Formation of geothermal resources at lithospheric subduction zones
Identifieur interne : 000482 ( Main/Exploration ); précédent : 000481; suivant : 000483Formation of geothermal resources at lithospheric subduction zones
Auteurs : John W. Reeder [États-Unis]Source :
- International Journal of Energy Research [ 0363-907X ] ; 1985-07.
Descripteurs français
- Wicri :
- topic : énergie géothermique.
English descriptors
- KwdEn :
- Active subduction zones, Active volcanoes, Aleutian, American journal, Andes, Andesite, Backarc regions, Basalt, Basaltic, Basaltic magmas, Central america, Central andes, Centre, Chichester, Compressional, Compressional environment, Continental crust, Crust, Crustal, Eastern aleutian islands, Explosive volcanism, Fracture, Geological society, Geophysical, Geophysical research, Geothermal, Geothermal energy, Geothermal fields, Geothermal resources, Geothermal systems, Heat energy, Heat flow, Heat source, High temperature, High temperature hydrothermal systems, Hydrothermal, Hydrothermal system, Hydrothermal systems, Intrusive rocks, Island arcs, Large hydrothermal systems, Lithosphere, Lithospheric, Lithospheric subduction zones, Magma, Magmatic, National academy press, Nations symposium, Northern part, Oceanic, Oceanic crust, Permeable, Plutonic, Quaternary, Reeder, Regional heat flow, Silicic, Southern andes, Special issue, Subduction, Subduction zone, Subduction zones, Such arcs, Such resources, Such systems, Tectonic, Tensional, Tholeiitic, Unalaska island, Uyeda, Volcanic, Volcanic arcs, Volcanic rocks, Volcanism, Volcano.
- Teeft :
- Active subduction zones, Active volcanoes, Aleutian, American journal, Andes, Andesite, Backarc regions, Basalt, Basaltic, Basaltic magmas, Central america, Central andes, Centre, Chichester, Compressional, Compressional environment, Continental crust, Crust, Crustal, Eastern aleutian islands, Explosive volcanism, Fracture, Geological society, Geophysical, Geophysical research, Geothermal, Geothermal energy, Geothermal fields, Geothermal resources, Geothermal systems, Heat energy, Heat flow, Heat source, High temperature, High temperature hydrothermal systems, Hydrothermal, Hydrothermal system, Hydrothermal systems, Intrusive rocks, Island arcs, Large hydrothermal systems, Lithosphere, Lithospheric, Lithospheric subduction zones, Magma, Magmatic, National academy press, Nations symposium, Northern part, Oceanic, Oceanic crust, Permeable, Plutonic, Quaternary, Reeder, Regional heat flow, Silicic, Southern andes, Special issue, Subduction, Subduction zone, Subduction zones, Such arcs, Such resources, Such systems, Tectonic, Tensional, Tholeiitic, Unalaska island, Uyeda, Volcanic, Volcanic arcs, Volcanic rocks, Volcanism, Volcano.
Abstract
This paper examines in a very broad fashion the formation of geothermal resources at lithospheric subduction zones. Regions of highly silicic calc‐alkaline Quaternary volcanoes and/or plutons have been identified as prime candidates for having high‐temperature hydrothermal systems. Regions of large tholeiitic Quaternary volcanoes have been identified as prime candidates for having large moderate‐temperature hydrothermal systems. In addition, active magmatic, phreatomagnetic, and/or tectonic fracturing must be occurring in order to keep any moderate to high temperature hydrothermal system from chemically sealing. Connate, meteoric and/or oceanic water sources must also be present. Owing to tectonic and magmatic processes, volcanic arcs of subduction zones represent regions of the crust that have anomalously high mechanical and heat energy. Such arc regions are expected to contain significantly more moderate to high temperature hydrothermal systems than what is presently known. Many of these arcs are briefly discussed with respect to their potential for containing such resources.
