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  1. 1
    ...) information and Ar-Ar geochronology for intraplate lavas from the Arctic Ocean. Subaerial lavas were collected...
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  2. 2
    ...) information and Ar-Ar geochronology for intraplate lavas from the Arctic Ocean. Subaerial lavas were collected...
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  3. 3
    ... of the NLT–WGR lavas confirms a binary mixing model involving melts from a depleted MORB mantle source and a...
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  4. 4
    ... (CLT) lavas display 4 He/ 3 He between 89,710 and 97,530 (R/Ra between 7.4 and 8.1), similar...
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  5. 5
    ... spreading Lena Trough (~0.75 cm/yr effective full rate). Central Lena Trough (CLT) lavas display 4He/3He...
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  6. 6
    ... of the NLT-WGR lavas confirms a binary mixing model involving melts from a depleted MORB mantle source and a...
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  7. 7
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  9. 9
    ... (CLT) lavas display 4 He/ 3 He between 89,710 and 97,530 (R/Ra between 7.4 and 8.1), similar...
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  10. 10
    ... (CLT) lavas display 4 He/ 3 He between 89,710 and 97,530 (R/Ra between 7.4 and 8.1), similar...
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  11. 11
    ... (CLT) lavas display 4 He/ 3 He between 89,710 and 97,530 (R/Ra between 7.4 and 8.1), similar...
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  12. 12
    ... (CLT) lavas display 4 He/ 3 He between 89,710 and 97,530 (R/Ra between 7.4 and 8.1), similar...
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  13. 13
    ... (CLT) lavas display 4 He/ 3 He between 89,710 and 97,530 (R/Ra between 7.4 and 8.1), similar...
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  14. 14
    ... (CLT) lavas display 4 He/ 3 He between 89,710 and 97,530 (R/Ra between 7.4 and 8.1), similar...
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  15. 15
  16. 16
    ... variability on Fe isotope systematics in mid-ocean ridge lavas. Scientific Reports, 11(1), (2021): 4123, https...
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  17. 17
    ... to existing data from the fast spreading East Pacific Rise ridge. Results indicate that Gakkel lavas...
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  18. 18
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