Matches in SemOpenAlex for { <https://semopenalex.org/work/W3016742730> ?p ?o ?g. }
- W3016742730 abstract "Abstract The Earth's mantle shows large‐scale geochemical heterogeneities bounded by several identifiable end‐member compositions. However, the origin of extreme mantle reservoirs, for example, high 238 U/ 204 Pb (HIMU), and their location in the Earth's interior remains poorly constrained. Clinopyroxenes from late Cenozoic Wudi lavas in eastern China have heterogeneous Pb isotopic compositions, even though the erupted lavas are isotopically homogeneous. Our new results provide, to our knowledge, the first evidence for the existence of a HIMU‐like component in the sources of late Cenozoic lavas. Analyses of olivines and their host lavas indicate that the basaltic melts are derived from partial melting of carbonated peridotite. The HIMU source is likely to be younger than 700 Ma old and related to subduction events of the Paleo‐Asian ocean. In addition to deep and ancient recycling, storage of a metasomatically produced mantle reservoir in the mantle transition zone may be an important mechanism for developing extreme isotopic signatures." @default.
- W3016742730 created "2020-04-24" @default.
- W3016742730 creator A5009286063 @default.
- W3016742730 creator A5025578211 @default.
- W3016742730 creator A5037808701 @default.
- W3016742730 creator A5058068415 @default.
- W3016742730 creator A5061481399 @default.
- W3016742730 creator A5074195634 @default.
- W3016742730 creator A5088290596 @default.
- W3016742730 date "2020-05-04" @default.
- W3016742730 modified "2023-10-17" @default.
- W3016742730 title "The Mantle Transition Zone Hosts the Missing HIMU Reservoir Beneath Eastern China" @default.
- W3016742730 cites W1524308656 @default.
- W3016742730 cites W1610512145 @default.
- W3016742730 cites W1656874552 @default.
- W3016742730 cites W1941456882 @default.
- W3016742730 cites W1963661785 @default.
- W3016742730 cites W1969859799 @default.
- W3016742730 cites W1974509843 @default.
- W3016742730 cites W1980456727 @default.
- W3016742730 cites W1984787349 @default.
- W3016742730 cites W1991521847 @default.
- W3016742730 cites W1997859575 @default.
- W3016742730 cites W2002041994 @default.
- W3016742730 cites W2004856555 @default.
- W3016742730 cites W2005195754 @default.
- W3016742730 cites W2005918222 @default.
- W3016742730 cites W2006592158 @default.
- W3016742730 cites W2011607179 @default.
- W3016742730 cites W2023419440 @default.
- W3016742730 cites W2025041546 @default.
- W3016742730 cites W2028642650 @default.
- W3016742730 cites W2030851389 @default.
- W3016742730 cites W2039382632 @default.
- W3016742730 cites W2039872199 @default.
- W3016742730 cites W2041911594 @default.
- W3016742730 cites W2044032834 @default.
- W3016742730 cites W2047121008 @default.
- W3016742730 cites W2063948740 @default.
- W3016742730 cites W2069053606 @default.
- W3016742730 cites W2073905341 @default.
- W3016742730 cites W2074843698 @default.
- W3016742730 cites W2075401877 @default.
- W3016742730 cites W2081958168 @default.
- W3016742730 cites W2084285443 @default.
- W3016742730 cites W2089369579 @default.
- W3016742730 cites W2098150726 @default.
- W3016742730 cites W2105942108 @default.
- W3016742730 cites W2106079840 @default.
- W3016742730 cites W2130869872 @default.
- W3016742730 cites W2131497882 @default.
- W3016742730 cites W2133042542 @default.
- W3016742730 cites W2148501813 @default.
- W3016742730 cites W2152572862 @default.
- W3016742730 cites W2170213361 @default.
- W3016742730 cites W2214888759 @default.
- W3016742730 cites W2257315609 @default.
- W3016742730 cites W2381600577 @default.
- W3016742730 cites W2513297223 @default.
- W3016742730 cites W2546817987 @default.
- W3016742730 cites W2555955218 @default.
- W3016742730 cites W2560573045 @default.
- W3016742730 cites W2565239340 @default.
- W3016742730 cites W2593940692 @default.
- W3016742730 cites W2772931677 @default.
- W3016742730 cites W2780478079 @default.
- W3016742730 cites W2800604401 @default.
- W3016742730 cites W2945221819 @default.
- W3016742730 cites W4245638129 @default.
- W3016742730 doi "https://doi.org/10.1029/2020gl087260" @default.
- W3016742730 hasPublicationYear "2020" @default.
- W3016742730 type Work @default.
- W3016742730 sameAs 3016742730 @default.
- W3016742730 citedByCount "6" @default.
- W3016742730 countsByYear W30167427302021 @default.
- W3016742730 countsByYear W30167427302022 @default.
- W3016742730 crossrefType "journal-article" @default.
- W3016742730 hasAuthorship W3016742730A5009286063 @default.
- W3016742730 hasAuthorship W3016742730A5025578211 @default.
- W3016742730 hasAuthorship W3016742730A5037808701 @default.
- W3016742730 hasAuthorship W3016742730A5058068415 @default.
- W3016742730 hasAuthorship W3016742730A5061481399 @default.
- W3016742730 hasAuthorship W3016742730A5074195634 @default.
- W3016742730 hasAuthorship W3016742730A5088290596 @default.
- W3016742730 hasConcept C109007969 @default.
- W3016742730 hasConcept C127313418 @default.
- W3016742730 hasConcept C151730666 @default.
- W3016742730 hasConcept C161509811 @default.
- W3016742730 hasConcept C163686574 @default.
- W3016742730 hasConcept C17409809 @default.
- W3016742730 hasConcept C1965285 @default.
- W3016742730 hasConcept C58097730 @default.
- W3016742730 hasConcept C67236022 @default.
- W3016742730 hasConcept C73707237 @default.
- W3016742730 hasConcept C77928131 @default.
- W3016742730 hasConcept C79572550 @default.
- W3016742730 hasConcept C84372278 @default.
- W3016742730 hasConceptScore W3016742730C109007969 @default.
- W3016742730 hasConceptScore W3016742730C127313418 @default.
- W3016742730 hasConceptScore W3016742730C151730666 @default.