Tectonic stresses on the boundary of the Aegean domain: “in situ” measurements by overcoring
Identifieur interne : 000511 ( Main/Merge ); précédent : 000510; suivant : 000512Tectonic stresses on the boundary of the Aegean domain: “in situ” measurements by overcoring
Auteurs : C. Paquin [France] ; J. Bloyet [France] ; C. Angelidis [Grèce]Source :
- Tectonophysics [ 0040-1951 ] ; 1984.
Descripteurs français
- Wicri :
- topic : Crète.
English descriptors
- KwdEn :
- Active faults, Aegean domain, Angelier, Characterised, Crete, Focal mechanisms, Ionian, Ionian islands, Limestone, Magmatic rocks, Marble outcrop, Mercier, Milo, Outcrop, Overcoring, Paquin, Preapulian zone, Quality factor, Regional tectonics, Structural analysis, Tectonic, Tectonic stresses, Tectonics, Volcanic, Volcanic rocks, Western crete.
- Teeft :
- Active faults, Aegean domain, Angelier, Characterised, Crete, Focal mechanisms, Ionian, Ionian islands, Limestone, Magmatic rocks, Marble outcrop, Mercier, Milo, Outcrop, Overcoring, Paquin, Preapulian zone, Quality factor, Regional tectonics, Structural analysis, Tectonic, Tectonic stresses, Tectonics, Volcanic, Volcanic rocks, Western crete.
Abstract
Abstract: Direct “in situ” measurements of the horizontal stresses on the border of the Aegean domain, obtained by overcoring in boreholes a few meters deep, revealed the various characteristics of plate boundaries: continent—continent collision, subduction, inter-arc basin, etc.
Url:
DOI: 10.1016/0040-1951(84)90062-3
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ISTEX:D2A1EAFAAE9B4D0BC360B82123915E5F2C1D9DB4Le document en format XML
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<term>Characterised</term>
<term>Crete</term>
<term>Focal mechanisms</term>
<term>Ionian</term>
<term>Ionian islands</term>
<term>Limestone</term>
<term>Magmatic rocks</term>
<term>Marble outcrop</term>
<term>Mercier</term>
<term>Milo</term>
<term>Outcrop</term>
<term>Overcoring</term>
<term>Paquin</term>
<term>Preapulian zone</term>
<term>Quality factor</term>
<term>Regional tectonics</term>
<term>Structural analysis</term>
<term>Tectonic</term>
<term>Tectonic stresses</term>
<term>Tectonics</term>
<term>Volcanic</term>
<term>Volcanic rocks</term>
<term>Western crete</term>
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<term>Aegean domain</term>
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<term>Crete</term>
<term>Focal mechanisms</term>
<term>Ionian</term>
<term>Ionian islands</term>
<term>Limestone</term>
<term>Magmatic rocks</term>
<term>Marble outcrop</term>
<term>Mercier</term>
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<term>Outcrop</term>
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<term>Paquin</term>
<term>Preapulian zone</term>
<term>Quality factor</term>
<term>Regional tectonics</term>
<term>Structural analysis</term>
<term>Tectonic</term>
<term>Tectonic stresses</term>
<term>Tectonics</term>
<term>Volcanic</term>
<term>Volcanic rocks</term>
<term>Western crete</term>
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<front><div type="abstract" xml:lang="en">Abstract: Direct “in situ” measurements of the horizontal stresses on the border of the Aegean domain, obtained by overcoring in boreholes a few meters deep, revealed the various characteristics of plate boundaries: continent—continent collision, subduction, inter-arc basin, etc.</div>
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