Ultra-slow cratonic denudation in Finland since 1.5 Ga indicated by tiered unconformities and impact structures
• Erosion history reconstructed for craton in southern Finland since 1.5 Ga. • Tiered unconformities and impact structures indicate erosion at <2.5 m/Ma. • Low-temperature thermochronology overestimates former sedimentary cover thickness. • Persistence of Phanerozoic fracture coatings, Palaeogene...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Hall, Adrian M. [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2021 |
|---|
| Schlagwörter: |
|---|
| Übergeordnetes Werk: |
Enthalten in: OC-043: Re-irradiation in head and neck cancers: A single institution prospective cohort study - Salunkhe, R. ELSEVIER, 2017, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:352 ; year:2021 ; pages:0 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.precamres.2020.106000 |
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Ultra-slow cratonic denudation in Finland since 1.5 Ga indicated by tiered unconformities and impact structures |
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• Erosion history reconstructed for craton in southern Finland since 1.5 Ga. • Tiered unconformities and impact structures indicate erosion at <2.5 m/Ma. • Low-temperature thermochronology overestimates former sedimentary cover thickness. • Persistence of Phanerozoic fracture coatings, Palaeogene groundwater and microbiomes. • Cratonic regime has tectonic stability, prolonged shallow burial and ultra-slow erosion. |
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• Erosion history reconstructed for craton in southern Finland since 1.5 Ga. • Tiered unconformities and impact structures indicate erosion at <2.5 m/Ma. • Low-temperature thermochronology overestimates former sedimentary cover thickness. • Persistence of Phanerozoic fracture coatings, Palaeogene groundwater and microbiomes. • Cratonic regime has tectonic stability, prolonged shallow burial and ultra-slow erosion. |
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• Erosion history reconstructed for craton in southern Finland since 1.5 Ga. • Tiered unconformities and impact structures indicate erosion at <2.5 m/Ma. • Low-temperature thermochronology overestimates former sedimentary cover thickness. • Persistence of Phanerozoic fracture coatings, Palaeogene groundwater and microbiomes. • Cratonic regime has tectonic stability, prolonged shallow burial and ultra-slow erosion. |
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