FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2118604845> ?p ?o ?g. }

• W2118604845 endingPage "1304" @default.
• W2118604845 startingPage "1296" @default.
• W2118604845 abstract "Research Article| September 01, 2008 Constraining ultrahigh-pressure (UHP) metamorphism and titanium ore formation from an infrared microthermometric study of fluid inclusions in rutile from Donghai UHP eclogites, eastern China Pei Ni; Pei Ni † 1State Key Laboratory for Mineral Deposits Research, Institute of Geo-fluids, Department of Earth Sciences, Nanjing University, Nanjing 210093, China †E-mail: peini@nju.edu.cn Search for other works by this author on: GSW Google Scholar Xia Zhu; Xia Zhu 1State Key Laboratory for Mineral Deposits Research, Institute of Geo-fluids, Department of Earth Sciences, Nanjing University, Nanjing 210093, China Search for other works by this author on: GSW Google Scholar Rucheng Wang; Rucheng Wang 1State Key Laboratory for Mineral Deposits Research, Institute of Geo-fluids, Department of Earth Sciences, Nanjing University, Nanjing 210093, China Search for other works by this author on: GSW Google Scholar Kun Shen; Kun Shen 2Institute of Geological Sciences of Shandong, Jinan 250013, China Search for other works by this author on: GSW Google Scholar Zeming Zhang; Zeming Zhang 3Institute of Geology, Chinese Academy of Geological Sciences, Beijing 10037, China Search for other works by this author on: GSW Google Scholar Jiansheng Qiu; Jiansheng Qiu 4State Key Laboratory for Mineral Deposit Research, Department of Earth Sciences, Nanjing University, Nanjing 210093, China Search for other works by this author on: GSW Google Scholar Jianping Huang Jianping Huang 5Geological Survey of Jiangsu, Nanjing 210093, China Search for other works by this author on: GSW Google Scholar Author and Article Information Pei Ni † 1State Key Laboratory for Mineral Deposits Research, Institute of Geo-fluids, Department of Earth Sciences, Nanjing University, Nanjing 210093, China Xia Zhu 1State Key Laboratory for Mineral Deposits Research, Institute of Geo-fluids, Department of Earth Sciences, Nanjing University, Nanjing 210093, China Rucheng Wang 1State Key Laboratory for Mineral Deposits Research, Institute of Geo-fluids, Department of Earth Sciences, Nanjing University, Nanjing 210093, China Kun Shen 2Institute of Geological Sciences of Shandong, Jinan 250013, China Zeming Zhang 3Institute of Geology, Chinese Academy of Geological Sciences, Beijing 10037, China Jiansheng Qiu 4State Key Laboratory for Mineral Deposit Research, Department of Earth Sciences, Nanjing University, Nanjing 210093, China Jianping Huang 5Geological Survey of Jiangsu, Nanjing 210093, China †E-mail: peini@nju.edu.cn Publisher: Geological Society of America Received: 13 Aug 2006 Revision Received: 30 Dec 2007 Received: 14 Jan 2008 First Online: 02 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 © 2008 Geological Society of America GSA Bulletin (2008) 120 (9-10): 1296–1304. https://doi.org/10.1130/B26090.1 Article history Received: 13 Aug 2006 Revision Received: 30 Dec 2007 Received: 14 Jan 2008 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Pei Ni, Xia Zhu, Rucheng Wang, Kun Shen, Zeming Zhang, Jiansheng Qiu, Jianping Huang; Constraining ultrahigh-pressure (UHP) metamorphism and titanium ore formation from an infrared microthermometric study of fluid inclusions in rutile from Donghai UHP eclogites, eastern China. GSA Bulletin 2008;; 120 (9-10): 1296–1304. doi: https://doi.org/10.1130/B26090.1 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 Eclogites in the Donghai area of the Sulu ultrahigh-pressure (UHP) metamorphic belt in eastern China contain both disseminated rutile and rutile deposits. The rutile occurs as small inclusions in garnet, omphacite, phengite, and quartz, as larger euhedral to subhedral grains in equilibrium with garnet, omphacite, phengite, and kyanite, and as discrete veinlets, aggregates, and megacrysts in cracks and along grain boundaries. To investigate the processes of rutile mineralization and its relationship to the evolution of the Sulu UHP metamorphic belt, we sampled the exposed Maobei deposit at Donghai and drill core between 100 and 2000 m in the nearby Chinese Continental Scientific Drilling Project (CCSD) main hole to carry out a detailed infrared microthermometric fluid inclusion study. Three types of fluid inclusions were identified: aqueous (Type I), CO2-H2O (Type II), and CH4 (Type III). Type I and Type II inclusions are the most common. Primary and pseudosecondary Type I inclusions, which were trapped during recrystallization of the eclogite or early amphibolite facies retrograde metamorphism, have a narrow range of homogenization temperatures but a wide range of salinities. In contrast, secondary Type I inclusions, which formed entirely during retrograde amphibolite-facies metamorphism associated with exhumation of the UHP rocks, have higher and more varied homogenization temperatures but medium to low salinities. Type II inclusions formed contemporaneously with the Type I variety and are characterized by having small amounts of CO2 and N2 in addition to H2O. In addition, some of the rutile grains contain sparse inclusions composed of CH4 (Type III). Our results combined with those of previous studies, suggest a great diversity of fluid composition in the peak metamorphic to early retrograde stages, implying very limited fluid-rock interaction during syn- to post-peak high-pressure (HP) and UHP metamorphism. This study shows that infrared microthermometric investigation of fluid inclusions can provide information not only on the composition of titanium ore-forming fluids but also on the relationship between mineralization and the evolution of UHP metamorphic belt. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W2118604845 created "2016-06-24" @default.
