{"title":"高3He/4He羽流更热,更容易融化:来自海洋岛屿玄武岩的岩石学和地球化学证据","authors":"Sunna Harðardóttir, Matthew G. Jackson","doi":"10.1016/j.epsl.2025.119490","DOIUrl":null,"url":null,"abstract":"<div><div>High <sup>3</sup>He/<sup>4</sup>He (i.e., <sup>3</sup>He/<sup>4</sup>He above the convecting upper mantle mid-ocean ridge basalt range (8 ± 2 R<sub>A</sub>)) is a rare component identified in hotspots that sample an early-formed, less-degassed domain in the planet. Relationships between the maximum <sup>3</sup>He/<sup>4</sup>He and high hotspot buoyancy flux, and between maximum <sup>3</sup>He/<sup>4</sup>He and low seismic shear-wave velocity anomalies, suggest that high <sup>3</sup>He/<sup>4</sup>He is entrained only by the hottest and most buoyant mantle plumes. A prediction of this model is that the high <sup>3</sup>He/<sup>4</sup>He component is sampled by high-degree melting. We use a new geochemical database of ocean island lavas to demonstrate that high <sup>3</sup>He/<sup>4</sup>He is found only in tholeiitic (low alkali index) and mildly alkalic (intermediate alkali index) lavas, which result from high and moderate degrees of melting, respectively. Highly alkalic (high alkali index) lavas that are generated by low degrees of melting are not observed to have very high <sup>3</sup>He/<sup>4</sup>He. These observations support a model where the highest <sup>3</sup>He/<sup>4</sup>He plumes are the hottest and therefore melt to high degrees, which results in generation of tholeiites and mildly alkalic lavas. However, our observations suggest that high degrees of melting of hot plumes is a necessary but insufficient condition for generation of high <sup>3</sup>He/<sup>4</sup>He lavas. High degrees of melting of mantle domains with a high fraction of recycled material and/or depleted mantle material—both of which have low <sup>3</sup>He/<sup>4</sup>He—will generate low <sup>3</sup>He/<sup>4</sup>He lavas. Thus, only hot melting of mantle domains that have relatively pure high <sup>3</sup>He/<sup>4</sup>He source material (i.e., little or no recycled material or depleted low <sup>3</sup>He/<sup>4</sup>He mantle material) will result in generation of high <sup>3</sup>He/<sup>4</sup>He lavas. The conclusion that high <sup>3</sup>He/<sup>4</sup>He plumes melt more is supported by geophysical observations that suggest high <sup>3</sup>He/<sup>4</sup>He plumes are hotter—they have higher buoyancy flux and lower shear-wave velocity anomalies in the upper mantle—and hotter plumes should melt more than cooler plumes.</div></div>","PeriodicalId":11481,"journal":{"name":"Earth and Planetary Science Letters","volume":"666 ","pages":"Article 119490"},"PeriodicalIF":4.8000,"publicationDate":"2025-06-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"High 3He/4He plumes are hotter and melt more: evidence from the petrology and geochemistry of ocean island basalts\",\"authors\":\"Sunna Harðardóttir, Matthew G. Jackson\",\"doi\":\"10.1016/j.epsl.2025.119490\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>High <sup>3</sup>He/<sup>4</sup>He (i.e., <sup>3</sup>He/<sup>4</sup>He above the convecting upper mantle mid-ocean ridge basalt range (8 ± 2 R<sub>A</sub>)) is a rare component identified in hotspots that sample an early-formed, less-degassed domain in the planet. Relationships between the maximum <sup>3</sup>He/<sup>4</sup>He and high hotspot buoyancy flux, and between maximum <sup>3</sup>He/<sup>4</sup>He and low seismic shear-wave velocity anomalies, suggest that high <sup>3</sup>He/<sup>4</sup>He is entrained only by the hottest and most buoyant mantle plumes. A prediction of this model is that the high <sup>3</sup>He/<sup>4</sup>He component is sampled by high-degree melting. We use a new geochemical database of ocean island lavas to demonstrate that high <sup>3</sup>He/<sup>4</sup>He is found only in tholeiitic (low alkali index) and mildly alkalic (intermediate alkali index) lavas, which result from high and moderate degrees of melting, respectively. Highly alkalic (high alkali index) lavas that are generated by low degrees of melting are not observed to have very high <sup>3</sup>He/<sup>4</sup>He. These observations support a model where the highest <sup>3</sup>He/<sup>4</sup>He plumes are the hottest and therefore melt to high degrees, which results in