Interior structure of the Moon: Constraints from seismic tomography, gravity and topography
Interior structure of the Moon constrained from seismic tomography, gravity and topography. * A thick (about 225km or more) and heterogeneous lunar lithosphere is suggested. * The observed flattening is likely a "fossil" bulge unrelated to present-day mantle anomalies.
Autor*in: |
Steinberger, Bernhard [verfasserIn] |
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Format: |
Artikel |
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Sprache: |
Englisch |
Erschienen: |
2015 |
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Rechteinformationen: |
Nutzungsrecht: © COPYRIGHT 2015 Elsevier B.V. |
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Schlagwörter: |
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Übergeordnetes Werk: |
Enthalten in: Physics of the earth and planetary interiors - Amsterdam [u.a.] : Elsevier, 1967, 245(2015), Seite 26-39 |
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Übergeordnetes Werk: |
volume:245 ; year:2015 ; pages:26-39 |
Links: |
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DOI / URN: |
10.1016/j.pepi.2015.05.005 |
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Interior structure of the Moon: Constraints from seismic tomography, gravity and topography |
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Interior structure of the Moon constrained from seismic tomography, gravity and topography. * A thick (about 225km or more) and heterogeneous lunar lithosphere is suggested. * The observed flattening is likely a "fossil" bulge unrelated to present-day mantle anomalies. |
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Interior structure of the Moon constrained from seismic tomography, gravity and topography. * A thick (about 225km or more) and heterogeneous lunar lithosphere is suggested. * The observed flattening is likely a "fossil" bulge unrelated to present-day mantle anomalies. |
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Interior structure of the Moon constrained from seismic tomography, gravity and topography. * A thick (about 225km or more) and heterogeneous lunar lithosphere is suggested. * The observed flattening is likely a "fossil" bulge unrelated to present-day mantle anomalies. |
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Interior structure of the Moon: Constraints from seismic tomography, gravity and topography |
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gravity and topography</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2015</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Interior structure of the Moon constrained from seismic tomography, gravity and topography. * A thick (about 225km or more) and heterogeneous lunar lithosphere is suggested. * The observed flattening is likely a "fossil" bulge unrelated to present-day mantle anomalies.</subfield></datafield><datafield tag="540" ind1=" 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