Pleistocene intraplate magmatism in the Goto Islands, SW Japan: Implications for mantle source evolution and regional geodynamics
• We report geochemical compositions of the youngest intraplate vocanics in NW Kyushu. • The regional lithosphere evolved from extension to compression since mid-Miocene. • The volcanism evolved from mid Miocene low-K tholeiite to Pleistocene alkali basalt. • Young asthenosphere-born magmas show hyb...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Hoang, Nguyen [verfasserIn] |
|---|
| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2013 |
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| Schlagwörter: |
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| Umfang: |
17 |
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| Übergeordnetes Werk: |
Enthalten in: Non-homothetic preferences: Explaining unidirectional movements in wage differentials - Santra, Sattwik ELSEVIER, 2014, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:68 ; year:2013 ; pages:1-17 ; extent:17 |
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| DOI / URN: |
10.1016/j.jog.2013.03.002 |
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Pleistocene intraplate magmatism in the Goto Islands, SW Japan: Implications for mantle source evolution and regional geodynamics |
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• We report geochemical compositions of the youngest intraplate vocanics in NW Kyushu. • The regional lithosphere evolved from extension to compression since mid-Miocene. • The volcanism evolved from mid Miocene low-K tholeiite to Pleistocene alkali basalt. • Young asthenosphere-born magmas show hybrids of depleted and enriched mantle type 1. • This composition is believed to present throughout East and SE Asian asthenosphere. |
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• We report geochemical compositions of the youngest intraplate vocanics in NW Kyushu. • The regional lithosphere evolved from extension to compression since mid-Miocene. • The volcanism evolved from mid Miocene low-K tholeiite to Pleistocene alkali basalt. • Young asthenosphere-born magmas show hybrids of depleted and enriched mantle type 1. • This composition is believed to present throughout East and SE Asian asthenosphere. |
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• We report geochemical compositions of the youngest intraplate vocanics in NW Kyushu. • The regional lithosphere evolved from extension to compression since mid-Miocene. • The volcanism evolved from mid Miocene low-K tholeiite to Pleistocene alkali basalt. • Young asthenosphere-born magmas show hybrids of depleted and enriched mantle type 1. • This composition is believed to present throughout East and SE Asian asthenosphere. |
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