generation of tholeiites and mildly alkalic lavas. However, our observations suggest that high degrees of melting of hot plumes is a necessary but insufficient condition for generation of high <sup>3</sup>He/<sup>4</sup>He lavas. High degrees of melting of mantle domains with a high fraction of recycled material and/or depleted mantle material—both of which have low <sup>3</sup>He/<sup>4</sup>He—will generate low <sup>3</sup>He/<sup>4</sup>He lavas. Thus, only hot melting of mantle domains that have relatively pure high <sup>3</sup>He/<sup>4</sup>He source material (i.e., little or no recycled material or depleted low <sup>3</sup>He/<sup>4</sup>He mantle material) will result in generation of high <sup>3</sup>He/<sup>4</sup>He lavas. The conclusion that high <sup>3</sup>He/<sup>4</sup>He plumes melt more is supported by geophysical observations that suggest high <sup>3</sup>He/<sup>4</sup>He plumes are hotter—they have higher buoyancy flux and lower shear-wave velocity anomalies in the upper mantle—and hotter plumes should melt more than cooler plumes.</div></div>\",\"PeriodicalId\":11481,\"journal\":{\"name\":\"Earth and Planetary Science Letters\",\"volume\":\"666 \",\"pages\":\"Article 119490\"},\"PeriodicalIF\":4.8000,\"publicationDate\":\"2025-06-19\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Earth and Planetary Science Letters\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0012821X25002894\",\"RegionNum\":1,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Earth and Planetary Science Letters","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0012821X25002894","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
High 3He/4He plumes are hotter and melt more: evidence from the petrology and geochemistry of ocean island basalts
High 3He/4He (i.e., 3He/4He above the convecting upper mantle mid-ocean ridge basalt range (8 ± 2 RA)) is a rare component identified in hotspots that sample an early-formed, less-degassed domain in the planet. Relationships between the maximum 3He/4He and high hotspot buoyancy flux, and between maximum 3He/4He and low seismic shear-wave velocity anomalies, suggest that high 3He/4He is entrained only by the hottest and most buoyant mantle plumes. A prediction of this model is that the high 3He/4He component is sampled by high-degree melting. We use a new geochemical database of ocean island lavas to demonstrate that high 3He/4He is found only in tholeiitic (low alkali index) and mildly alkalic (intermediate alkali index) lavas, which result from high and moderate degrees of melting, respectively. Highly alkalic (high alkali index) lavas that are generated by low degrees of melting are not observed to have very high 3He/4He. These observations support a model where the highest 3He/4He plumes are the hottest and therefore melt to high degrees, which results in generation of tholeiites and mildly alkalic lavas. However, our observations suggest that high degrees of melting of hot plumes is a necessary but insufficient condition for generation of high 3He/4He lavas. High degrees of melting of mantle domains with a high fraction of recycled material and/or depleted mantle material—both of which have low 3He/4He—will generate low 3He/4He lavas. Thus, only hot melting of mantle domains that have relatively pure high 3He/4He source material (i.e., little or no recycled material or depleted low 3He/4He mantle material) will result in generation of high 3He/4He lavas. The conclusion that high 3He/4He plumes melt more is supported by geophysical observations that suggest high 3He/4He plumes are hotter—they have higher buoyancy flux and lower shear-wave velocity anomalies in the upper mantle—and hotter plumes should melt more than cooler plumes.
期刊介绍:
Earth and Planetary Science Letters (EPSL) is a leading journal for researchers across the entire Earth and planetary sciences community. It publishes concise, exciting, high-impact articles ("Letters") of broad interest. Its focus is on physical and chemical processes, the evolution and general properties of the Earth and planets - from their deep interiors to their atmospheres. EPSL also includes a Frontiers section, featuring invited high-profile synthesis articles by leading experts on timely topics to bring cutting-edge research to the wider community.