• W2118604845 creator A5005793265 @default.
• W2118604845 creator A5007623581 @default.
• W2118604845 creator A5020035674 @default.
• W2118604845 creator A5046420497 @default.
• W2118604845 creator A5048793244 @default.
• W2118604845 creator A5049050105 @default.
• W2118604845 creator A5049270029 @default.
• W2118604845 date "2008-09-01" @default.
• W2118604845 modified "2023-10-11" @default.
• W2118604845 title "Constraining ultrahigh-pressure (UHP) metamorphism and titanium ore formation from an infrared microthermometric study of fluid inclusions in rutile from Donghai UHP eclogites, eastern China" @default.
• W2118604845 cites W1580768618 @default.
• W2118604845 cites W1964408118 @default.
• W2118604845 cites W1967418588 @default.
• W2118604845 cites W1967545344 @default.
• W2118604845 cites W1967658665 @default.
• W2118604845 cites W1975652198 @default.
• W2118604845 cites W1985195619 @default.
• W2118604845 cites W1990060235 @default.
• W2118604845 cites W2004896572 @default.
• W2118604845 cites W2005175480 @default.
• W2118604845 cites W2006471814 @default.
• W2118604845 cites W2008499749 @default.
• W2118604845 cites W2011049153 @default.
• W2118604845 cites W2015222366 @default.
• W2118604845 cites W2016511472 @default.
• W2118604845 cites W2018693918 @default.
• W2118604845 cites W2023004601 @default.
• W2118604845 cites W2024068462 @default.
• W2118604845 cites W2024086248 @default.
• W2118604845 cites W2031972408 @default.
• W2118604845 cites W2039948923 @default.
• W2118604845 cites W2040903195 @default.
• W2118604845 cites W2042402460 @default.
• W2118604845 cites W2044404173 @default.
• W2118604845 cites W2044537972 @default.
• W2118604845 cites W2044600702 @default.
• W2118604845 cites W2048505147 @default.
• W2118604845 cites W2050832078 @default.
• W2118604845 cites W2054310315 @default.
• W2118604845 cites W2055363559 @default.
• W2118604845 cites W2063341968 @default.
• W2118604845 cites W2063754919 @default.
• W2118604845 cites W2068137312 @default.
• W2118604845 cites W2074452712 @default.
• W2118604845 cites W2074525585 @default.
• W2118604845 cites W2078327201 @default.
• W2118604845 cites W2081394262 @default.
• W2118604845 cites W2086959586 @default.
• W2118604845 cites W2088578530 @default.
• W2118604845 cites W2168626633 @default.
• W2118604845 cites W2430155535 @default.
• W2118604845 cites W2485975790 @default.
• W2118604845 cites W3152033523 @default.
• W2118604845 doi "https://doi.org/10.1130/b26090.1" @default.
• W2118604845 hasPublicationYear "2008" @default.
• W2118604845 type Work @default.
• W2118604845 sameAs 2118604845 @default.
• W2118604845 citedByCount "19" @default.
• W2118604845 countsByYear W21186048452012 @default.
• W2118604845 countsByYear W21186048452014 @default.
• W2118604845 countsByYear W21186048452015 @default.
• W2118604845 countsByYear W21186048452018 @default.
• W2118604845 countsByYear W21186048452019 @default.
• W2118604845 countsByYear W21186048452021 @default.
• W2118604845 countsByYear W21186048452022 @default.
• W2118604845 countsByYear W21186048452023 @default.
• W2118604845 crossrefType "journal-article" @default.
• W2118604845 hasAuthorship W2118604845A5005793265 @default.
• W2118604845 hasAuthorship W2118604845A5007623581 @default.
• W2118604845 hasAuthorship W2118604845A5020035674 @default.
• W2118604845 hasAuthorship W2118604845A5046420497 @default.
• W2118604845 hasAuthorship W2118604845A5048793244 @default.
• W2118604845 hasAuthorship W2118604845A5049050105 @default.
• W2118604845 hasAuthorship W2118604845A5049270029 @default.
• W2118604845 hasConcept C112764850 @default.
• W2118604845 hasConcept C127313418 @default.
• W2118604845 hasConcept C151730666 @default.
• W2118604845 hasConcept C16674752 @default.
• W2118604845 hasConcept C166957645 @default.
• W2118604845 hasConcept C173347748 @default.
• W2118604845 hasConcept C17409809 @default.
• W2118604845 hasConcept C191935318 @default.
• W2118604845 hasConcept C2778304055 @default.
• W2118604845 hasConcept C2984488660 @default.
• W2118604845 hasConcept C58097730 @default.
• W2118604845 hasConcept C66264921 @default.
• W2118604845 hasConcept C77928131 @default.
• W2118604845 hasConcept C95457728 @default.
• W2118604845 hasConceptScore W2118604845C112764850 @default.
• W2118604845 hasConceptScore W2118604845C127313418 @default.
• W2118604845 hasConceptScore W2118604845C151730666 @default.
• W2118604845 hasConceptScore W2118604845C16674752 @default.
• W2118604845 hasConceptScore W2118604845C166957645 @default.
• W2118604845 hasConceptScore W2118604845C173347748 @default.
• W2118604845 hasConceptScore W2118604845C17409809 @default.
• W2118604845 hasConceptScore W2118604845C191935318 @default.

• next