Gravity modeling finds a large magma body in the deep crust below the Gulf of Naples, Italy
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- ISSN
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2045-2322
- Extent
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Online-Ressource
- Language
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Englisch
- Notes
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online resource.
- Bibliographic citation
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Gravity modeling finds a large magma body in the deep crust below the Gulf of Naples, Italy ; volume:8 ; number:1 ; day:29 ; month:5 ; year:2018 ; pages:1-19 ; date:12.2018
Scientific reports ; 8, Heft 1 (29.5.2018), 1-19, 12.2018
- Classification
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Geowissenschaften
- Creator
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Fedi, M.
- Contributor
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Cella, F.
D’Antonio, M.
Florio, G.
Paoletti, V.
Morra, V.
SpringerLink (Online service)
- DOI
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10.1038/s41598-018-26346-z
- URN
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urn:nbn:de:101:1-2018080222535494462188
- Rights
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Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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15.08.2025, 7:38 AM CEST
Data provider
This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Fedi, M.
- Cella, F.
- D’Antonio, M.
- Florio, G.
- Paoletti, V.
- Morra, V.
- SpringerLink (Online service)
Other Objects (12)
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Dendritic crystallization in hydrous basaltic magmas controls magma mobility within the Earth’s crust
The generation of felsic magmas in the oceanic crust: assimilation-fractional-crystallization processes versus re-melting of the crust
Numerical simulation of magma ascent by dykes and crust formation at spreading centres
Numerical simulation of magma ascent by dykes and crust formation at spreading centres
Znaleziska / Finds
A 5-km-thick reservoir with > 380,000 km3 of magma within the ancient Earth's crust
CRUSt
CRUSt
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:CRUSt:
Silicic magma reservoirs in the Earth’s crust
Mechanisms of magma emplacement in the upper crust
Dendritic crystallization in hydrous basaltic magmas controls magma mobility within the Earth’s crust
The generation of felsic magmas in the oceanic crust: assimilation-fractional-crystallization processes versus re-melting of the crust
Numerical simulation of magma ascent by dykes and crust formation at spreading centres
Numerical simulation of magma ascent by dykes and crust formation at spreading centres
Znaleziska / Finds
A 5-km-thick reservoir with > 380,000 km3 of magma within the ancient Earth's crust
CRUSt
CRUSt
CRUSt
:CRUSt:
Silicic magma reservoirs in the Earth’s crust
Mechanisms of magma emplacement in the upper crust
Dendritic crystallization in hydrous basaltic magmas controls magma mobility within the Earth’s crust
The generation of felsic magmas in the oceanic crust: assimilation-fractional-crystallization processes versus re-melting of the crust
Numerical simulation of magma ascent by dykes and crust formation at spreading centres
Numerical simulation of magma ascent by dykes and crust formation at spreading centres
Znaleziska / Finds
A 5-km-thick reservoir with > 380,000 km3 of magma within the ancient Earth's crust
CRUSt
CRUSt
CRUSt