Url:
DOI: 10.1002/er.4440090305
Affiliations:
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Reeder</name><affiliation wicri:level="1"><country xml:lang="fr">États-Unis</country><wicri:regionArea>Alaska Div. Geol. & Geophys. 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system</term><term>Hydrothermal systems</term><term>Intrusive rocks</term><term>Island arcs</term><term>Large hydrothermal systems</term><term>Lithosphere</term><term>Lithospheric</term><term>Lithospheric subduction zones</term><term>Magma</term><term>Magmatic</term><term>National academy press</term><term>Nations symposium</term><term>Northern part</term><term>Oceanic</term><term>Oceanic crust</term><term>Permeable</term><term>Plutonic</term><term>Quaternary</term><term>Reeder</term><term>Regional heat flow</term><term>Silicic</term><term>Southern andes</term><term>Special issue</term><term>Subduction</term><term>Subduction zone</term><term>Subduction zones</term><term>Such arcs</term><term>Such resources</term><term>Such systems</term><term>Tectonic</term><term>Tensional</term><term>Tholeiitic</term><term>Unalaska island</term><term>Uyeda</term><term>Volcanic</term><term>Volcanic arcs</term><term>Volcanic rocks</term><term>Volcanism</term><term>Volcano</term></keywords><keywords scheme="Teeft" xml:lang="en"><term>Active subduction zones</term><term>Active volcanoes</term><term>Aleutian</term><term>American journal</term><term>Andes</term><term>Andesite</term><term>Backarc regions</term><term>Basalt</term><term>Basaltic</term><term>Basaltic magmas</term><term>Central america</term><term>Central andes</term><term>Centre</term><term>Chichester</term><term>Compressional</term><term>Compressional environment</term><term>Continental crust</term><term>Crust</term><term>Crustal</term><term>Eastern aleutian islands</term><term>Explosive volcanism</term><term>Fracture</term><term>Geological society</term><term>Geophysical</term><term>Geophysical research</term><term>Geothermal</term><term>Geothermal energy</term><term>Geothermal fields</term><term>Geothermal resources</term><term>Geothermal systems</term><term>Heat energy</term><term>Heat flow</term><term>Heat source</term><term>High temperature</term><term>High temperature hydrothermal systems</term><term>Hydrothermal</term><term>Hydrothermal system</term><term>Hydrothermal systems</term><term>Intrusive rocks</term><term>Island arcs</term><term>Large hydrothermal systems</term><term>Lithosphere</term><term>Lithospheric</term><term>Lithospheric subduction zones</term><term>Magma</term><term>Magmatic</term><term>National academy press</term><term>Nations symposium</term><term>Northern part</term><term>Oceanic</term><term>Oceanic crust</term><term>Permeable</term><term>Plutonic</term><term>Quaternary</term><term>Reeder</term><term>Regional heat flow</term><term>Silicic</term><term>Southern andes</term><term>Special issue</term><term>Subduction</term><term>Subduction zone</term><term>Subduction zones</term><term>Such arcs</term><term>Such resources</term><term>Such systems</term><term>Tectonic</term><term>Tensional</term><term>Tholeiitic</term><term>Unalaska island</term><term>Uyeda</term><term>Volcanic</term><term>Volcanic arcs</term><term>Volcanic rocks</term><term>Volcanism</term><term>Volcano</term></keywords><keywords scheme="Wicri" type="topic" xml:lang="fr"><term>énergie géothermique</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">This paper examines in a very broad fashion the formation of geothermal resources at lithospheric subduction zones. Regions of highly silicic calc‐alkaline Quaternary volcanoes and/or plutons have been identified as prime candidates for having high‐temperature hydrothermal systems. Regions of large tholeiitic Quaternary volcanoes have been identified as prime candidates for having large moderate‐temperature hydrothermal systems. In addition, active magmatic, phreatomagnetic, and/or tectonic fracturing must be occurring in order to keep any moderate to high temperature hydrothermal system from chemically sealing. Connate, meteoric and/or oceanic water sources must also be present. Owing to tectonic and magmatic processes, volcanic arcs of subduction zones represent regions of the crust that have anomalously high mechanical and heat energy. Such arc regions are expected to contain significantly more moderate to high temperature hydrothermal systems than what is presently known. Many of these arcs are briefly discussed with respect to their potential for containing such resources.</div></front></TEI><affiliations><list><country><li>États-Unis</li></country></list><tree><country name="États-Unis"><noRegion><name sortKey="Reeder, John W" sort="Reeder, John W" uniqKey="Reeder J" first="John W." last="Reeder">John W. Reeder</name></noRegion></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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