditions on some marine basin floors result from upwelling, nutrient-rich currents and high productivity in surface waters. In this setting, biogenic processes could contribute to the concentration of barium from hydrothermal sources." @default.
- W2083372372 created "2016-06-24" @default.
- W2083372372 creator A5015261639 @default.
- W2083372372 creator A5058543617 @default.
- W2083372372 creator A5068782130 @default.
- W2083372372 date "2004-01-01" @default.
- W2083372372 modified "2023-10-01" @default.
- W2083372372 title "Comparison of some sediment-hosted, stratiform barite deposits in China, the United States, and India" @default.
- W2083372372 cites W1682777677 @default.
- W2083372372 cites W1965785221 @default.
- W2083372372 cites W1966826280 @default.
- W2083372372 cites W1979124271 @default.
- W2083372372 cites W1980146808 @default.
- W2083372372 cites W1985060923 @default.
- W2083372372 cites W1996138242 @default.
- W2083372372 cites W1996266935 @default.
- W2083372372 cites W1996793675 @default.
- W2083372372 cites W2007986887 @default.
- W2083372372 cites W2053615902 @default.
- W2083372372 cites W2057828470 @default.
- W2083372372 cites W2057944078 @default.
- W2083372372 cites W2060733703 @default.
- W2083372372 cites W2067609750 @default.
- W2083372372 cites W2071402402 @default.
- W2083372372 cites W2082972472 @default.
- W2083372372 cites W2083217550 @default.
- W2083372372 cites W2083966883 @default.
- W2083372372 cites W2094972513 @default.
- W2083372372 cites W2104560951 @default.
- W2083372372 cites W2125571496 @default.
- W2083372372 cites W2147633252 @default.
- W2083372372 cites W2150005997 @default.
- W2083372372 cites W2150275801 @default.
- W2083372372 cites W2156433034 @default.
- W2083372372 cites W2164521762 @default.
- W2083372372 doi "https://doi.org/10.1016/j.oregeorev.2003.08.009" @default.
- W2083372372 hasPublicationYear "2004" @default.
- W2083372372 type Work @default.
- W2083372372 sameAs 2083372372 @default.
- W2083372372 citedByCount "72" @default.
- W2083372372 countsByYear W20833723722012 @default.
- W2083372372 countsByYear W20833723722013 @default.
- W2083372372 countsByYear W20833723722014 @default.
- W2083372372 countsByYear W20833723722015 @default.
- W2083372372 countsByYear W20833723722016 @default.
- W2083372372 countsByYear W20833723722017 @default.
- W2083372372 countsByYear W20833723722018 @default.
- W2083372372 countsByYear W20833723722019 @default.
- W2083372372 countsByYear W20833723722020 @default.
- W2083372372 countsByYear W20833723722021 @default.
- W2083372372 countsByYear W20833723722022 @default.
- W2083372372 countsByYear W20833723722023 @default.
- W2083372372 crossrefType "journal-article" @default.
- W2083372372 hasAuthorship W2083372372A5015261639 @default.
- W2083372372 hasAuthorship W2083372372A5058543617 @default.
- W2083372372 hasAuthorship W2083372372A5068782130 @default.
- W2083372372 hasConcept C107832698 @default.
- W2083372372 hasConcept C117485682 @default.
- W2083372372 hasConcept C127313418 @default.
- W2083372372 hasConcept C127413603 @default.
- W2083372372 hasConcept C13106087 @default.
- W2083372372 hasConcept C147176958 @default.
- W2083372372 hasConcept C149347711 @default.
- W2083372372 hasConcept C151730666 @default.
- W2083372372 hasConcept C156622251 @default.
- W2083372372 hasConcept C17409809 @default.
- W2083372372 hasConcept C201867031 @default.
- W2083372372 hasConcept C2776152364 @default.
- W2083372372 hasConcept C2780416900 @default.
- W2083372372 hasConcept C2781297371 @default.
- W2083372372 hasConcept C6494504 @default.
- W2083372372 hasConcept C77928131 @default.
- W2083372372 hasConcept C93033518 @default.
- W2083372372 hasConceptScore W2083372372C107832698 @default.
- W2083372372 hasConceptScore W2083372372C117485682 @default.
- W2083372372 hasConceptScore W2083372372C127313418 @default.
- W2083372372 hasConceptScore W2083372372C127413603 @default.
- W2083372372 hasConceptScore W2083372372C13106087 @default.
- W2083372372 hasConceptScore W2083372372C147176958 @default.
- W2083372372 hasConceptScore W2083372372C149347711 @default.
- W2083372372 hasConceptScore W2083372372C151730666 @default.
- W2083372372 hasConceptScore W2083372372C156622251 @default.
- W2083372372 hasConceptScore W2083372372C17409809 @default.
- W2083372372 hasConceptScore W2083372372C201867031 @default.
- W2083372372 hasConceptScore W2083372372C2776152364 @default.
- W2083372372 hasConceptScore W2083372372C2780416900 @default.
- W2083372372 hasConceptScore W2083372372C2781297371 @default.
- W2083372372 hasConceptScore W2083372372C6494504 @default.
- W2083372372 hasConceptScore W2083372372C77928131 @default.
- W2083372372 hasConceptScore W2083372372C93033518 @default.
- W2083372372 hasIssue "1-2" @default.
- W2083372372 hasLocation W20833723721 @default.
- W2083372372 hasOpenAccess W2083372372 @default.
- W2083372372 hasPrimaryLocation W20833723721 @default.
- W2083372372 hasRelatedWork W2001949408 @default.
- W2083372372 hasRelatedWork W2017846080 @default.
- W2083372372 hasRelatedWork W2022266193 @default.
- W2083372372 hasRelatedWork W2022392508 @default.